中国陆相白垩系沉积特征与古地理面貌
|
摘要
陆地是地球表层系统的重要组成部分,白垩纪地球表层系统重大地质事件在陆地上也得到良好的响应。科学界已经认识到：缺乏来自陆地沉积记录的研究,将很难完整而准确地探索白垩纪地球表层系统变化的性质和机制。东亚大陆是白垩纪时期最大的陆地,而中国处于东亚大陆东部边缘,白垩纪地层发育,对研究白垩纪构造体制的转变及气候变化具有重要意义。
白垩纪地层格架的建立是本文的工作基础。本文在前人成果的基础上,补充了大量火山岩同位素年代地层学数据、生物地层学数据及磁性地层学数据,建立了中国陆相白垩纪地层格架。早白垩世早期地层只在西部地区发育,而早白垩世晚期地层在全国范围内广泛发育；晚白垩世早期,西北地区地层缺失,东北地区除松辽盆地外地层缺失,华北及东南地区地层分布局限,西南及中南地区地层发育；晚白垩世晚期,东南地区及华北地区地层缺失,西北及东北地区零星分布,西南及中南地区地层发育。
对不同地区典型剖面进行了岩相、充填序列及沉积相研究,结合白垩纪沉积盆地的性质讨论了不同地区盆地沉积特征在不同盆地演化阶段沉积特征的异同。在此基础上,将中国陆相白垩纪地层划分为东北地层区、西北地层区、华北地层区、西南地层区、中南地层区及东南地层区。认为西南地层区及西北地层区盆地具有挠曲盆地的性质,在干旱-半干旱气候环境下形成了以红色碎屑岩系为主的河湖相沉积；而东北地层区、华北地层区、中南地层区及华南地层区形成了巨大的裂谷盆地系统,这些裂谷盆地在不同地层区充填序列的差异受构造活动和气候状况共同控制。
中国白垩纪古地理面貌的重建是本文研究的最终目的。在白垩纪地层数据库的支撑下,本文限定了白垩纪中国的海陆边界,统计了白垩纪恐龙和“特殊沉积”的分布,在此基础上编制了《中国白垩纪古地理面貌资料底图》并最终重建了中国白垩纪古地理面貌。早白垩世早期,沉积盆地主要在西部地区发育,中国的古地理面貌为“东高西低”；早白垩世晚期,沉积盆地遍布全国,大兴安岭-太行山-华蓥山一线及祁连山-秦岭-大别山一线分别构成了中国东、西与南、北的分界线,中国东部进入大规模伸展时期。晚白垩世早期,沉积盆地主要发育在中南及西南地层区,古地理面貌特征为“西高东低”,古亚洲高原形成,华北地层区及东北地层区(除松辽盆地外)隆起剥蚀。晚白垩世晚期,西北地层区及东北地层区局部凹陷接受沉积,沉积盆地主要发育在中南及西南地层区,华北高原及东部山脉扩张。
Continent is an important part of earth surface system. Some important event happened in Cretaceous occurred on continent too. Scientists had realized that it is impossible to research the characteristic and mechanism of earth surface system changing in Cretaceous. East Asia is the largest continent in Cretaceous. China lies in its east margin. It is important to research Cretaceous stratum in China. They contain information of tectonic system change, basin-mountain coupling, and climate change.
Continental stratigraphic framework in China is the base of this paper. Basis in the former study, a new stratigraphic framework which includes many new data of lava ages, biostratigraphy and magnetostratigraphy is established. Cretaceous stratums only occur in western China in early Early Cretaceous and they grow all over China in late Early Cretaceous, In early Late Cretaceous, northwestern China and northeastern China except Songliao basin are lack of Cretaceous stratum. Cretaceous stratums occur locally in North China and southeastern China but they extensively occur in southwestern and central South China through early Late Cretaceous. In late Late Cretaceous, southeastern China and North China are lack of Cretaceous stratum and Cretaceous stratums occur locally in northwestern and northeastern China but they extensively occur in southwestern and central South China.
Based on the study of lithofacies, filling sequence, basin type and sedimentary facies from many typical profiles in different basins, Cretaceous continental stratums are divided into six types which are named Northeast area, Northwest area, North China area, Southwest area, Central South area and Southeast area. It is considered that basins in Southwest area and Northwest area are flexural basins. They are filled by red bed which is formed in river and lake system under arid to semi-arid climate. Northeast area, North China area, Central South area and Southeast area lied in a huge rift basin system. The differences between these basins in filling sequence are controlled by both tectonic activity and climate.
Reconstruction of the paleogeography of China in Cretaceous is the most important matter. Under the help of continental Cretaceous stratum data-base, Cretaceous dinosaurs and'special deposition'in China are checked. And the boundary of the land in China has been suggested. A chart named'Data chart of Cretaceous paleography in China'has been finished. And Cretaceous paleogeography in China has been reconstructed. A huge plateau named'East plateau'lied across the east margin of China, and basins lied in western China in early Early Cretaceous. In late Early Cretaceous, eastern China is under extension condition. Sediment basins are exist all over China. The Da Hinggan-Taihang mountain-Huaying mountain and Qilian mountain-Qinling-Dabie mountain have existed and they are the boundary of western-eastern China and North-South China. There is a huge plateau in central Asian, which is named Ancient Asian plateau. North area and Northeast area (except Songliao basin) lifted in early Late Cretaceous. In late Late Cretaceous, North China plateau and east range exist. Northeast area and Northwest area are locally filled by clastic rock formed in river and lake. Central South area and Southeast area are the main depositional location through Late Cretaceous.
白垩纪地层格架的建立是本文的工作基础。本文在前人成果的基础上,补充了大量火山岩同位素年代地层学数据、生物地层学数据及磁性地层学数据,建立了中国陆相白垩纪地层格架。早白垩世早期地层只在西部地区发育,而早白垩世晚期地层在全国范围内广泛发育；晚白垩世早期,西北地区地层缺失,东北地区除松辽盆地外地层缺失,华北及东南地区地层分布局限,西南及中南地区地层发育；晚白垩世晚期,东南地区及华北地区地层缺失,西北及东北地区零星分布,西南及中南地区地层发育。
对不同地区典型剖面进行了岩相、充填序列及沉积相研究,结合白垩纪沉积盆地的性质讨论了不同地区盆地沉积特征在不同盆地演化阶段沉积特征的异同。在此基础上,将中国陆相白垩纪地层划分为东北地层区、西北地层区、华北地层区、西南地层区、中南地层区及东南地层区。认为西南地层区及西北地层区盆地具有挠曲盆地的性质,在干旱-半干旱气候环境下形成了以红色碎屑岩系为主的河湖相沉积；而东北地层区、华北地层区、中南地层区及华南地层区形成了巨大的裂谷盆地系统,这些裂谷盆地在不同地层区充填序列的差异受构造活动和气候状况共同控制。
中国白垩纪古地理面貌的重建是本文研究的最终目的。在白垩纪地层数据库的支撑下,本文限定了白垩纪中国的海陆边界,统计了白垩纪恐龙和“特殊沉积”的分布,在此基础上编制了《中国白垩纪古地理面貌资料底图》并最终重建了中国白垩纪古地理面貌。早白垩世早期,沉积盆地主要在西部地区发育,中国的古地理面貌为“东高西低”；早白垩世晚期,沉积盆地遍布全国,大兴安岭-太行山-华蓥山一线及祁连山-秦岭-大别山一线分别构成了中国东、西与南、北的分界线,中国东部进入大规模伸展时期。晚白垩世早期,沉积盆地主要发育在中南及西南地层区,古地理面貌特征为“西高东低”,古亚洲高原形成,华北地层区及东北地层区(除松辽盆地外)隆起剥蚀。晚白垩世晚期,西北地层区及东北地层区局部凹陷接受沉积,沉积盆地主要发育在中南及西南地层区,华北高原及东部山脉扩张。
Continent is an important part of earth surface system. Some important event happened in Cretaceous occurred on continent too. Scientists had realized that it is impossible to research the characteristic and mechanism of earth surface system changing in Cretaceous. East Asia is the largest continent in Cretaceous. China lies in its east margin. It is important to research Cretaceous stratum in China. They contain information of tectonic system change, basin-mountain coupling, and climate change.
Continental stratigraphic framework in China is the base of this paper. Basis in the former study, a new stratigraphic framework which includes many new data of lava ages, biostratigraphy and magnetostratigraphy is established. Cretaceous stratums only occur in western China in early Early Cretaceous and they grow all over China in late Early Cretaceous, In early Late Cretaceous, northwestern China and northeastern China except Songliao basin are lack of Cretaceous stratum. Cretaceous stratums occur locally in North China and southeastern China but they extensively occur in southwestern and central South China through early Late Cretaceous. In late Late Cretaceous, southeastern China and North China are lack of Cretaceous stratum and Cretaceous stratums occur locally in northwestern and northeastern China but they extensively occur in southwestern and central South China.
Based on the study of lithofacies, filling sequence, basin type and sedimentary facies from many typical profiles in different basins, Cretaceous continental stratums are divided into six types which are named Northeast area, Northwest area, North China area, Southwest area, Central South area and Southeast area. It is considered that basins in Southwest area and Northwest area are flexural basins. They are filled by red bed which is formed in river and lake system under arid to semi-arid climate. Northeast area, North China area, Central South area and Southeast area lied in a huge rift basin system. The differences between these basins in filling sequence are controlled by both tectonic activity and climate.
Reconstruction of the paleogeography of China in Cretaceous is the most important matter. Under the help of continental Cretaceous stratum data-base, Cretaceous dinosaurs and'special deposition'in China are checked. And the boundary of the land in China has been suggested. A chart named'Data chart of Cretaceous paleography in China'has been finished. And Cretaceous paleogeography in China has been reconstructed. A huge plateau named'East plateau'lied across the east margin of China, and basins lied in western China in early Early Cretaceous. In late Early Cretaceous, eastern China is under extension condition. Sediment basins are exist all over China. The Da Hinggan-Taihang mountain-Huaying mountain and Qilian mountain-Qinling-Dabie mountain have existed and they are the boundary of western-eastern China and North-South China. There is a huge plateau in central Asian, which is named Ancient Asian plateau. North area and Northeast area (except Songliao basin) lifted in early Late Cretaceous. In late Late Cretaceous, North China plateau and east range exist. Northeast area and Northwest area are locally filled by clastic rock formed in river and lake. Central South area and Southeast area are the main depositional location through Late Cretaceous.
引文
[1]Peter W S, Robert A S, Simon P K, et al. The Cretaceous World [M]. Cambridge:Cambridge University Press,2003:360.
[2]马宗晋,杜品仁,卢苗安.地球的多圈层相互作用[J].地学前缘,2001，8：3-8.
[3]Larson R L. Latest pulse of the Earth:Evidence for a mid-Cretaceous superplume [J]. Geology, 1991,19:547-550.
[4]Kaiho K, Saito S. Oceanic crust production and climate during the past 100 Myr [J]. Terra Nova,1994,6:376-384.
[5]Schlanger S O, Jenkyns H C. Cretaceous oceanic anoxic events:Cause and consequence [J]. Geologie en Mijinbouw,1976,55:179-184.
[6]王成善,胡修棉.白垩纪世界与大洋红层[J].地学前缘,2005,12(2)：11-21.
[7]Wang C S, Hu X M, et al. Upper Cretaceous oceanic red beds in southern Tibet:A major change from anoxic to oxic, deep-sea environments [J]. Cretaceous Research,2005,26: 21-32.
[8]Hu X M, Luba J, Wang C S, et al. Upper Cretaceous oceanic red beds (CORBs) in the Tethys: occurrences, lithofacies, age and environments [J]. Cretaceous Research,2005,26:3-20.
[9]Leckie R M, Bralower T J, Cashman R. Oceanic anoxic events and plankon evolution:biotic response to tectonic forcing during the mid-Cretaceous [J]. Paleoceanography,2002,17 (3): 1041. doi:10.1029/2001PA000623.
[10]Cronin M, Tauxe L, Constable C, et al. Noise in the quite zone [J]. Earth and Planetary Science Letters,2001,190:13-30.
[11]史瑞萍,朱日祥.白垩纪地球物理场异常与地球深部动力学[J].地球物理学进展,2002,17(2)：295-300.
[12]Zhao X X. The Earth's magnetic field and global geologic phenomena in Mid-Cretaceous [J]. Earth Science Frontiers,2005,12 (2):199-216.
[13]王成善,曹珂等.沉积记录与白垩纪地球表层系统变化[J].地学前缘,2009，16(5)：1-14.
[14]Tarduno J A, Sliter W V, Kroenke L, Leckie R M, Mayer H, Mahoney J J, Musgrave R, Storey M, and Winterer E L. Rapid formation of Ontong Java Plateau by Aptian mantle volcanism [J]. Science,1991,254:399-403.
[15]Duncan R A. A time frame for construction of the Kerguelen Plateau and Broken Ridge [J]. Petrol,2002,43:1109-1119.
[16]Duncan R A, Hargraves RB. Plate tectonic evolution of the Caribbean region in the mantle reference frame [J]. Geol. Soc. Amer. Mem,1984,162:81-93.
[17]Vaughan A P M. Circum-Pacific mid-Cretaceous deformation and uplift:a superplume-related event [J]? Geology,1995,23:491-494.
[18]Ratcliff J T, Bercovici D, Schubert G, et al. Mantle plume heads and the initiation of plate tectonic reorganizations [J]. Earth and Planetary Science Letters,1998,156:195-207.
[19]Wilson P A, Norris R D. Warm tropical ocean surface and global anoxia during the mid-Cretaceous period [J], Nature,2001,412:425-429.
[20]Chumakov N M. Climatic zones in the middle of the Cretaceous Period [J], Stratigraphy and Geological Correlation,1995,3:3-14.
[21]Kominz M A. Oceanic ridge volumes and sea-level change:an error analysis [M] (in Interregional Unconformities and Hydrocarbon Accumulation), edited by J.S. Schlee, Amer. Assoc. Petrol. Geol. Mem.1984,36:109-127.
[22]Matsumoto T. Inter-regional correlation of transgressions and regressions in the Cretaceous period [J]. Cretaceous Research,1980,1 (4):359-373.
[23]Huber B T, Norris R D, Kenneth G, MacLeod. Deep-sea paleotemperature record of extreme warmth during the Cretaceous [J]. Geology,2002,30:123-126.
[24]Jarvis I, Amina M, Richard T J, et al. Late Cretaceous (Campanian) carbon isotope events, sea-level change and correlation of the Tethyan and Boreal realms [J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2002,188:215-248.
[25]Jenkyns H C, Cretaceous anoxic events:From continents to oceans[J]. Geol. Soc. London, 1980,137,171-188.
[26]Arthur M A, Schlanger S O. Cretaceous "Oceanic Anoxic Events" as causal factors in development of reef-reservoired giant oil fields [J]. Amer. Assoc. Petrol. Geol. Bull.,1979, 63,870-885.
[27]Scholle P A, Arthur M A. Carbon isotope fluctuations in Cretaceous pelagic limestones: Potential stratigraphic and petroleum exploration tool [J]. AAPG Bull.,1980,64,67-87.
[28]Bralower T J, Fullagar P D, Paull C K, et al. Mid-Cretaceous strontium-isotope stratigraphy of deep-sea sections. Geological Society of America Bulletin [J],1997,109:1421-1442.
[29]Jones, C E, H C. Jenkyns. Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous [J]. Amer. Jour. Science,2001 301, 112-149.
[30]Tarduno J, Brinkman D B, Renne P R, et al. Evidence for extreme climatic warmth from Late Cretaceous Arctic vertebrates [J]. Science,1998,282:2241-2244.
[31]Huber, B T, Hodell, D A, and C P Hamilton. Middle-Late Cretaceous climate of the southern high latitudes:Stable isotopic evidence for minimal equator-to-pole thermal gradients [J]. Geol. Soc. Amer. Bull.,1995,107,1164-1191.
[32]Norris R D, P A Wilson. Low-latitude sea-surface temperatures for the mid-Cretaceous and the evolution of planktic foraminifera [J]. Geol.,1998,26:823-826.
[33]Fassell M L, T J Bralower. Warm, equable mid-Cretaceous:Stable isotope evidence, in Evolution of the Cretaceous Ocean-Climate System [J]. Geol. Soc. Amer. Spec. Paper.1999, 332:121-142.
[34]Huber B T, Leckie R M, Norris R D, et al.Foraminiferal assemblage and stable isotopic change across the Cenomanian-Turonian boundary in the subtropical North Atlantic [J]. Jour. Foram. Res.,1999,29,392-417.
[35]Bice K L, Birgel D, Meyers P A, et al. A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO2 concentrations [J]. Paleoceanography,2006,21(2): PA2002
[36]Fricke H C. Latitudinal gradients in temperature over North America during the early Eocene using a combined oxygen isotope, paleobotanical approach (in Early Paleogene warm climates and biosphere dynamics; short papers and extended abstracts). GFF,2000,122 (l):50
[37]Tim W, Luis Gonzalez, Greg L, Chris P. Middle Cretaceous greenhouse hydrologic cycle of North America. Geology [J],2001,29:363-366.
[38]Huber B T., Richard D N, Kenneth G M. Deep-sea paleotemperature record of extreme warmth during the Cretaceous [J]. Geology,2002,30:123-126.
[39]李祥辉,·胡修棉等.白垩纪古海洋气候变化及主要问题[J].地球科学进展,2004，19(增刊)：83-92.
[40]Royer D L, Berner R A, Montanez I P, et al. CO_2 as a primary driver of Phanerozoic climate [J]. GSA Today,2004,14:4-10.
[41]Bice K L, Norris R D. Possible atmospheric CO_2 extremes of the warm mid-Cretaceous (late Albian-Turonian) [J]. Paleoceanography,2003,18 (2):1031, doi:10.1029/2002PA000848.
[42]Premoli Silva I, Sliter W V. Cretaceous Paleoceanography:Evidence from planktonic foraminiferal evolution [J]. Soc. Am., Spec. Paper,1999,332:301-328.
[43]Erbacher J, Thurow J, Littke R. Evolution patterns of radiolaria and organic matter variations: A new approach to identify sea-level changes in mid-Cretaceous pelagic environments [J]. Geology,1996,24:499-502.
[44]Bown P R, Rutledge D C, Crux J A, Gallagher L T. Lower Cretaceous (in Calcareous nannofossil biostratigraphy. Bown, part of British Micropalaeontological Society Publication Series) Kluwer Academic Publishers, Dordrecht, Netherlands.1999,86-131.
[45]姬书安.热河生物群重大研究进展综述[J].中国地质,2001,28(4)：19-23.
[46]黄清华,谭伟等.松辽盆地白垩纪地层序列与年代地层[J].大庆石油地质与开发,1999,18(6)：15-17.
[47]罗以达,俞云文.试论永康群时代及区域地层对比[J].中国地质,2004,31(4)：395-399.
[481张妮.江苏侏罗系-白垩系火山岩地层对比及划分探讨[J].地层学杂志,2009，33(1)：91-97.
[49]梅冥相,于炳松等.塔里木盆地库车凹陷白垩纪层序地层格架及古地理演化[J].,占地理学报,2004,6(3)：261-278.
[50]贾进华.塔里木盆地早白垩世沉积相特征与古地理[J].古地理学报，2009，11(2)：167-176.
[51]张泓,晋香兰,李贵红等.鄂尔多斯盆地侏罗纪-白垩纪原始面貌与古地理演化[J].占地理学报,2008,10(1)：1-11.
[52]Ji Qiang, Zhexi Luo and Ji Shu'an. Chinese triconodont mammal and mosaic evolution of the mammalian skeleton [J]. Nature,1999,398:326-330.
[53]邓胜徽,陈芬中.中国东北地区早白垩世真蕨类植物[M].北京：地质出版社,2001.
[54]曹正尧.浙江早白垩世物群[M].北京：科学出版社,1999，174pp.
[55]Zheng S L and Zhou Z Y. A new Mesozoic Ginkgo from western Liaoning, China and its evolutionary significance [J]. Rev. Palaeobot. Palynol.,2004,131:91-103.
[56]Chen P J. Cretaceous paleogeography of China[J]. Palaeogeography, Paleoclimatology, Paleoecology,1987,59:49-56.
[57]Wan X Q, Chen P J, Wei M J. The Cretaceous system in China[J]. Acta Geologica Sinica, 2007,81 (6):957-983.
[58]杨万里松辽陆相盆地石地质[M].北京：石油工业出版社,1985.
[59]王东坡，刘招君,刘立.松辽盆地的演化与海平面升降[M].北京：地质出版社，1992.
[60]陈不基.中国陆相侏罗、白垩系划分对比述评[J].地层学杂志.2000，24(2)：114-119.
[61]郝诒纯,苏德英,余静贤等.中国的白垩系[M].北京：地质出版社,1986.
[62]宋之琛,尚玉珂等.中国孢粉化石(第二卷)：中生代孢粉[M].北京：科学出版社,2000.
[63]何承全,黎文本Parahorologinella gen. nov.——松辽盆地早白垩世孢形体-新属[J].古 生物学报,2004,43(3)：332-337.
[64]李曼英.安徽宣州晚白垩世和古近纪孢粉组合[J].微体古生物学报,2005，22(1)：59-77.
[65]张清波,常英.北京地区大灰厂组孢粉组合及其地质意义[J].北京地质,1994，2：1-7.
[66]常英,张清波.北京西山坨里组孢粉组合及其地层意义[J].北京地质,1994，3：1-9.
[67]江德昕,杨惠秋.朝鲜安州盆地早白垩世孢粉组合[J].植物学报,1996，38(2)：150-155.
[68]刘耕武.川西高原白垩纪孢粉组合的发现及其意义[J].微体古生物学报,1999，16(1)：54-60.
[69]黎文本.从孢粉组合论证松辽盆地泉头组的地质时代及上、下白垩统界线[J].古生物学报,2001,40(2)：153-176.
[70]黄清华,杨建国,孔惠.东北依兰-伊通地堑方正断陷方正组的建立及其意义[J].地层学杂志,2003,27(12)：138-145.
[71]梁诗经,文斐成,陈润生等.福建泰宁白垩纪红层植物及孢粉化石组合特征[J].福建地质,2006,25(1)：1-9.
[72]李建国,杜宝安.甘肃平凉安国镇白垩系六盘山群的孢粉植物群[J].古生物学报,2006,45(4)：498-513.
[73]刘兆生.甘肃玉门早峡早白垩世孢粉组合[J].微体古生物学报.2000，17(3)：73-84.
[74]邵红君,万传彪,任延广等.海拉尔盆地贝16井含油地层划分对比[J].世界地质,2007,26(2)：230-239.
[75]李春柏,万传彪,乔秀云等.海拉尔盆地海参1井伊敏组孢粉组合的地层意义[J].地层学杂志,2007,31(1)：23-34.
[76]宋之琛,我国早白垩世被子植物花粉研究之回顾[J].微体古生物学报,1986，3(4)：373-386
[77]黄嫔,龙文国.海南乐东洪帽剖面鹿母湾组孢粉组合及其地层意义[J].微体古生物学报,2008,25(1)：79-90.
[78]万传彪,乔秀云,孔惠等.黑龙江北安地区早白垩世孢粉组合[J].微体古生物学报,2002,19(1)：83-90.
[79]赵海滨,尹志刚,汪岩等.黑龙江北部嘉荫盆地中南部原划新近系时代的重新厘定.地质通报,2006,25(4)：460-464.
[80]王鑫甫,曹流.黑龙江嘉荫晚白垩世渔亮子组孢粉地层研究[J].微体古生物学报,1999,16(2)：190-194.
[81]尚玉珂.黑龙江省鸡西城子河组被子植物化石层的孢粉研究[J].微体古生物学报,1997,14(2)：161-174.
[82]郑玉龙,刘文龙,乔秀云.黑龙江孙吴-嘉荫盆地白垩纪孢粉组合及地层划分对比[J]地层学杂志,2005,29(4)：342-347.
[83]姜宝玉,冯金宝.鸡西群城子河组时代的进一步探讨[J].地层学杂志,2001，25(3)：217-221.
[84]黄嫔,张光富.吉林延边智新盆地大拉子组孢粉组合[J].微体古生物学报,2002，19(3)：263-275,
[85]黎文本,李建国.吉林榆树榆-302孔阿尔布期孢粉组合[J].古生物学报,2005，44(2)：209-228.
[86]万传彪,刘本培,乔秀云等.嘉荫盆地太平林场组巴尔姆孢(Balmeisporites)的发现及其意义[J].地质学报,2004,78(1)：1-9.
[87]刘耕武,李伟同,张清如等.江汉盆地渔洋组上部的古新世孢粉组合[J].古生物学报,2006,45(1)：60-68.
[88]杨雪英,周山富.江苏淮安地区上白垩统含盐地层孢粉组合序列[J].地层学杂志,2002,26(3)：193-211.
[89]温国强.辽河盆地大民屯凹陷沈249井早白垩世九佛堂组孢粉组合[J].微体古生物学报,2006,23(2)：191-198.
[90]吴炳伟,雷安贵.辽宁铁岭盆地早白垩世孢粉组合[J].微体古生物学报,2007，24(1)89-97.
[91]吴河勇,黄清华,党毅敏等.内蒙古海拉尔盆地白垩纪生物地层研究进展[J].古生物学报,2006,45(2)：283-291.
[92]黄清华,赵来时,卢古武等.内蒙古海拉尔盆地大磨拐河组孢粉化石及其时代浅析[J].地质科技情报,2006,25(1)：19-26.
[93]李凤霞.内蒙古开鲁盆地早白垩世阜新组孢粉组合[J].微体古生物学报,2005，22(1)：87-96.
[94]司双印.李洲,张森宝.山东省白垩系下统孢粉组合及地层意义[J].中国地质,2001，28(6)：21-27.
[95]司双印.山东省大盛群孢粉组合及其年代地层意义[J].地层学杂志,2001，26(2)：126-131.
[96]王家文,常峰.山东郯城王氏组被子植物花粉研究[J].合肥工业大学学报(自然科学版),1997,20(6)：99-102.
[97]尚玉珂,袁德艳.松辽盆地南部梨树凹陷登楼库组孢粉组合[J].微体古生物学报,1995,12(3)：307-321.
[98]万传彪,乔秀云,孔惠等.松辽盆地三站地区营城组孢粉化石的意义[J].大庆石油地质与开发,2002,21(2)：12-14.
[99]乔秀云,孙跃武,万传彪等.孙吴-嘉荫盆地嘉D1井孢粉地层学研究[J].世界地质,2005,24(1)：11-17.
[100]江德昕,王永栋,何卓生等.新疆塔里木拜城地区早白垩世舒善河组孢粉组合[J].微体古生物学报,2007,24(3)：247-260.
[101]江德听,王永栋,何卓生等.新疆塔里木盆地早白垩世克孜勒苏群孢粉组合[J].微体古生物学报,2006,23(4)：371-291.
[102]詹家祯,师天明,周春梅等.新疆准噶尔盆地芳3井晚白垩世孢粉组合的发现及其地质意义[J].微体古生物学报,2007,24(1)：15-27.
[103]张剑,刘洪涛,吴炳伟.彰武盆地张强凹陷早白垩世孢粉组合[J].微体古生物学报,20086,25(2)：196-203.
[104]张光富.中国吉林大拉子组的时代探讨[J].地层学杂志,2005，29(4)：381-388.
[105]张文堂,陈丕基,沈炎彬.中国的叶肢介化石[M].北京：科学出版社,1976，325pp.
[106]Chen P J. Cretaceous conchostracan faunas of China [J]. Cretaceous Research,1994,15: 259-269.
[107]Gang Li, Yanbin Shen, David J. Batten. Yanjiestheria, Yanshania and the development of the Eosestheria conchostracan fauna of the Jehol Biota in China [J]. Cretaceous Research,2007, 28 (2):225-234.
[108]杨静,王志萍,王伟栋.二连盆地西部赛汉塔拉组轮藻化石及其时代意义[J].大庆石油地质与开发,2003,22(3)：19-23.
[109]王启飞,杨景林,卢辉楠.甘肃高台早白垩世下沟组轮藻化石[J].微体古生物学报,2003，20(2)：187-198.
[110]符俊辉,卢辉楠.甘肃花海盆地截大板沟早白垩世轮藻化石[J].古生物学报,1997，36 (3)：350-357.
[111]符俊辉,袁凤钿.甘肃花海盆地早白垩世的介形类[J].古生物学报,1998，37(3)：333-338.
[112]巫建华.江西信江盆地早白至世晚期轮藻及其地层意义[J].微体古生物学报,1995，12(1)：79-87.
[113]彭维松,王启飞,薛铎等.内蒙古银根-额济纳旗盆地白垩纪轮藻化石[J].微体古生物学报,2003,20(4)：365-376.
[114]杨景林,王启飞,卢辉楠.准噶尔盆地白垩纪轮藻化石组合序列[J].微体古生物学报,2008,25(4)：345-363.
[115]姜宝玉,蔡华伟.黑龙江省东部七虎林组中阿普第期的两属异齿类双壳类化石[J].古生物学报,2004,43(2)：112-117.
[116]邢光福,陈荣等.东南沿海晚白垩世火山岩浆活动特征及其构造背景[J].岩石学报.2009,25(1)：77-91.
[117]谢桂青,毛景文等.长江中下游鄂东南地区大寺组或砂岩SHRIMP定年及其意义[J].科学通报.2006,51(19)：2283-2291.
[118]杨经绥,孟繁聪,张建新等.重新认识阿尔金断裂东段红柳峡火山岩的时代及构造意义[J].中国科学,2001,31(增刊)：83-89
[119]唐嘉锋,刘玉琳,王启飞.山东中生代火山岩年代学研究[J].岩石学报,2008，24(6)：1333-1338.
[120]凌文黎,谢先军,柳小明,程建萍.鲁东中生代标准剖面青山群火山岩锆石U-Pb年龄及其构造意义[J1.岩石学报,2006,36(5)：401～411.
[121]杨振宇.高精度地层划分对比的可靠方法——磁性地层学研究[J].地质通报,2002，21(2)：45-47.
[122]Heller F, Evans M E. Loess Magnetism [J]. Reviw Geophysics,1995,33:211-240.
[123]庄忠海、田端孝、马醒华.四川盆地雅安至天全白垩系一下第三系古地磁研究[J].物探与化探,1988,12(3)：224-228.
[124]尹济云,孙知明,杨振宇等.滇西兰坪盆地白垩纪-早第三纪古地磁结果及其地质意义[JJ.地球物理学报,1999,42(5)：648-659.
[125]孟自芳.兰州附近下白垩统河口群中下岩段磁性地层划分[J].地球物理学报,1994，37(增刊)：342-347.
[126]唐玉虎.兰州-民和盆地早白垩世磁性地层年代与青藏高原北部隆升：硕士学位论文.兰州：兰州大学,2008.
[127]戴霜,朱强,胡鸿飞等.六盘山群磁性地层年代[J].地层学杂志,2009,33(2)：188-192.
[128]彭守涛,李忠,黄宝春等.库车坳陷北部白垩系磁性地层划分[J].科学通报.2005，50(19)：2136-2144.
[129]陈丕基.中国侏罗、白垩纪古地理轮廓——兼论长江起源[J]；北京大学学报(自然科学版),1979,3：92-111.
[130]殷鸿福.中国古生物地理学[M].中国地质大学出版社：武汉.1988.
[131]中国地质科学院地质研究所、武汉地质学院,中国古地理图集[M].北京：地图出版社.1985，6：108-119.
[132]杨卫东,陈南生,倪师军,等1白垩纪红层碳酸盐岩和恐龙蛋壳碳氧同位素组成及环境意义[J].科学通报,1993,38(23)：2161～2163.
[133]Yi Yan, Bin Xia, Ge Lin et al. Geochemistry of the sedimentary rocks from the Nanxiong Basin, South China and implications for provenance, paleoenvironment and paleoclimate at
the K/T boundary [J]. Sedimentary Geology,2007,197 (1-2):127-147.
[134]曹珂,李祥辉,王成善.四川盆地白垩系粘土矿物特征及古气候探讨[J].地质学报,2008,82(1)：115-123.
[135]J.Madhavaraju, S. Ramasamy, Alastair Ruffell et al. Clay mineralogy of the Late Cretaceous and early Tertiary successions of the Cauvery Basin (southeastern India):implications for sediment source and palaeoclimates at the K/T boundary [J]. Cretaceous Research,2002,23: 153-163
[136]Bice K L, Birgel D, Meyers P A, et al. A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO_2 concentrations [J]. Paleoceanography,2006, 21(2):PA2002
[137]A. J. Boucot,陈旭,C. R. Scotese,樊隽轩,显生宙全球古气候重建[M].北京：科学出版社,2009.
[138]向芳,宋见春,罗来等.白垩纪早期陆相特殊沉积的分布特征及气候意义[J].地学前缘,2009,16(5)：48-62.
[139]Su-chin Chang, Haichun Zhang, Paul R Renne, Yan Fang. High-precision 40Ar/39Ar age for the Jehol Biota [J]. Palaeogeography, Paleoclimatology, Paleoecology,2009,280:94-104.
[140]Hakuyu Okada. Nature and development of Cretaceous sedimentary basins in East Asia:a review [J]. Geosciences Journal,2000,4 (4):271-282.
[141]曹珂,王猛.沉积记录对白垩纪中国大陆古气候模拟的约束[J].地学前缘,2009，16(5)：29-36.
[142]Scotese. www.scotese.com,2002.
[143]董树文,李廷栋,钟大赉等.侏罗纪／白垩纪之交东亚板块汇聚的研究进展和展望[J].中国科学基金,2009,5：281-286.
[144]董树文,张岳桥,龙长兴等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11)：1449-1461.
[145]Yin A, Nie S. A Phaneozoic palinspastic reconst ruction of China and it s neighboring regions [M]. In:Yin A and Harrison T M (eds). The Tectonic Evolution of Asia. Cambrige University Press,1996:442-485.
[146]Yang Z,Sun Z,Ma X, Huang B,Zhou Y. APWP and tectonic movement s of t he Nort h China Block during t he Phanerozoic [J]. Science in China, Series D,1998,41 (supp.):51-65.
[147]Meng Q R, Hu J M, Jin J Q, et al. Tectonics of the late Mesozoic wide extensional basin system in t he China -Mongolia border region [J]. Basin Research,2003,15:397-415.
[148]陈丕基,E Norling.西藏构造楔与塔里木-华南地块的裂解[J].科学通报,1994，39(16)：1512-1515.
[149]Moores G W. Mesozoic and Cenozoic paleogeographic development of the Pacific region. Abstract,28th International Geological Congress,1988,2-474. Washington D C, USA.
[150]Shigenori Maruyama, Yukio Isozaki, Gaku Kimura et al.. Paleogeographic maps of the Japanese islands:Plate tectonic synthesis from 750Ma to the present [J]. The Island Arc, 1997,6:121-142.
[151]Seno T, Maruyama S. Paleogeographic reconstruction and origin of the Philippine Sea [J]. Tectonophysics,1984,102:53-84.
[152]Maruyama S, Seno T. Orogeny and relative plate motions:example of the Japanese Islands [J]. Tectonophysics,1986,127:305-329.
[153]Uyeda S, Miyashiro A. Plate tectonics and the Japanese Islands:a synthesis [J]. Geological Society of America Bulletin,1974S 85:1159-1170.
[154]Takahashi M. Space-time distribution of Late Mesozoic to Early Cenozoic magmatism in East Asia and its tectonic implications [J]. In:Hashimoto, M. and Uyeda, S. (eds.), Accretion Tectonics in the Circum-Pacific Regions. Terra, Tokyo,1983, p.69-88.
[155]Kinoshita O. A migration model of magmatism explaining a ridge subduction, and its details on a statistical analysis of the granite ages in Cretaceous Southwest Japan [J]. The Island Arc,1999,8:181-189.
[156]Larson R L, Kincaid C. Onset of mid-Cretaceous volcanism by elevation of 670 km thermal boundary layer [J]. Geology,1996,24:551-554.
[157]Okada H. Plume-related sedimentary basins in East Asia during the Cretaceous [J]. Palaeogeography, Palaeoclimatology, Palaeoecology,1999,150:1-11.
[158]Yano T, Wu G Y. Late Mesozoic geodynamics relating Circum-Pacific mobile belt and Darwin Rise [J]. Journal of Geological Society of the Philippines.1997,52:235-271.
[159]马杏垣.1：4,000,000中国及邻近海域岩石圈动力学图[M].北京：地质出版社,1989.
[160]Gilder S A, Keller G R,Luo Ming, Goodell P C. Timing and spatial dist ribution of rifting in China [J]. Tectonophysics,1991,197:225-243.
[161]Ren J Y, Tamaki K, Li Sitian, Zheng J unxia. Late Mesozoic and Cenozoic rifting and it s dynamic setting in eastern China and adjacent areas [J]. Tectonophysics,2002,344:175-205.
[162]Lin Wei,Wang Qingchen. Late Mesozoic extensional tectonics in the North China Block:a crustal response to subcontinental mantle removal [J]? Bull. Geol. Soc. France,2006,117 (6): 287-297.
[163]Liu Junlai, Davis G A, Wu Fuyuan. The Liaonan metamorphic core complex, Southeastern Liaoning Province, North China:a likely cont ributor to Cretaceous rotation of Eastern Liaoning, Korea and contiguous areas [J]. Tectonophysics,2005,407:65-80.
[164]季强,陈文,王五力等.中国辽西中生代热河生物群[M].北京：地质出版社,2004：1-357.
[165]Wong W H. Crust movement in eastern China. Proceedings of 3th Pan-Pacific Science Congress, Tokyo,1926:642-685.
[166]Wong W H. Crustal movement and ignous activities in eastern China since Mesozoic time [J]. Bulletin of Geological Society of China,1927,6 (1):9-36.
[167]Wong W H. The Mesozoic orogenic movement in eastern China [J]. Bulletin of Geological Society of China,1929,8:33-44.
[168]任纪舜,王作勋,陈炳蔚等.中国及邻区大地构造图(1／500万)及简要说明书——从全球看中国大地构造[M].北京：地质出版社,1999：6-9.
[169]崔盛芹,李锦蓉,吴珍汉等.燕山地区中新生代陆内造山[M].北京：地质出版社,2002：1-386.
[170]万天丰.中国大地构造学纲要[M].北京,地质出版社,2004.
[171]赵越,徐刚,张拴红.燕山运动与东亚构造体制的转变[J].地学前缘，2004，11(3)：319-328.
[172]任纪舜,陈廷愚,牛宝贵等.中国东部及邻区大陆岩石圈的构造演化与成矿[M].北京：科学出版社,1990,1-205.
[173]任纪舜,牛宝贵,和政军等,中国东部的构造格局和动力演化[M].任纪舜和杨巍然主编：中国东部岩石圈结构与构造岩浆演化.北京：原子能出版社,1998,1-12.
[174]Niu B G, He Z J,Song B,Xiao W W. SHRIMP geochronology of volcanics of the Zhangjiakou and Yixian Formations, Northern Hebei Province, with a discussion on the age of the Xingpanling Group of the Great Hinggan Mountains and volcanic strata of the southeastern coastal area of China [J]. Acta Geologica Sinica (English Edition),2004, 78:1214-1228.
[175]张旗,钱青,王二七等.燕山中晚期中国东部高原：埃达克岩的启示[J].地质科学,2001,36(2)：248-255.
[176]吴福元,徐义刚,高山,等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报,2008,24：1145-1174
[177]姜耀辉,蒋少涌,赵葵东,等.辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约[J].科学通报,2005，50：2161-2168
[178]徐义刚,李洪颜,庞崇进,等.论华北克拉通破坏的时限[J].科学通报,2009，54：1974-1989
[179]Zhou Xinhua, Yang Jinhui, Zhang Lianchang. Metallogenesis of superlarge gold deposit s in Jiaodong region and deep processes of subcontinental lithosphere beneath north China craton in Mesozoic [J]. Science in China (series D),2002,32 (suppl.):11-20.
[180]吴福元,葛文春,孙德有等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,10(3)：51-60
[181]Wu Fuyuan, Lin Jingqian, Wilde S A et al. Nature and significance of the Early Cretaceous giantigneous event in eastern China [J]. Earth Planet Science Letter,2005,233:103-119.
[182]徐贵忠,周瑞,闫臻等.论胶东地区中生代岩石圈减薄的证据及其动力学机制[J].大地构造与成矿学,2001,25(4)：368-380.
[183]张岳桥,李金良,张田等.胶莱盆地及其邻区白垩纪-古近世沉积构造演化历史及其区域动力学意义[J].地质学报,2008,82(9)：1229-257.
[184]Mao Jingwen, Wang Yitian, Zhang Zuoheng, et al. Geodynamic settings of Mesozoic large-scale mineralization in North China and adjacent areas:Implication from the highly precise and accurate ages of metal deposits [J]. Science in China (series D),2003,46 (8): 838-851.
[185]Chen Jiangfeng, Xie Zhen, Li Huimin, et al. U-Pb zircon ages for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrain, China [J]. Geochemical Journal, 2003,37(1):35-46.
[186]郭敬辉,陈福坤,张晓曼等.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞一.碰撞后构造过程：锆石U-Pb年代学[J].岩石学报,2005,21(4)：1281-1301.
[187]陈毓川,常印佛,裴荣富等.中国成矿体系与区域成矿评价[M].北京：地质出版社,2007.
[188]万桂梅,汤良杰,金文正等.郯庐断裂带研究进展及存在问题探讨[J].地质论评,2009,55(2)：251-259.
[189]Yin An, Nie Sh Y. An indentation model for t he north and south China collision and the development of the Tanlu and Honam fault system, eastern Asia [J]. Tectonics,1993,12 (4): 801-813.
[190]Fletcher C J N, Fitches W R, Rundle C C et al. Geological and isotopic constraints on the timing of the movements in the Tan-Lu fault zone [J]. Journal of Southeast Asian Earth Science,1995,11:15-22.
[191]Ross J V, Mercier J C, Xu Y G. Diffusion creep in the upper mantle:an example from the
Tan-Lu Fault, nort heastern China [J]. Tectonophysics,1996,261:315-329.
[192]Gilder S A, Leloup P H, Courtiliot V, et al. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via middle Triassic to early Cenozoic paleomagnetic data [J]. Journal of the Geophysical Research,1999,104 (B7):15365-15390.
[193]Rat schbacher L, Hacker B R, Webb L E, et al. Exhumation of ultra-high pressure continental crust in east central China:Cretaceous and Cenozoic unroofing and the Tan-Lu fault [J]. Journal of the Geophysical Research,2000,105 (B6):13303-13338.
[194]Li Jianwei, Zhou Meifu, Li Xianfu, et al. The Hunan-Jiangxi strike-slip fault system in southern China:southern termination of the Tan-Lu fault [J]. Journal of Geodynamics,2001, 32:333-354.
[195]Zhang Yueqiao, Dong Shuwen, Shi Wei. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province, eastern China [J]. Tectonophysics,2003,363: 243-258.
[196]Zhu Guang, Wang Yongsheng, Liu Guosheng, et al.~(40)Ar/~(39)Ar dating of strike-slip motion on t he Tan-Lu fault zone, East China [J]. Journal of Structural Geology,2005,27: 1379-1398.
[197]徐嘉炜,马国锋.郯庐断裂研究的十年回顾[J].地质论评,1992,38(4)：316-324.
[198]罗志立,李景明,李小军等.试论郯城—庐江断裂带形成、演化及问题[J].吉林大学学报(地球科学版),2005,35(6)：699-706.
[199]张用夏,李卢玲.郯庐断裂带的平移及其对邻区构造的影响[J].构造地质论丛(3).北京：地质出版社,1984：1-8.
[200]朱光,牛漫兰,宋传中等.郯庐断裂带新生代的上地幔剪切作用与火山活动[J].安徽地质,2001,11(2)：106-112.
[201]万天丰.郯庐断裂带的演化与古应力场[J].地球科学,1995：526-534.
[202]万天丰,朱鸿.郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报,1996,2(1)：14-27.
[203]Mercier J L, Hou Minjing, Vergely P, et al. Structural and stratigraphical constraints on the kinematics history of the Southern Tan-Lu Fault Zone during the Mesozoic Anhui Province, China [J]. Tectonophysics,2007,439:33-66.
[204]陈宣华,王小凤,张青等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000,30(3)：215-220.
[205]徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995，10(2)：121-132.
[206]朱光,刘国生,牛漫兰等.郯庐断裂带的平移运动与成因[J].地质通报,2003，22(3)：200-207.
[207]汤加富,许卫.郯庐断裂带南段并无巨大平移——来自安徽境内的证据[J].地质论评,2002,48(5)：449-456.
[208]劳秋元.郑庐断裂带前古生代、古生代的形成演化间题[M].见：《构造地质论丛(3)》北京：地质出版社,1984：80-93.
[209]陈不基.郯庐断裂巨大平移的时代与格局[J].科学通报,1988,33(4)：289-293.
[210]翁世劫.关于郑庐断裂带的几个地质问题[M].见：《构造地质论丛(3)》.北京：地质出版社,1984：66-71.
[211]郭振一.沂沐断裂带的基本特征及其活动方式[M].见：《构造地质论丛(3)》.北京：地质出版社,1984：142-151.
[212]吴根耀,马力,梁兴等.从郯庐断裂带两侧的”盆”“山”耦合演化看前白垩纪“郯庐断裂带”的性质[J].地质通报,2008,27(3)：308-325.
[213]朱光,徐嘉炜,孙世群.郯庐断裂带平移时代的同位素年龄证据[J].地质论评,1995,41(5)：452-456.
[214]王勇生,朱光,胡召齐等.郯庐断裂带沂沭段伸展活动断层泥K-Ar同位素定年[J].中国科学(D),2009,52(4)：489-503,
[215]Wang Pujun, Xie Xiao'an, Mattern Frank et al. The Cretaceous Songliao Basin: volcanogenic succession, sedimentary sequence and Tectonic evolution, NE China [J]. Acta geologica sinica,2007,81 (6):1002-1011.
[216]和钟铧,刘招君,陈秀艳等.黑龙江省东部残留盆地群早白垩世沉积相特征及演化[J].古地理学报,2008,10(2)：151-158.
[217]张世红,张传恒,李红生.黑龙江省东部裴德组砾石中放射虫的发现及其意义[J].地层学杂志,1999,23(3)：201-205.
[218]孙革,郑少林,姜剑红,等.黑龙江鸡西含煤盆地早白垩世生物地层研究新进展[J].煤田地质与勘探,1999,27(6)：1-3.
[219]姜宝玉.黑龙江省东部七虎林组的一些双壳类化石[J].动物学杂志,2003，38(4)85-100.
[220]杨建国,赵传本.黑龙江省龙爪沟地区侏罗系研究新进展[J].大庆石油地质与开发,1998,17(6)：16-18.
[221]孙革,郑少林.中国东北中生代地层划分对比之新见[J].地层学杂志,2000，24(1)：60-64.
[222]杨小菊,何承全,黎文本,等.鸡西盆地早白垩世穆棱组海相沟鞭藻的发现及其古环境意义[J].科学通报,2003,48(14)：1553-1556.
[223]程金辉,何承全.黑龙江省东部鸡西盆地早白垩世滴道组的沟鞭藻类[J].古生物学杂志,2001,40(1)：127-133.
[224]Kellys R A, Wang Yigang, ZhengLin. A revised Cretaceous age for ammonites, originally identified as Middle Jurassic, from eastern Hei longjiang, China [J]. Acta Palaeontologica Sinica,1994,33 (4):509-517.
[225]Futakami M, Matsukawa M, Chen Piji, et al. Barremian ammonite from the Longzhaogou Group in eastern Heilongjiang, northeast China [J]. The Journal of the Geological Society of Japan,1995,101 (1):79-85.
[226]沙金庚.黑龙江东部早白垩世生物地层学研究的主要进展[J].地学前缘,2002，9(3)：95-101.
[227]潘华璋,朱祥根.黑龙江省东部早白垩世的一些海相和半咸水相腹足类[J].古生物学报,2004,43 (3):338-348.
[228]万传彪,闫风兰,尹楠.黑龙江集贤地区早白垩世沟鞭藻类和其他藻类[J].微体古生物学报,1995,12(1):51-52.
[229]陈义贤,陈文寄.辽西及邻区中生代火山岩——年代学、地球化学和构造背景[J].北京：地震出版社,1997,106-163
[230]景山.冀北-辽西地区早白垩世义县组沉积环境及其与盆地演化的关系：[硕士学位论文].北京：中国地质大学(北京),2008.
[231]柳永清,田树刚,庞其清.滦平盆地大北沟组-大店子组沉积和地层格架及陆相层型意义[J].地球学报,2001,22 (5):391-396
[232]柳永清,庞其清,李佩贤.冀北滦平陆相侏罗-白垩系生物地层界线及候选层型研究进 展[J].地质通报,2002,21(3)：176-180
[233]季强,论热河生物群[J].地质论评,2002,48(3)：290-296
[234]季强,陈文,王五力等.中国辽西中生代热河生物群[M].北京：地质出版社,2004.
[235]王璞珺,杜小弟,王东坡.松辽盆地白垩纪湖侵沉积层序与湖海沟通事件的地球化学记录[J].岩相古地理,1995,15(4)：14-20
[236]贾军涛,王璞珺,张斌等.哈尔滨东宾县凹陷白垩纪地层层序及其与松辽盆地的对比[J].地质通报,2006,25(9-10)：1143-1151.
[237]樊馥,蔡进功,高福红.孙吴—嘉荫盆地太平林场组烃源岩海侵特征研究[J].沉积学报,2009,27(4)：650-656.
[238]章凤奇,陈汉林,董传万等.松辽盆地北部火山岩锆石SHRIMP测年与营城组时代探讨[J].地层学杂志,2008,32(1)：15-20.
[239]丁日新,舒萍,曲延明等.松辽盆地庆深气田储层火山岩锆石U-Pb同位素年龄及其地质意义[J].吉林大学学报(地球科学版),37(3)：525-530.
[240]舒萍,丁日新,纪学雁等.松辽盆地庆深气田储层火山岩锆石地质年代学研究[J].岩石矿物学杂志,2007,26(3)：239-346.
[241]王璞珺,高有峰,任延广等.松辽盆地青山口组橄榄粗安岩~(40)Ar/~(39)Ar年龄、地球化学及其成盆、成烃和成藏意义[J].岩石学报,2009,25(5)：1178-1190.
[242]叶得泉,钟筱春,石宝珩等.中国北方含油气区白垩系[M].北京：石油工业出版社,1990.
[243]赵传本，叶得泉,魏德恩等.中国油气区第三系(Ⅲ)——东北油气区分册[M].北京：石油工业出版社,1990.
[244]Swisher C C,汪筱林,周忠和等.义县组同位素年代新证据及土城子组~(40)Ar/~(39)Ar年龄测定[J].科学通报,2001,46(23)：2009-2012.
[245]杨进辉,吴福元,邵济安等.冀北张-宣地区后城组、张家口组火山岩锆石U-Pb年龄和Hf同位素[J].地球科学,2006,31(1)：71-80.
[246]张宏,王明新,柳小明LA-ICP-MS测年对辽西-冀北地区髫髻山组火山岩上限年龄的限定[J].科学通报,2008,53(15)：1815-1824.
[247]张宏,柳小明,张哗卿等.冀北滦平-辽西凌源地区张家口组火山岩顶、底的单颗粒锆石U-Pb测年及意义[J].地球科学——中国地质大学学报,2005，30：387-401.
[248]Cope T C. Sedimentary Evolution of the Yanshan Fold-thrust Belt, Northeast China [J]. Califonia:Stanford Uni,2003.1-230.
[249]张宏,柳小明,高山等.辽西凌源地区张家口组的重新厘定及其意义——来自激光ICP-MS锆石U-Pb年龄的制约[J].地质通报,2005,24(2)：110-117.
[250]李佩贤,程政武,庞其清.辽西北票孔子鸟Confuciusornis的层位及年代[J].地质学报,2001,75(1)：1-13.
[251]张宏,柳小明,袁洪林等.辽西凌源地区义县组下部层位的U-Pb测年及意义[J].地质评论,2006,52(1)：63-71.
[252]Swisher C C, Wang Y Q, Wang X L, et al. Cretaceous age of thefeathered dinosaurs of Liaoning, China [J]. Nature,1999,400:58-61.
[253]朱日祥,邵济安,潘永信等.辽西自垩纪火山岩古地磁测定与陆内旋转运动[J].科学通报,2002,47(17)：1335-1440.
[254]Zhu R X, Pan YX, Shaw J, et al. Geomagnetic palaeointensity just prior to the Cretaceous normal superchron [J]. Physics of the earth and planetary interiors,2001,128 (1-4):207-222
[255]王清利,陈文,张彦.辽西喀左县孤山义县组安山岩激光~(40)Ar/~(39)Ar和锆石SHRIMP U-Pb年龄及其地质意义[J].地质论评,2008,54(1)：125-133.
[256]陈文,张彦,季强等.2005.四合屯珍稀化石层的时代一一39Ar/40 Ar和SHRIMPU-Pb年龄新证据[J].地层学杂志,29：582～588.
[257]孟凡雪,高山,柳小明.辽西凌源地区义县组火山岩锆石U-Pb年代学和地球化学特征[J].地质通报,2008,27(3)：364-373.
[258]王松山,胡华光,李佩贤等.再讨论辽西四合屯脊椎动物生存时代Ar-Ar年龄证据[J].岩石学报,2001,17(4)：663-668.
[259]汪方跃,高山,牛宝贵等.河北承德盆地114 Ma大北沟组玄武岩地球化学及其对华北克拉通岩石圈地幔减薄作用的制约[J].地学前缘,2007，14(2)：98-108.
[260]Zhang H, Wang M X, Liu XW. LA-ICP-MS dating of Zhangjiakou formation volcanic rocks in the Zhangjiakou region and its geological significance [J]. Progress in Nature Science,2008,18 (8):975-982.
[261]牛宝贵,和政军,宋彪等.张家口组火山岩SHRIMP定年及其重大意义[J].地质通报,I2003,22(2)：140-141.
[262]柳永清,李佩贤,田树刚等.冀北滦平晚中生代火山碎屑(熔)岩中锆石SHRIMP U-Pb年龄及其地质意义[J].岩石矿物学杂志,2003，22(3)：237-244.
[263]孙立新,赵风清,王惠初等.燕山地区土城子组划分、时代与盆地性质探讨[J].地质学报；2007,81(4)：445-454.
[264]韦忠良,张宏,柳小明等.张家口地区张家口组火山岩的LA-ICP-MS测年及其地质意义[J].自然科学进展,2008,18(5)：523-530.
[265]贾军涛,王璞珺,万晓樵.松辽盆地断陷期白垩纪营城组的时代归属.地质论评,2008,54(4)：439-448.
[266]赵重远.鄂尔多斯盆地的演化历史、形成机制和含油气有利地区[M]／／赵重远.华北克拉通沉积盆地形成与演化及油气赋存.西安：西北大学出版社,1990.
[267]李向平,陈刚,章辉若等.鄂尔多斯盆地中生代构造事件及其沉积响应特点[J]。西安石油大学学报(自然科学版),2006，21(3)：1-5.
[268]张泓,晋香兰,李贵红,杨志远,张慧,贾建称.鄂尔多斯盆地侏罗纪一白垩纪原始面貌与古地理演化.古地理学报,2008，10(1)：1-11.
[269]江新胜、潘忠习.中国白垩纪沙漠及气候[M].北京：地质出版社,2005.
[270]江新胜,潘习忠.白垩纪时期东亚大气环流格局初探[J].中国科学(D辑),2000，30(5)：587-591.
[271]吴仁贵,余达淦,周万蓬等.鄂尔多斯盆地北部早白垩世地层特征及对比[J].地层学杂志,2005,29(1)：50-54.
[272]齐骅.宁夏固原六盘山群下部的介形类化石[J].地层古生物论文集,1987，18：74-147.
[273]齐骅.宁夏固原六盘：山群上部的介形类化石[J].地层古生物论文集,1988，22：85-127.
[274]李祖望.平凉安国镇六盘山群介形类[J].甘肃地质学报,1995，4(2)：10-21.
[275]蔡雄飞,李长安,朱伟元等.兰州-民和盆地红古城组的建立及其地质学意义[J].甘肃地质学报,1998,7(2)：49-53.
[276]蔡雄飞,李长安,占车生等.民和盆地南缘盐锅峡组的建立及其地质意义[J].岩相古地理,1999,19(3)：16-20.
[277]蔡雄飞,顾延生,李长安.兰州-民和盆地恐龙足印化石形成的地质特征[J].地层学杂志,2005,29(3)：306-309.
[278]吉利明民和盆地早白坚世晚期的抱粉组合[J].植物学报.1995，37(7)：566-573.
[279]何光玉,杨树锋,陈汉林等.河西走廊西段及邻区早白垩世盆地的重新厘定[J].石油
学报,2004,25(6)：18-22.
[280]李奋其.酒泉盆地形成机制与演化：博士学位论文.成都：成都理工大学,2004.
[281]胡艳霞.甘肃玉门红柳峡早白垩世下沟组的介形类[J].微体古生物学报.2004，21(4)：439-455.
[282]胡艳霞,徐东来.甘肃玉门下沟地区早白垩世下沟组介形类[J].微体古生物学报.2005,22(2)：173-184.
[283]邓胜徽,卢远征.甘肃酒泉盆地早白垩世植物化石及其古气候意义[J].地质学报,2008,82(1)：104-116
[284]卫平生,张虎权,陈启林等.银根-额济纳旗盆地下白垩统银根组的确立[J].地层学杂志,2007,31(2)：184-189.
[285]吴少波,白玉宝,刘勇等.银根盆地苏红图组火山岩特征及其与油气的关系[J].西安石油学院学报,1998,13(6)：8-11.
[286]吴少波,白玉宝.银根盆地早白垩世火山岩特征及形成大地构造环境[J].矿物岩石,1999,32(4)：24-28.
[287]付国斌,李罡,任玉光等.内蒙古呼伦陶勒盖下白垩统巴音戈壁组的叶肢介化石[J].古生物学报,2007,46(2)：244-248.
[288]吴仁贵,周万蓬,刘平华.关于内蒙古巴音戈壁盆地早白垩世地层的讨论[J].地层学杂志,2009,33(1)：87-90.
[289]郭彦如,刘全新,樊太等.查干断陷湖盆层序地层框架中的含油气系统[M].北京：地质出版社,2003.
[290]郭宪璞，叶留生,李汉敏等.塔里木盆地白垩纪地层对比及格架[J].中国西部油气地质,2006,2(2)：140-146.
[291]苏新,郭宪璞,丁孝忠.塔里木北部库车前陆盆地晚白垩世和古新世的钙质超微化石组合[J].现代地质,2003,17(4)：370-377.
[292]和钟铧,刘招君,郭巍等.柴达木北缘中生代盆地的成因类型及构造沉积演化.吉林大学学报(地球科学版),2002,32(4)：333-339.
[293]郑秀亮,商华.介形类化石Cypridea (Pseudocypridina) gigantea的地层及环境意义[J].新疆石油地质,2007,28(1)：64-66.
[294]杨景林,王启飞,卢辉楠.准噶尔盆地南缘呼2井晚白垩世、古新世轮藻植物群的发现及其意义[J].微体古生物学报,2005,22(3)：251-268.
[295]李伟.渤海湾盆地区中生代盆地演化与前第三系油气勘探：博士学位论文.东营：石油大学,2007.
[296]张增奇,刘明渭.山东省岩石地层[M].武汉：中国地质大学出版社,1996.
[297]刘明渭,张庆玉,宋万千.山东省白垩纪岩石地层序列与火山岩系地层划分[J].地层学杂志,2003,27(3)：248-254.
[298]李浩敏.安徽五河下白垩统被子植物叶化石[J].科学通报,2003，48(4)：375-378.
[299]吴海权,江来利,戴圣潜.安徽霍山-毛坦厂地区中生代地层层序的厘定[J].地层学杂志,2002,26(1)：39-45.
[300]韩树棻,杨有根,朱彬等.安徽北部中、新生代沉积盆地分析[J].安徽地质,1994，4(3)：27-35.
[301]王岳军,范蔚茗,郭锋等.北大别晚中生代火山岩的地球化学特征及对北大别构造属性的启示[J].地学前缘,2003,10(4)：529-538.
[302]王岳军,范蔚茗,郭锋.北淮阳晚中生代火山岩定年及火山砾石地球化学：对大别灰色片麻岩隆升和中生代地层格架的约束[J].科学通报,2002,47(20)：1528-1534.
[303]牛漫兰,朱光,宋传中.郯庐断裂带中生代火山活动与深部过程[J].合肥工业大学学报(自然科学版),2001,24(2)：147-153.
[304]闫峻,刘海泉,宋传中等.长江中下游繁昌-宁芜火山盆地火山岩锆石U-Pb年代学及其地质意义[J].科学通报,2009,54(12)：1716-1724.
[305]张旗,简平,刘敦一等.宁芜火山岩的锆石SHRIMP定年及其意义[J].中国科学(D辑),2003，33(4)：309-314.
[306]张春彬.江苏句容早白垩世孢粉组合[J].古生物学报,1962,10(2)：246-286
[307]宋之琛,郑亚惠,刘金陵等.江苏地区白垩纪一第三纪孢粉组合[M].北京：地质出版社,1981.
[308]张一勇,李建国.江苏白垩纪孢粉组合序列[J].地层学杂志,2000，24(1)：65-71.
[309]周山富,王伟铭.江苏句容白垩纪葛村组花粉-新属及其地史分布[J].古生物学报,2001,40(4)：457-462.
[310]傅强,李益,张国栋等.苏北盆地晚白垩世-古新世海侵湖泊的证据及其地质意义[J].沉积学报,2007,25(3)：380-385.
[311]邢立达；王丰平；潘世刚等.重庆綦江中白垩统夹关组恐龙足迹群的发现及其意义[J].地质学报,2007,81(11)：1591-1604
[312]雷奕振.长江三峡地区生物地层学——白垩纪、第三纪分册[M].北京：地质出版社，1987.
[313]李伟同.中国当阳跑马岗组白垩-古近系界线附近的轮藻组合[J].微体古生物学报,2003,20(2)：183-186.
[314]俞云文,徐步台.浙江中生代晚期火山-沉积岩系层序和时代[J].地学前缘,1999，23(2)：136-145.
[315]张万良,李子颖.相山“流纹英安岩”单颗粒锆石U-Pb年龄及地质意义[J].岩石矿物学杂志,2007,26(1)：21-26.
[316]张家菁,施光海,童贵生等.浙江徐家墩鹅湖岭组含铜多金属矿火山岩的地球化学与年代学[J].地质学报,1999,83(6)：791-799.
[317]张利民.试论我国东部火山岩型铀矿床赋存层位的地质时代[J].铀矿地质,1996，12(3)：139-143.
[318]张万良.盛源盆地火山岩系地层的时代归属[J].铀矿地质,2000,16(2)：99-101.
[319]王勇,管太阳,黄国夫等.赣东北地区燕山晚期火山岩同位素年代学研究[J].地球学报,2002,23(3)：233-236.
[320]李坤英,沈加林,王小平.浙闽赣中生代陆相火山岩同位素年代学[J].中国地质科学院南京地质矿产研究所所刊,1989,(增刊)：87-132.
[321]张利民.江西中生代火山岩系地层划分及时代刍议[J].华东地质学院学报,1990，13(2)：9-14.
[322]余达淦,艾桂根等.江西周潭群同位素年龄特征及其地质意义[J].地球学报,1999,20(2)：195-200.
[323]梁诗经,文斐成,陈润生等.福建泰宁白垩纪红层植物及孢粉化石组合特征[J].福建地质,2006,25(1)：1-9.
[324]巫建华,张树明,周维勋.赣南-粤北版石群及其地质时代[J].地层学杂志,1999,23(3)：226-233.
[325]宋之琛,王鑫甫,钟林.三水盆地早白垩世白鹤洞组的被子植物花粉[J].古生物学报,1992,31(4)：501-512
[326]Miall A D. Architectural element analysis:a new method of facies analysis applied to fluvial deposits [J]. Earth-Science Review,1985,22:261-308.
[327]刘朋波,蒲仁海,刘娟霞.十屋断陷火石岭组-营城组沉积微相研究与储层识别[J].石油地球物理勘探,2009,44(3)：347-356.
[328]程日辉,刘万洙,王璞珺等.松辽盆地东缘下白垩统营城组二段火山碎屑沉积的过程、相和结构[J].吉林大学学报(地球科学版),2007,37(6)：1166-1175.
[329]郭峰,陈世悦,胡光明等.松辽盆地北部下白垩统地震相及沉积相分析[J].大庆石油地质与开发,2005,24(6)：20-24.
[330]王国栋,程日辉,王璞珺等.松科1井南孔白垩系泉头组沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：324-338.
[331]高有峰,王璞珺,程日辉等.松科1井南孔白垩系青山口组一段沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：314-323.
[332]王璞珺,高有峰,程日辉等.松科1井南孔白垩系青山口组二、三段沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：288-313.
[333]程日辉,王国栋,王璞珺等.松科1井南孔白垩系姚家组沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：272-287.
[334]韩建辉,王英民,李树青等.松辽盆地北部湖盆萎缩期层序结构与沉积充填[J].沉积学报.2009,27(3)：479-486
[335]邢德和,孙春林,孙跃武等.辽西金-羊盆地士城子组层序地层学[J].地质与资源,2006,15(3)：166-173.
[336]靳卫广,梅冥相.库车盆地白垩纪沙漠沉积体系的层序地层格架[J].断块油气田,2005,12(5)：17-20.
[337]程宏岗.楚雄中生代盆地原始盆地恢复及其演化：硕士学位论文.西安：西北大学,2004.
[338]李正芳.中扬子区晚侏罗世和白垩纪沉积古地理研究：硕士学位论文.北京：中国地质大学(北京),2009.
[339]李金良.胶莱盆地沉积分析及构造演化：博士学位论文.北京：中国地质科学院,2006.
[340]岳文浙,丁保良.江苏白垩纪陆相层序地层研究[J].资源调查与环境,1999，20(4)：287-344.
[341]白云风,程日辉,孔庆莹等.下扬子地区晚白垩世浦口期沉积古地理及地质背景[J].吉林大学学报(地球科学版),2007,37(4)：684-689.
[342]任红民,陈丽琼,王文军等.苏北盆地晚白垩世泰州期原型盆地恢复[J].石油实验地质,2008,30(1)：52-57.
[343]李思田,路风香,林畅松等.中国东部及临区中、新生代盆地演化及地球动力学背景[M].武汉：中国地质大学出版社,1997.
[344]Olsen, P E. Tectonic, climatic, and biotic modulation of lacustrine ecosystems-examples from Newark supergroup of Eastern North America. Lacustrine Basin Exploration:Case studies and modern analogs [J]. AAPG Memoir,1990,50,209-224.
[345]Carroll A R. Stratigraphic classification of ancient lakes Balancing tectonic and climatic controls [J]. Geology,1999,27 (2):99-102.
[346]Carroll A R. Lake-type controls on petroleum source rock potential in nonmarine basins. AAPG Bulletin [J],2001,85(6):1033-1053.
[347]Bohacs K M, Carroll A R. Lake-Basin type, source potential, and hydrocarbon character:an integrated sequence-stratigraphic geochemical framework [J]. AAPG Studies in Geology, 2000,46:3-34.
[348]A S Cohen. Paleolimnology:the History and Evolution of Lake Systerms [J]. M. New York, Oxford University Press,2003,211-213.
[349]殷洪福.中国古生物地理学[M].中国地质大学出版社：武汉.1988，250-270.
[350]陈丕基,云南中生代红层[M].科学出版社：北京.1975，31-48.
[351]Sha J G, Hiromichi H, Yao X G, et al. Late Mesozoic transgressions of eastern Heilongjiang and their significance in tectonics, and coal and oil accumulation in northeast China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2008,263 (3-4):119-130.
[352]葛肖虹,马文璞.东北亚南区中-新生代大地构造轮廓[J].中国地质,2007，34(2)：212-228.
[353]Sha Jingeng. Cretaceous stratigraphy of northeast China:non-marine and marine correlation [J]. Cretaceous research,2007,28:146-170.
[354]祝幼华,何承全.黑龙江省东部中侏罗世至早白垩世沟鞭藻组合序列[J].地层学杂志,2003,27(4)：282-289.
[355]何承全,孙学坤.黑龙江省东部鸡西盆地城子河组下部早白垩世欧特里夫晚期海相沟鞭藻类[J].古生物学报,2000,39(1)：46-62.
[356]Sha J G, Matsukawa M, Cai H W et al. The Upper Jurassic-Lower Cretaceous of eastern Heilongjiang, northeast China:stratigraphy and regional basin history[J]. Cretaceous research, 2003,24:715-728.
[357]Jiang B Y, Cai H W, Sha J G. Early Cretaceous Aucellina (bivalvia) from the Dajiashan area, northeastern China[J]. Journal of Asian Earth Sciences,2004,23:365-371.
[358]张松海,程立人,刘典涛.胶南地区莱阳群绒枝藻化石的发现[J].长春科技大学学报,2001,31(3)：209-212.
[359]李玉文.四川盆地白垩纪半咸水有孔虫和介形虫的发现及其意义[J].地质论评,1979,25(1)：2-11.
[360]Okada H. High sea-level vs. high sedimentation rates during the Cretaceous [J]. Geological Society of Japan Memoirs,1997,48,1-6.
[361]冯晓杰,张川燕,王春修等.东海陆架和台西南盆地中生界及其油气勘探潜力[J].中国海上油气(地质),2001,15(5)：306-311.
[362]郑绵平,赵元艺,刘俊英.第四纪盐湖沉积与古气候[J].第四纪研究,1998，4：297-307.
[363]Yaalon D H, Ward G D. Observations on calcrete and Recent calcic horizons in relation to landforms, central Namib Desert [J]. Palaeoecology of Africa and of the Surrounding Islands and Antarctica,1982,15:183-186.
[364]Glennie K W. Desert sedimentary environments, present and past [J]. Sedimentary Geology, 1987,50(1-3):135-165.
[365]江新胜,蔡习尧,潘忠习等.塔里木盆地西南部早白垩世风成沙丘古风向测量与古风带恢复[J].沉积与特提斯地质,2009,29(4)：1-4.
[366]江新胜,潘忠习,徐金沙等.江西信江盆地晚白垩世风成沙丘的发现及其古风向[J].地质通报,2006,25(7)：833-838.
[367]M Matsukawa, K Saiki, M Ito et al. Early Cretaceous terrestrial ecosystems in East Asia based on food-web and energy-flow models [J]. Cretaceous Research,2006,27:285-307.
[368]张旗,王元龙,金惟俊等.晚中生代的中国东部高原：证据、问题和启示[J].地质通报,2008,27(9)：1404-1430.
[369]邵济安,张履桥,肖庆辉,等.中生代大兴安岭的隆起：一种可能的陆内造山机制[J].岩石学报,2005,21(3)：789-794.
[370]刘训.中国西北盆山地区中-新生代古地理及地壳构造演化[J].古地理学报,2004，6(4)：448-458.
[371]李伍平,李献华.燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报,2004,20(3)：501-510.
[372]Hendrix M, Graham S, Caxroll A et al. Sedimentary record and climatic implication of recurrent deformation in the Tianshan:evidence from Mesozoic strata of the north Tarim, south Junggar, and Turpan basins, northwest China[J]. Geological Society of Ameriea Bulletin,1992,104(1):53-79
[373]Graham S, Hendrix M, Wang Z et al. Collisional successor basins of western China:impact of tectonic inheritance on sand composition [J]. Geological Society of America Bulletin, 1993,105 (3):323-344.
[374]吴根耀.白垩纪：中国及邻区板块构造演化的一个重要变换期[J].中国地质,2006，33(1)：64-77.
[375]袁四化,刘永江,葛肖虹等.阿尔金山中新生代隆升历史研究进展[J].世界地质,2006,25(2)：164-171.
[376]郑德文,张培震,万景林等.西秦岭北缘中生代构造活动的~(40)Ar/~(39)Ar、FT热年代学证据[J].岩石学报,2004，20(3)：697-706.
[377]唐玉虎,戴霜,黄永波等.兰州-民和盆地河口群沉积相和岩石磁化率——祁连山白垩纪隆升的记录[J].地学前缘,2008,15(2)：261-271.
[378]陈正乐,李丽,刘健等,西天山隆升-剥露过程初步研究[J].岩石学报,2008，24(4)：625-636.
[379]张传恒,刘典波,张传林等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1)：294-302.
[380]沈传波,梅廉夫,徐振平等.大巴山中-新生代隆升的裂变径迹证据[J].岩石学报,2007,23(11)：2901-2910.
[381]赵红格,刘池洋,王锋等.贺兰山隆升时限及其演化[J]中国科学(D辑),2007,37(增刊)：185-192.
[382]吴中海,吴珍汉.大青山晚白垩世以来的隆升历史[J].地球学报,2003，24(3)：205-210.
[383]郑德文,张培震,万景林等.六盘山盆地热历史的裂变径迹证据[J].地球物理学报,2005,48(1)：157-164.
[384]陈正乐,万景林,刘健等.西天山山脉多期次隆升-剥露的裂变径迹证据[J].地球学报,2006,27(2)：97-106.
[385]彭兆蒙,彭仕宓,吴智平等.华北东部侏罗-白垩纪盆地演化及其对构造运动的响应[J].西安石油大学学报(自然科学版).2009，24(5)：7-13.
[386]李小明,王岳军,谭凯旋等.云开地块中新生代隆升剥露作用的裂变径迹研究[J].科学通报,50(6)：577-583.
[2]马宗晋,杜品仁,卢苗安.地球的多圈层相互作用[J].地学前缘,2001，8：3-8.
[3]Larson R L. Latest pulse of the Earth:Evidence for a mid-Cretaceous superplume [J]. Geology, 1991,19:547-550.
[4]Kaiho K, Saito S. Oceanic crust production and climate during the past 100 Myr [J]. Terra Nova,1994,6:376-384.
[5]Schlanger S O, Jenkyns H C. Cretaceous oceanic anoxic events:Cause and consequence [J]. Geologie en Mijinbouw,1976,55:179-184.
[6]王成善,胡修棉.白垩纪世界与大洋红层[J].地学前缘,2005,12(2)：11-21.
[7]Wang C S, Hu X M, et al. Upper Cretaceous oceanic red beds in southern Tibet:A major change from anoxic to oxic, deep-sea environments [J]. Cretaceous Research,2005,26: 21-32.
[8]Hu X M, Luba J, Wang C S, et al. Upper Cretaceous oceanic red beds (CORBs) in the Tethys: occurrences, lithofacies, age and environments [J]. Cretaceous Research,2005,26:3-20.
[9]Leckie R M, Bralower T J, Cashman R. Oceanic anoxic events and plankon evolution:biotic response to tectonic forcing during the mid-Cretaceous [J]. Paleoceanography,2002,17 (3): 1041. doi:10.1029/2001PA000623.
[10]Cronin M, Tauxe L, Constable C, et al. Noise in the quite zone [J]. Earth and Planetary Science Letters,2001,190:13-30.
[11]史瑞萍,朱日祥.白垩纪地球物理场异常与地球深部动力学[J].地球物理学进展,2002,17(2)：295-300.
[12]Zhao X X. The Earth's magnetic field and global geologic phenomena in Mid-Cretaceous [J]. Earth Science Frontiers,2005,12 (2):199-216.
[13]王成善,曹珂等.沉积记录与白垩纪地球表层系统变化[J].地学前缘,2009，16(5)：1-14.
[14]Tarduno J A, Sliter W V, Kroenke L, Leckie R M, Mayer H, Mahoney J J, Musgrave R, Storey M, and Winterer E L. Rapid formation of Ontong Java Plateau by Aptian mantle volcanism [J]. Science,1991,254:399-403.
[15]Duncan R A. A time frame for construction of the Kerguelen Plateau and Broken Ridge [J]. Petrol,2002,43:1109-1119.
[16]Duncan R A, Hargraves RB. Plate tectonic evolution of the Caribbean region in the mantle reference frame [J]. Geol. Soc. Amer. Mem,1984,162:81-93.
[17]Vaughan A P M. Circum-Pacific mid-Cretaceous deformation and uplift:a superplume-related event [J]? Geology,1995,23:491-494.
[18]Ratcliff J T, Bercovici D, Schubert G, et al. Mantle plume heads and the initiation of plate tectonic reorganizations [J]. Earth and Planetary Science Letters,1998,156:195-207.
[19]Wilson P A, Norris R D. Warm tropical ocean surface and global anoxia during the mid-Cretaceous period [J], Nature,2001,412:425-429.
[20]Chumakov N M. Climatic zones in the middle of the Cretaceous Period [J], Stratigraphy and Geological Correlation,1995,3:3-14.
[21]Kominz M A. Oceanic ridge volumes and sea-level change:an error analysis [M] (in Interregional Unconformities and Hydrocarbon Accumulation), edited by J.S. Schlee, Amer. Assoc. Petrol. Geol. Mem.1984,36:109-127.
[22]Matsumoto T. Inter-regional correlation of transgressions and regressions in the Cretaceous period [J]. Cretaceous Research,1980,1 (4):359-373.
[23]Huber B T, Norris R D, Kenneth G, MacLeod. Deep-sea paleotemperature record of extreme warmth during the Cretaceous [J]. Geology,2002,30:123-126.
[24]Jarvis I, Amina M, Richard T J, et al. Late Cretaceous (Campanian) carbon isotope events, sea-level change and correlation of the Tethyan and Boreal realms [J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2002,188:215-248.
[25]Jenkyns H C, Cretaceous anoxic events:From continents to oceans[J]. Geol. Soc. London, 1980,137,171-188.
[26]Arthur M A, Schlanger S O. Cretaceous "Oceanic Anoxic Events" as causal factors in development of reef-reservoired giant oil fields [J]. Amer. Assoc. Petrol. Geol. Bull.,1979, 63,870-885.
[27]Scholle P A, Arthur M A. Carbon isotope fluctuations in Cretaceous pelagic limestones: Potential stratigraphic and petroleum exploration tool [J]. AAPG Bull.,1980,64,67-87.
[28]Bralower T J, Fullagar P D, Paull C K, et al. Mid-Cretaceous strontium-isotope stratigraphy of deep-sea sections. Geological Society of America Bulletin [J],1997,109:1421-1442.
[29]Jones, C E, H C. Jenkyns. Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous [J]. Amer. Jour. Science,2001 301, 112-149.
[30]Tarduno J, Brinkman D B, Renne P R, et al. Evidence for extreme climatic warmth from Late Cretaceous Arctic vertebrates [J]. Science,1998,282:2241-2244.
[31]Huber, B T, Hodell, D A, and C P Hamilton. Middle-Late Cretaceous climate of the southern high latitudes:Stable isotopic evidence for minimal equator-to-pole thermal gradients [J]. Geol. Soc. Amer. Bull.,1995,107,1164-1191.
[32]Norris R D, P A Wilson. Low-latitude sea-surface temperatures for the mid-Cretaceous and the evolution of planktic foraminifera [J]. Geol.,1998,26:823-826.
[33]Fassell M L, T J Bralower. Warm, equable mid-Cretaceous:Stable isotope evidence, in Evolution of the Cretaceous Ocean-Climate System [J]. Geol. Soc. Amer. Spec. Paper.1999, 332:121-142.
[34]Huber B T, Leckie R M, Norris R D, et al.Foraminiferal assemblage and stable isotopic change across the Cenomanian-Turonian boundary in the subtropical North Atlantic [J]. Jour. Foram. Res.,1999,29,392-417.
[35]Bice K L, Birgel D, Meyers P A, et al. A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO2 concentrations [J]. Paleoceanography,2006,21(2): PA2002
[36]Fricke H C. Latitudinal gradients in temperature over North America during the early Eocene using a combined oxygen isotope, paleobotanical approach (in Early Paleogene warm climates and biosphere dynamics; short papers and extended abstracts). GFF,2000,122 (l):50
[37]Tim W, Luis Gonzalez, Greg L, Chris P. Middle Cretaceous greenhouse hydrologic cycle of North America. Geology [J],2001,29:363-366.
[38]Huber B T., Richard D N, Kenneth G M. Deep-sea paleotemperature record of extreme warmth during the Cretaceous [J]. Geology,2002,30:123-126.
[39]李祥辉,·胡修棉等.白垩纪古海洋气候变化及主要问题[J].地球科学进展,2004，19(增刊)：83-92.
[40]Royer D L, Berner R A, Montanez I P, et al. CO_2 as a primary driver of Phanerozoic climate [J]. GSA Today,2004,14:4-10.
[41]Bice K L, Norris R D. Possible atmospheric CO_2 extremes of the warm mid-Cretaceous (late Albian-Turonian) [J]. Paleoceanography,2003,18 (2):1031, doi:10.1029/2002PA000848.
[42]Premoli Silva I, Sliter W V. Cretaceous Paleoceanography:Evidence from planktonic foraminiferal evolution [J]. Soc. Am., Spec. Paper,1999,332:301-328.
[43]Erbacher J, Thurow J, Littke R. Evolution patterns of radiolaria and organic matter variations: A new approach to identify sea-level changes in mid-Cretaceous pelagic environments [J]. Geology,1996,24:499-502.
[44]Bown P R, Rutledge D C, Crux J A, Gallagher L T. Lower Cretaceous (in Calcareous nannofossil biostratigraphy. Bown, part of British Micropalaeontological Society Publication Series) Kluwer Academic Publishers, Dordrecht, Netherlands.1999,86-131.
[45]姬书安.热河生物群重大研究进展综述[J].中国地质,2001,28(4)：19-23.
[46]黄清华,谭伟等.松辽盆地白垩纪地层序列与年代地层[J].大庆石油地质与开发,1999,18(6)：15-17.
[47]罗以达,俞云文.试论永康群时代及区域地层对比[J].中国地质,2004,31(4)：395-399.
[481张妮.江苏侏罗系-白垩系火山岩地层对比及划分探讨[J].地层学杂志,2009，33(1)：91-97.
[49]梅冥相,于炳松等.塔里木盆地库车凹陷白垩纪层序地层格架及古地理演化[J].,占地理学报,2004,6(3)：261-278.
[50]贾进华.塔里木盆地早白垩世沉积相特征与古地理[J].古地理学报，2009，11(2)：167-176.
[51]张泓,晋香兰,李贵红等.鄂尔多斯盆地侏罗纪-白垩纪原始面貌与古地理演化[J].占地理学报,2008,10(1)：1-11.
[52]Ji Qiang, Zhexi Luo and Ji Shu'an. Chinese triconodont mammal and mosaic evolution of the mammalian skeleton [J]. Nature,1999,398:326-330.
[53]邓胜徽,陈芬中.中国东北地区早白垩世真蕨类植物[M].北京：地质出版社,2001.
[54]曹正尧.浙江早白垩世物群[M].北京：科学出版社,1999，174pp.
[55]Zheng S L and Zhou Z Y. A new Mesozoic Ginkgo from western Liaoning, China and its evolutionary significance [J]. Rev. Palaeobot. Palynol.,2004,131:91-103.
[56]Chen P J. Cretaceous paleogeography of China[J]. Palaeogeography, Paleoclimatology, Paleoecology,1987,59:49-56.
[57]Wan X Q, Chen P J, Wei M J. The Cretaceous system in China[J]. Acta Geologica Sinica, 2007,81 (6):957-983.
[58]杨万里松辽陆相盆地石地质[M].北京：石油工业出版社,1985.
[59]王东坡，刘招君,刘立.松辽盆地的演化与海平面升降[M].北京：地质出版社，1992.
[60]陈不基.中国陆相侏罗、白垩系划分对比述评[J].地层学杂志.2000，24(2)：114-119.
[61]郝诒纯,苏德英,余静贤等.中国的白垩系[M].北京：地质出版社,1986.
[62]宋之琛,尚玉珂等.中国孢粉化石(第二卷)：中生代孢粉[M].北京：科学出版社,2000.
[63]何承全,黎文本Parahorologinella gen. nov.——松辽盆地早白垩世孢形体-新属[J].古 生物学报,2004,43(3)：332-337.
[64]李曼英.安徽宣州晚白垩世和古近纪孢粉组合[J].微体古生物学报,2005，22(1)：59-77.
[65]张清波,常英.北京地区大灰厂组孢粉组合及其地质意义[J].北京地质,1994，2：1-7.
[66]常英,张清波.北京西山坨里组孢粉组合及其地层意义[J].北京地质,1994，3：1-9.
[67]江德昕,杨惠秋.朝鲜安州盆地早白垩世孢粉组合[J].植物学报,1996，38(2)：150-155.
[68]刘耕武.川西高原白垩纪孢粉组合的发现及其意义[J].微体古生物学报,1999，16(1)：54-60.
[69]黎文本.从孢粉组合论证松辽盆地泉头组的地质时代及上、下白垩统界线[J].古生物学报,2001,40(2)：153-176.
[70]黄清华,杨建国,孔惠.东北依兰-伊通地堑方正断陷方正组的建立及其意义[J].地层学杂志,2003,27(12)：138-145.
[71]梁诗经,文斐成,陈润生等.福建泰宁白垩纪红层植物及孢粉化石组合特征[J].福建地质,2006,25(1)：1-9.
[72]李建国,杜宝安.甘肃平凉安国镇白垩系六盘山群的孢粉植物群[J].古生物学报,2006,45(4)：498-513.
[73]刘兆生.甘肃玉门早峡早白垩世孢粉组合[J].微体古生物学报.2000，17(3)：73-84.
[74]邵红君,万传彪,任延广等.海拉尔盆地贝16井含油地层划分对比[J].世界地质,2007,26(2)：230-239.
[75]李春柏,万传彪,乔秀云等.海拉尔盆地海参1井伊敏组孢粉组合的地层意义[J].地层学杂志,2007,31(1)：23-34.
[76]宋之琛,我国早白垩世被子植物花粉研究之回顾[J].微体古生物学报,1986，3(4)：373-386
[77]黄嫔,龙文国.海南乐东洪帽剖面鹿母湾组孢粉组合及其地层意义[J].微体古生物学报,2008,25(1)：79-90.
[78]万传彪,乔秀云,孔惠等.黑龙江北安地区早白垩世孢粉组合[J].微体古生物学报,2002,19(1)：83-90.
[79]赵海滨,尹志刚,汪岩等.黑龙江北部嘉荫盆地中南部原划新近系时代的重新厘定.地质通报,2006,25(4)：460-464.
[80]王鑫甫,曹流.黑龙江嘉荫晚白垩世渔亮子组孢粉地层研究[J].微体古生物学报,1999,16(2)：190-194.
[81]尚玉珂.黑龙江省鸡西城子河组被子植物化石层的孢粉研究[J].微体古生物学报,1997,14(2)：161-174.
[82]郑玉龙,刘文龙,乔秀云.黑龙江孙吴-嘉荫盆地白垩纪孢粉组合及地层划分对比[J]地层学杂志,2005,29(4)：342-347.
[83]姜宝玉,冯金宝.鸡西群城子河组时代的进一步探讨[J].地层学杂志,2001，25(3)：217-221.
[84]黄嫔,张光富.吉林延边智新盆地大拉子组孢粉组合[J].微体古生物学报,2002，19(3)：263-275,
[85]黎文本,李建国.吉林榆树榆-302孔阿尔布期孢粉组合[J].古生物学报,2005，44(2)：209-228.
[86]万传彪,刘本培,乔秀云等.嘉荫盆地太平林场组巴尔姆孢(Balmeisporites)的发现及其意义[J].地质学报,2004,78(1)：1-9.
[87]刘耕武,李伟同,张清如等.江汉盆地渔洋组上部的古新世孢粉组合[J].古生物学报,2006,45(1)：60-68.
[88]杨雪英,周山富.江苏淮安地区上白垩统含盐地层孢粉组合序列[J].地层学杂志,2002,26(3)：193-211.
[89]温国强.辽河盆地大民屯凹陷沈249井早白垩世九佛堂组孢粉组合[J].微体古生物学报,2006,23(2)：191-198.
[90]吴炳伟,雷安贵.辽宁铁岭盆地早白垩世孢粉组合[J].微体古生物学报,2007，24(1)89-97.
[91]吴河勇,黄清华,党毅敏等.内蒙古海拉尔盆地白垩纪生物地层研究进展[J].古生物学报,2006,45(2)：283-291.
[92]黄清华,赵来时,卢古武等.内蒙古海拉尔盆地大磨拐河组孢粉化石及其时代浅析[J].地质科技情报,2006,25(1)：19-26.
[93]李凤霞.内蒙古开鲁盆地早白垩世阜新组孢粉组合[J].微体古生物学报,2005，22(1)：87-96.
[94]司双印.李洲,张森宝.山东省白垩系下统孢粉组合及地层意义[J].中国地质,2001，28(6)：21-27.
[95]司双印.山东省大盛群孢粉组合及其年代地层意义[J].地层学杂志,2001，26(2)：126-131.
[96]王家文,常峰.山东郯城王氏组被子植物花粉研究[J].合肥工业大学学报(自然科学版),1997,20(6)：99-102.
[97]尚玉珂,袁德艳.松辽盆地南部梨树凹陷登楼库组孢粉组合[J].微体古生物学报,1995,12(3)：307-321.
[98]万传彪,乔秀云,孔惠等.松辽盆地三站地区营城组孢粉化石的意义[J].大庆石油地质与开发,2002,21(2)：12-14.
[99]乔秀云,孙跃武,万传彪等.孙吴-嘉荫盆地嘉D1井孢粉地层学研究[J].世界地质,2005,24(1)：11-17.
[100]江德昕,王永栋,何卓生等.新疆塔里木拜城地区早白垩世舒善河组孢粉组合[J].微体古生物学报,2007,24(3)：247-260.
[101]江德听,王永栋,何卓生等.新疆塔里木盆地早白垩世克孜勒苏群孢粉组合[J].微体古生物学报,2006,23(4)：371-291.
[102]詹家祯,师天明,周春梅等.新疆准噶尔盆地芳3井晚白垩世孢粉组合的发现及其地质意义[J].微体古生物学报,2007,24(1)：15-27.
[103]张剑,刘洪涛,吴炳伟.彰武盆地张强凹陷早白垩世孢粉组合[J].微体古生物学报,20086,25(2)：196-203.
[104]张光富.中国吉林大拉子组的时代探讨[J].地层学杂志,2005，29(4)：381-388.
[105]张文堂,陈丕基,沈炎彬.中国的叶肢介化石[M].北京：科学出版社,1976，325pp.
[106]Chen P J. Cretaceous conchostracan faunas of China [J]. Cretaceous Research,1994,15: 259-269.
[107]Gang Li, Yanbin Shen, David J. Batten. Yanjiestheria, Yanshania and the development of the Eosestheria conchostracan fauna of the Jehol Biota in China [J]. Cretaceous Research,2007, 28 (2):225-234.
[108]杨静,王志萍,王伟栋.二连盆地西部赛汉塔拉组轮藻化石及其时代意义[J].大庆石油地质与开发,2003,22(3)：19-23.
[109]王启飞,杨景林,卢辉楠.甘肃高台早白垩世下沟组轮藻化石[J].微体古生物学报,2003，20(2)：187-198.
[110]符俊辉,卢辉楠.甘肃花海盆地截大板沟早白垩世轮藻化石[J].古生物学报,1997，36 (3)：350-357.
[111]符俊辉,袁凤钿.甘肃花海盆地早白垩世的介形类[J].古生物学报,1998，37(3)：333-338.
[112]巫建华.江西信江盆地早白至世晚期轮藻及其地层意义[J].微体古生物学报,1995，12(1)：79-87.
[113]彭维松,王启飞,薛铎等.内蒙古银根-额济纳旗盆地白垩纪轮藻化石[J].微体古生物学报,2003,20(4)：365-376.
[114]杨景林,王启飞,卢辉楠.准噶尔盆地白垩纪轮藻化石组合序列[J].微体古生物学报,2008,25(4)：345-363.
[115]姜宝玉,蔡华伟.黑龙江省东部七虎林组中阿普第期的两属异齿类双壳类化石[J].古生物学报,2004,43(2)：112-117.
[116]邢光福,陈荣等.东南沿海晚白垩世火山岩浆活动特征及其构造背景[J].岩石学报.2009,25(1)：77-91.
[117]谢桂青,毛景文等.长江中下游鄂东南地区大寺组或砂岩SHRIMP定年及其意义[J].科学通报.2006,51(19)：2283-2291.
[118]杨经绥,孟繁聪,张建新等.重新认识阿尔金断裂东段红柳峡火山岩的时代及构造意义[J].中国科学,2001,31(增刊)：83-89
[119]唐嘉锋,刘玉琳,王启飞.山东中生代火山岩年代学研究[J].岩石学报,2008，24(6)：1333-1338.
[120]凌文黎,谢先军,柳小明,程建萍.鲁东中生代标准剖面青山群火山岩锆石U-Pb年龄及其构造意义[J1.岩石学报,2006,36(5)：401～411.
[121]杨振宇.高精度地层划分对比的可靠方法——磁性地层学研究[J].地质通报,2002，21(2)：45-47.
[122]Heller F, Evans M E. Loess Magnetism [J]. Reviw Geophysics,1995,33:211-240.
[123]庄忠海、田端孝、马醒华.四川盆地雅安至天全白垩系一下第三系古地磁研究[J].物探与化探,1988,12(3)：224-228.
[124]尹济云,孙知明,杨振宇等.滇西兰坪盆地白垩纪-早第三纪古地磁结果及其地质意义[JJ.地球物理学报,1999,42(5)：648-659.
[125]孟自芳.兰州附近下白垩统河口群中下岩段磁性地层划分[J].地球物理学报,1994，37(增刊)：342-347.
[126]唐玉虎.兰州-民和盆地早白垩世磁性地层年代与青藏高原北部隆升：硕士学位论文.兰州：兰州大学,2008.
[127]戴霜,朱强,胡鸿飞等.六盘山群磁性地层年代[J].地层学杂志,2009,33(2)：188-192.
[128]彭守涛,李忠,黄宝春等.库车坳陷北部白垩系磁性地层划分[J].科学通报.2005，50(19)：2136-2144.
[129]陈丕基.中国侏罗、白垩纪古地理轮廓——兼论长江起源[J]；北京大学学报(自然科学版),1979,3：92-111.
[130]殷鸿福.中国古生物地理学[M].中国地质大学出版社：武汉.1988.
[131]中国地质科学院地质研究所、武汉地质学院,中国古地理图集[M].北京：地图出版社.1985，6：108-119.
[132]杨卫东,陈南生,倪师军,等1白垩纪红层碳酸盐岩和恐龙蛋壳碳氧同位素组成及环境意义[J].科学通报,1993,38(23)：2161～2163.
[133]Yi Yan, Bin Xia, Ge Lin et al. Geochemistry of the sedimentary rocks from the Nanxiong Basin, South China and implications for provenance, paleoenvironment and paleoclimate at
the K/T boundary [J]. Sedimentary Geology,2007,197 (1-2):127-147.
[134]曹珂,李祥辉,王成善.四川盆地白垩系粘土矿物特征及古气候探讨[J].地质学报,2008,82(1)：115-123.
[135]J.Madhavaraju, S. Ramasamy, Alastair Ruffell et al. Clay mineralogy of the Late Cretaceous and early Tertiary successions of the Cauvery Basin (southeastern India):implications for sediment source and palaeoclimates at the K/T boundary [J]. Cretaceous Research,2002,23: 153-163
[136]Bice K L, Birgel D, Meyers P A, et al. A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO_2 concentrations [J]. Paleoceanography,2006, 21(2):PA2002
[137]A. J. Boucot,陈旭,C. R. Scotese,樊隽轩,显生宙全球古气候重建[M].北京：科学出版社,2009.
[138]向芳,宋见春,罗来等.白垩纪早期陆相特殊沉积的分布特征及气候意义[J].地学前缘,2009,16(5)：48-62.
[139]Su-chin Chang, Haichun Zhang, Paul R Renne, Yan Fang. High-precision 40Ar/39Ar age for the Jehol Biota [J]. Palaeogeography, Paleoclimatology, Paleoecology,2009,280:94-104.
[140]Hakuyu Okada. Nature and development of Cretaceous sedimentary basins in East Asia:a review [J]. Geosciences Journal,2000,4 (4):271-282.
[141]曹珂,王猛.沉积记录对白垩纪中国大陆古气候模拟的约束[J].地学前缘,2009，16(5)：29-36.
[142]Scotese. www.scotese.com,2002.
[143]董树文,李廷栋,钟大赉等.侏罗纪／白垩纪之交东亚板块汇聚的研究进展和展望[J].中国科学基金,2009,5：281-286.
[144]董树文,张岳桥,龙长兴等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11)：1449-1461.
[145]Yin A, Nie S. A Phaneozoic palinspastic reconst ruction of China and it s neighboring regions [M]. In:Yin A and Harrison T M (eds). The Tectonic Evolution of Asia. Cambrige University Press,1996:442-485.
[146]Yang Z,Sun Z,Ma X, Huang B,Zhou Y. APWP and tectonic movement s of t he Nort h China Block during t he Phanerozoic [J]. Science in China, Series D,1998,41 (supp.):51-65.
[147]Meng Q R, Hu J M, Jin J Q, et al. Tectonics of the late Mesozoic wide extensional basin system in t he China -Mongolia border region [J]. Basin Research,2003,15:397-415.
[148]陈丕基,E Norling.西藏构造楔与塔里木-华南地块的裂解[J].科学通报,1994，39(16)：1512-1515.
[149]Moores G W. Mesozoic and Cenozoic paleogeographic development of the Pacific region. Abstract,28th International Geological Congress,1988,2-474. Washington D C, USA.
[150]Shigenori Maruyama, Yukio Isozaki, Gaku Kimura et al.. Paleogeographic maps of the Japanese islands:Plate tectonic synthesis from 750Ma to the present [J]. The Island Arc, 1997,6:121-142.
[151]Seno T, Maruyama S. Paleogeographic reconstruction and origin of the Philippine Sea [J]. Tectonophysics,1984,102:53-84.
[152]Maruyama S, Seno T. Orogeny and relative plate motions:example of the Japanese Islands [J]. Tectonophysics,1986,127:305-329.
[153]Uyeda S, Miyashiro A. Plate tectonics and the Japanese Islands:a synthesis [J]. Geological Society of America Bulletin,1974S 85:1159-1170.
[154]Takahashi M. Space-time distribution of Late Mesozoic to Early Cenozoic magmatism in East Asia and its tectonic implications [J]. In:Hashimoto, M. and Uyeda, S. (eds.), Accretion Tectonics in the Circum-Pacific Regions. Terra, Tokyo,1983, p.69-88.
[155]Kinoshita O. A migration model of magmatism explaining a ridge subduction, and its details on a statistical analysis of the granite ages in Cretaceous Southwest Japan [J]. The Island Arc,1999,8:181-189.
[156]Larson R L, Kincaid C. Onset of mid-Cretaceous volcanism by elevation of 670 km thermal boundary layer [J]. Geology,1996,24:551-554.
[157]Okada H. Plume-related sedimentary basins in East Asia during the Cretaceous [J]. Palaeogeography, Palaeoclimatology, Palaeoecology,1999,150:1-11.
[158]Yano T, Wu G Y. Late Mesozoic geodynamics relating Circum-Pacific mobile belt and Darwin Rise [J]. Journal of Geological Society of the Philippines.1997,52:235-271.
[159]马杏垣.1：4,000,000中国及邻近海域岩石圈动力学图[M].北京：地质出版社,1989.
[160]Gilder S A, Keller G R,Luo Ming, Goodell P C. Timing and spatial dist ribution of rifting in China [J]. Tectonophysics,1991,197:225-243.
[161]Ren J Y, Tamaki K, Li Sitian, Zheng J unxia. Late Mesozoic and Cenozoic rifting and it s dynamic setting in eastern China and adjacent areas [J]. Tectonophysics,2002,344:175-205.
[162]Lin Wei,Wang Qingchen. Late Mesozoic extensional tectonics in the North China Block:a crustal response to subcontinental mantle removal [J]? Bull. Geol. Soc. France,2006,117 (6): 287-297.
[163]Liu Junlai, Davis G A, Wu Fuyuan. The Liaonan metamorphic core complex, Southeastern Liaoning Province, North China:a likely cont ributor to Cretaceous rotation of Eastern Liaoning, Korea and contiguous areas [J]. Tectonophysics,2005,407:65-80.
[164]季强,陈文,王五力等.中国辽西中生代热河生物群[M].北京：地质出版社,2004：1-357.
[165]Wong W H. Crust movement in eastern China. Proceedings of 3th Pan-Pacific Science Congress, Tokyo,1926:642-685.
[166]Wong W H. Crustal movement and ignous activities in eastern China since Mesozoic time [J]. Bulletin of Geological Society of China,1927,6 (1):9-36.
[167]Wong W H. The Mesozoic orogenic movement in eastern China [J]. Bulletin of Geological Society of China,1929,8:33-44.
[168]任纪舜,王作勋,陈炳蔚等.中国及邻区大地构造图(1／500万)及简要说明书——从全球看中国大地构造[M].北京：地质出版社,1999：6-9.
[169]崔盛芹,李锦蓉,吴珍汉等.燕山地区中新生代陆内造山[M].北京：地质出版社,2002：1-386.
[170]万天丰.中国大地构造学纲要[M].北京,地质出版社,2004.
[171]赵越,徐刚,张拴红.燕山运动与东亚构造体制的转变[J].地学前缘，2004，11(3)：319-328.
[172]任纪舜,陈廷愚,牛宝贵等.中国东部及邻区大陆岩石圈的构造演化与成矿[M].北京：科学出版社,1990,1-205.
[173]任纪舜,牛宝贵,和政军等,中国东部的构造格局和动力演化[M].任纪舜和杨巍然主编：中国东部岩石圈结构与构造岩浆演化.北京：原子能出版社,1998,1-12.
[174]Niu B G, He Z J,Song B,Xiao W W. SHRIMP geochronology of volcanics of the Zhangjiakou and Yixian Formations, Northern Hebei Province, with a discussion on the age of the Xingpanling Group of the Great Hinggan Mountains and volcanic strata of the southeastern coastal area of China [J]. Acta Geologica Sinica (English Edition),2004, 78:1214-1228.
[175]张旗,钱青,王二七等.燕山中晚期中国东部高原：埃达克岩的启示[J].地质科学,2001,36(2)：248-255.
[176]吴福元,徐义刚,高山,等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报,2008,24：1145-1174
[177]姜耀辉,蒋少涌,赵葵东,等.辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约[J].科学通报,2005，50：2161-2168
[178]徐义刚,李洪颜,庞崇进,等.论华北克拉通破坏的时限[J].科学通报,2009，54：1974-1989
[179]Zhou Xinhua, Yang Jinhui, Zhang Lianchang. Metallogenesis of superlarge gold deposit s in Jiaodong region and deep processes of subcontinental lithosphere beneath north China craton in Mesozoic [J]. Science in China (series D),2002,32 (suppl.):11-20.
[180]吴福元,葛文春,孙德有等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,10(3)：51-60
[181]Wu Fuyuan, Lin Jingqian, Wilde S A et al. Nature and significance of the Early Cretaceous giantigneous event in eastern China [J]. Earth Planet Science Letter,2005,233:103-119.
[182]徐贵忠,周瑞,闫臻等.论胶东地区中生代岩石圈减薄的证据及其动力学机制[J].大地构造与成矿学,2001,25(4)：368-380.
[183]张岳桥,李金良,张田等.胶莱盆地及其邻区白垩纪-古近世沉积构造演化历史及其区域动力学意义[J].地质学报,2008,82(9)：1229-257.
[184]Mao Jingwen, Wang Yitian, Zhang Zuoheng, et al. Geodynamic settings of Mesozoic large-scale mineralization in North China and adjacent areas:Implication from the highly precise and accurate ages of metal deposits [J]. Science in China (series D),2003,46 (8): 838-851.
[185]Chen Jiangfeng, Xie Zhen, Li Huimin, et al. U-Pb zircon ages for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrain, China [J]. Geochemical Journal, 2003,37(1):35-46.
[186]郭敬辉,陈福坤,张晓曼等.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞一.碰撞后构造过程：锆石U-Pb年代学[J].岩石学报,2005,21(4)：1281-1301.
[187]陈毓川,常印佛,裴荣富等.中国成矿体系与区域成矿评价[M].北京：地质出版社,2007.
[188]万桂梅,汤良杰,金文正等.郯庐断裂带研究进展及存在问题探讨[J].地质论评,2009,55(2)：251-259.
[189]Yin An, Nie Sh Y. An indentation model for t he north and south China collision and the development of the Tanlu and Honam fault system, eastern Asia [J]. Tectonics,1993,12 (4): 801-813.
[190]Fletcher C J N, Fitches W R, Rundle C C et al. Geological and isotopic constraints on the timing of the movements in the Tan-Lu fault zone [J]. Journal of Southeast Asian Earth Science,1995,11:15-22.
[191]Ross J V, Mercier J C, Xu Y G. Diffusion creep in the upper mantle:an example from the
Tan-Lu Fault, nort heastern China [J]. Tectonophysics,1996,261:315-329.
[192]Gilder S A, Leloup P H, Courtiliot V, et al. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via middle Triassic to early Cenozoic paleomagnetic data [J]. Journal of the Geophysical Research,1999,104 (B7):15365-15390.
[193]Rat schbacher L, Hacker B R, Webb L E, et al. Exhumation of ultra-high pressure continental crust in east central China:Cretaceous and Cenozoic unroofing and the Tan-Lu fault [J]. Journal of the Geophysical Research,2000,105 (B6):13303-13338.
[194]Li Jianwei, Zhou Meifu, Li Xianfu, et al. The Hunan-Jiangxi strike-slip fault system in southern China:southern termination of the Tan-Lu fault [J]. Journal of Geodynamics,2001, 32:333-354.
[195]Zhang Yueqiao, Dong Shuwen, Shi Wei. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province, eastern China [J]. Tectonophysics,2003,363: 243-258.
[196]Zhu Guang, Wang Yongsheng, Liu Guosheng, et al.~(40)Ar/~(39)Ar dating of strike-slip motion on t he Tan-Lu fault zone, East China [J]. Journal of Structural Geology,2005,27: 1379-1398.
[197]徐嘉炜,马国锋.郯庐断裂研究的十年回顾[J].地质论评,1992,38(4)：316-324.
[198]罗志立,李景明,李小军等.试论郯城—庐江断裂带形成、演化及问题[J].吉林大学学报(地球科学版),2005,35(6)：699-706.
[199]张用夏,李卢玲.郯庐断裂带的平移及其对邻区构造的影响[J].构造地质论丛(3).北京：地质出版社,1984：1-8.
[200]朱光,牛漫兰,宋传中等.郯庐断裂带新生代的上地幔剪切作用与火山活动[J].安徽地质,2001,11(2)：106-112.
[201]万天丰.郯庐断裂带的演化与古应力场[J].地球科学,1995：526-534.
[202]万天丰,朱鸿.郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报,1996,2(1)：14-27.
[203]Mercier J L, Hou Minjing, Vergely P, et al. Structural and stratigraphical constraints on the kinematics history of the Southern Tan-Lu Fault Zone during the Mesozoic Anhui Province, China [J]. Tectonophysics,2007,439:33-66.
[204]陈宣华,王小凤,张青等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000,30(3)：215-220.
[205]徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995，10(2)：121-132.
[206]朱光,刘国生,牛漫兰等.郯庐断裂带的平移运动与成因[J].地质通报,2003，22(3)：200-207.
[207]汤加富,许卫.郯庐断裂带南段并无巨大平移——来自安徽境内的证据[J].地质论评,2002,48(5)：449-456.
[208]劳秋元.郑庐断裂带前古生代、古生代的形成演化间题[M].见：《构造地质论丛(3)》北京：地质出版社,1984：80-93.
[209]陈不基.郯庐断裂巨大平移的时代与格局[J].科学通报,1988,33(4)：289-293.
[210]翁世劫.关于郑庐断裂带的几个地质问题[M].见：《构造地质论丛(3)》.北京：地质出版社,1984：66-71.
[211]郭振一.沂沐断裂带的基本特征及其活动方式[M].见：《构造地质论丛(3)》.北京：地质出版社,1984：142-151.
[212]吴根耀,马力,梁兴等.从郯庐断裂带两侧的”盆”“山”耦合演化看前白垩纪“郯庐断裂带”的性质[J].地质通报,2008,27(3)：308-325.
[213]朱光,徐嘉炜,孙世群.郯庐断裂带平移时代的同位素年龄证据[J].地质论评,1995,41(5)：452-456.
[214]王勇生,朱光,胡召齐等.郯庐断裂带沂沭段伸展活动断层泥K-Ar同位素定年[J].中国科学(D),2009,52(4)：489-503,
[215]Wang Pujun, Xie Xiao'an, Mattern Frank et al. The Cretaceous Songliao Basin: volcanogenic succession, sedimentary sequence and Tectonic evolution, NE China [J]. Acta geologica sinica,2007,81 (6):1002-1011.
[216]和钟铧,刘招君,陈秀艳等.黑龙江省东部残留盆地群早白垩世沉积相特征及演化[J].古地理学报,2008,10(2)：151-158.
[217]张世红,张传恒,李红生.黑龙江省东部裴德组砾石中放射虫的发现及其意义[J].地层学杂志,1999,23(3)：201-205.
[218]孙革,郑少林,姜剑红,等.黑龙江鸡西含煤盆地早白垩世生物地层研究新进展[J].煤田地质与勘探,1999,27(6)：1-3.
[219]姜宝玉.黑龙江省东部七虎林组的一些双壳类化石[J].动物学杂志,2003，38(4)85-100.
[220]杨建国,赵传本.黑龙江省龙爪沟地区侏罗系研究新进展[J].大庆石油地质与开发,1998,17(6)：16-18.
[221]孙革,郑少林.中国东北中生代地层划分对比之新见[J].地层学杂志,2000，24(1)：60-64.
[222]杨小菊,何承全,黎文本,等.鸡西盆地早白垩世穆棱组海相沟鞭藻的发现及其古环境意义[J].科学通报,2003,48(14)：1553-1556.
[223]程金辉,何承全.黑龙江省东部鸡西盆地早白垩世滴道组的沟鞭藻类[J].古生物学杂志,2001,40(1)：127-133.
[224]Kellys R A, Wang Yigang, ZhengLin. A revised Cretaceous age for ammonites, originally identified as Middle Jurassic, from eastern Hei longjiang, China [J]. Acta Palaeontologica Sinica,1994,33 (4):509-517.
[225]Futakami M, Matsukawa M, Chen Piji, et al. Barremian ammonite from the Longzhaogou Group in eastern Heilongjiang, northeast China [J]. The Journal of the Geological Society of Japan,1995,101 (1):79-85.
[226]沙金庚.黑龙江东部早白垩世生物地层学研究的主要进展[J].地学前缘,2002，9(3)：95-101.
[227]潘华璋,朱祥根.黑龙江省东部早白垩世的一些海相和半咸水相腹足类[J].古生物学报,2004,43 (3):338-348.
[228]万传彪,闫风兰,尹楠.黑龙江集贤地区早白垩世沟鞭藻类和其他藻类[J].微体古生物学报,1995,12(1):51-52.
[229]陈义贤,陈文寄.辽西及邻区中生代火山岩——年代学、地球化学和构造背景[J].北京：地震出版社,1997,106-163
[230]景山.冀北-辽西地区早白垩世义县组沉积环境及其与盆地演化的关系：[硕士学位论文].北京：中国地质大学(北京),2008.
[231]柳永清,田树刚,庞其清.滦平盆地大北沟组-大店子组沉积和地层格架及陆相层型意义[J].地球学报,2001,22 (5):391-396
[232]柳永清,庞其清,李佩贤.冀北滦平陆相侏罗-白垩系生物地层界线及候选层型研究进 展[J].地质通报,2002,21(3)：176-180
[233]季强,论热河生物群[J].地质论评,2002,48(3)：290-296
[234]季强,陈文,王五力等.中国辽西中生代热河生物群[M].北京：地质出版社,2004.
[235]王璞珺,杜小弟,王东坡.松辽盆地白垩纪湖侵沉积层序与湖海沟通事件的地球化学记录[J].岩相古地理,1995,15(4)：14-20
[236]贾军涛,王璞珺,张斌等.哈尔滨东宾县凹陷白垩纪地层层序及其与松辽盆地的对比[J].地质通报,2006,25(9-10)：1143-1151.
[237]樊馥,蔡进功,高福红.孙吴—嘉荫盆地太平林场组烃源岩海侵特征研究[J].沉积学报,2009,27(4)：650-656.
[238]章凤奇,陈汉林,董传万等.松辽盆地北部火山岩锆石SHRIMP测年与营城组时代探讨[J].地层学杂志,2008,32(1)：15-20.
[239]丁日新,舒萍,曲延明等.松辽盆地庆深气田储层火山岩锆石U-Pb同位素年龄及其地质意义[J].吉林大学学报(地球科学版),37(3)：525-530.
[240]舒萍,丁日新,纪学雁等.松辽盆地庆深气田储层火山岩锆石地质年代学研究[J].岩石矿物学杂志,2007,26(3)：239-346.
[241]王璞珺,高有峰,任延广等.松辽盆地青山口组橄榄粗安岩~(40)Ar/~(39)Ar年龄、地球化学及其成盆、成烃和成藏意义[J].岩石学报,2009,25(5)：1178-1190.
[242]叶得泉,钟筱春,石宝珩等.中国北方含油气区白垩系[M].北京：石油工业出版社,1990.
[243]赵传本，叶得泉,魏德恩等.中国油气区第三系(Ⅲ)——东北油气区分册[M].北京：石油工业出版社,1990.
[244]Swisher C C,汪筱林,周忠和等.义县组同位素年代新证据及土城子组~(40)Ar/~(39)Ar年龄测定[J].科学通报,2001,46(23)：2009-2012.
[245]杨进辉,吴福元,邵济安等.冀北张-宣地区后城组、张家口组火山岩锆石U-Pb年龄和Hf同位素[J].地球科学,2006,31(1)：71-80.
[246]张宏,王明新,柳小明LA-ICP-MS测年对辽西-冀北地区髫髻山组火山岩上限年龄的限定[J].科学通报,2008,53(15)：1815-1824.
[247]张宏,柳小明,张哗卿等.冀北滦平-辽西凌源地区张家口组火山岩顶、底的单颗粒锆石U-Pb测年及意义[J].地球科学——中国地质大学学报,2005，30：387-401.
[248]Cope T C. Sedimentary Evolution of the Yanshan Fold-thrust Belt, Northeast China [J]. Califonia:Stanford Uni,2003.1-230.
[249]张宏,柳小明,高山等.辽西凌源地区张家口组的重新厘定及其意义——来自激光ICP-MS锆石U-Pb年龄的制约[J].地质通报,2005,24(2)：110-117.
[250]李佩贤,程政武,庞其清.辽西北票孔子鸟Confuciusornis的层位及年代[J].地质学报,2001,75(1)：1-13.
[251]张宏,柳小明,袁洪林等.辽西凌源地区义县组下部层位的U-Pb测年及意义[J].地质评论,2006,52(1)：63-71.
[252]Swisher C C, Wang Y Q, Wang X L, et al. Cretaceous age of thefeathered dinosaurs of Liaoning, China [J]. Nature,1999,400:58-61.
[253]朱日祥,邵济安,潘永信等.辽西自垩纪火山岩古地磁测定与陆内旋转运动[J].科学通报,2002,47(17)：1335-1440.
[254]Zhu R X, Pan YX, Shaw J, et al. Geomagnetic palaeointensity just prior to the Cretaceous normal superchron [J]. Physics of the earth and planetary interiors,2001,128 (1-4):207-222
[255]王清利,陈文,张彦.辽西喀左县孤山义县组安山岩激光~(40)Ar/~(39)Ar和锆石SHRIMP U-Pb年龄及其地质意义[J].地质论评,2008,54(1)：125-133.
[256]陈文,张彦,季强等.2005.四合屯珍稀化石层的时代一一39Ar/40 Ar和SHRIMPU-Pb年龄新证据[J].地层学杂志,29：582～588.
[257]孟凡雪,高山,柳小明.辽西凌源地区义县组火山岩锆石U-Pb年代学和地球化学特征[J].地质通报,2008,27(3)：364-373.
[258]王松山,胡华光,李佩贤等.再讨论辽西四合屯脊椎动物生存时代Ar-Ar年龄证据[J].岩石学报,2001,17(4)：663-668.
[259]汪方跃,高山,牛宝贵等.河北承德盆地114 Ma大北沟组玄武岩地球化学及其对华北克拉通岩石圈地幔减薄作用的制约[J].地学前缘,2007，14(2)：98-108.
[260]Zhang H, Wang M X, Liu XW. LA-ICP-MS dating of Zhangjiakou formation volcanic rocks in the Zhangjiakou region and its geological significance [J]. Progress in Nature Science,2008,18 (8):975-982.
[261]牛宝贵,和政军,宋彪等.张家口组火山岩SHRIMP定年及其重大意义[J].地质通报,I2003,22(2)：140-141.
[262]柳永清,李佩贤,田树刚等.冀北滦平晚中生代火山碎屑(熔)岩中锆石SHRIMP U-Pb年龄及其地质意义[J].岩石矿物学杂志,2003，22(3)：237-244.
[263]孙立新,赵风清,王惠初等.燕山地区土城子组划分、时代与盆地性质探讨[J].地质学报；2007,81(4)：445-454.
[264]韦忠良,张宏,柳小明等.张家口地区张家口组火山岩的LA-ICP-MS测年及其地质意义[J].自然科学进展,2008,18(5)：523-530.
[265]贾军涛,王璞珺,万晓樵.松辽盆地断陷期白垩纪营城组的时代归属.地质论评,2008,54(4)：439-448.
[266]赵重远.鄂尔多斯盆地的演化历史、形成机制和含油气有利地区[M]／／赵重远.华北克拉通沉积盆地形成与演化及油气赋存.西安：西北大学出版社,1990.
[267]李向平,陈刚,章辉若等.鄂尔多斯盆地中生代构造事件及其沉积响应特点[J]。西安石油大学学报(自然科学版),2006，21(3)：1-5.
[268]张泓,晋香兰,李贵红,杨志远,张慧,贾建称.鄂尔多斯盆地侏罗纪一白垩纪原始面貌与古地理演化.古地理学报,2008，10(1)：1-11.
[269]江新胜、潘忠习.中国白垩纪沙漠及气候[M].北京：地质出版社,2005.
[270]江新胜,潘习忠.白垩纪时期东亚大气环流格局初探[J].中国科学(D辑),2000，30(5)：587-591.
[271]吴仁贵,余达淦,周万蓬等.鄂尔多斯盆地北部早白垩世地层特征及对比[J].地层学杂志,2005,29(1)：50-54.
[272]齐骅.宁夏固原六盘山群下部的介形类化石[J].地层古生物论文集,1987，18：74-147.
[273]齐骅.宁夏固原六盘：山群上部的介形类化石[J].地层古生物论文集,1988，22：85-127.
[274]李祖望.平凉安国镇六盘山群介形类[J].甘肃地质学报,1995，4(2)：10-21.
[275]蔡雄飞,李长安,朱伟元等.兰州-民和盆地红古城组的建立及其地质学意义[J].甘肃地质学报,1998,7(2)：49-53.
[276]蔡雄飞,李长安,占车生等.民和盆地南缘盐锅峡组的建立及其地质意义[J].岩相古地理,1999,19(3)：16-20.
[277]蔡雄飞,顾延生,李长安.兰州-民和盆地恐龙足印化石形成的地质特征[J].地层学杂志,2005,29(3)：306-309.
[278]吉利明民和盆地早白坚世晚期的抱粉组合[J].植物学报.1995，37(7)：566-573.
[279]何光玉,杨树锋,陈汉林等.河西走廊西段及邻区早白垩世盆地的重新厘定[J].石油
学报,2004,25(6)：18-22.
[280]李奋其.酒泉盆地形成机制与演化：博士学位论文.成都：成都理工大学,2004.
[281]胡艳霞.甘肃玉门红柳峡早白垩世下沟组的介形类[J].微体古生物学报.2004，21(4)：439-455.
[282]胡艳霞,徐东来.甘肃玉门下沟地区早白垩世下沟组介形类[J].微体古生物学报.2005,22(2)：173-184.
[283]邓胜徽,卢远征.甘肃酒泉盆地早白垩世植物化石及其古气候意义[J].地质学报,2008,82(1)：104-116
[284]卫平生,张虎权,陈启林等.银根-额济纳旗盆地下白垩统银根组的确立[J].地层学杂志,2007,31(2)：184-189.
[285]吴少波,白玉宝,刘勇等.银根盆地苏红图组火山岩特征及其与油气的关系[J].西安石油学院学报,1998,13(6)：8-11.
[286]吴少波,白玉宝.银根盆地早白垩世火山岩特征及形成大地构造环境[J].矿物岩石,1999,32(4)：24-28.
[287]付国斌,李罡,任玉光等.内蒙古呼伦陶勒盖下白垩统巴音戈壁组的叶肢介化石[J].古生物学报,2007,46(2)：244-248.
[288]吴仁贵,周万蓬,刘平华.关于内蒙古巴音戈壁盆地早白垩世地层的讨论[J].地层学杂志,2009,33(1)：87-90.
[289]郭彦如,刘全新,樊太等.查干断陷湖盆层序地层框架中的含油气系统[M].北京：地质出版社,2003.
[290]郭宪璞，叶留生,李汉敏等.塔里木盆地白垩纪地层对比及格架[J].中国西部油气地质,2006,2(2)：140-146.
[291]苏新,郭宪璞,丁孝忠.塔里木北部库车前陆盆地晚白垩世和古新世的钙质超微化石组合[J].现代地质,2003,17(4)：370-377.
[292]和钟铧,刘招君,郭巍等.柴达木北缘中生代盆地的成因类型及构造沉积演化.吉林大学学报(地球科学版),2002,32(4)：333-339.
[293]郑秀亮,商华.介形类化石Cypridea (Pseudocypridina) gigantea的地层及环境意义[J].新疆石油地质,2007,28(1)：64-66.
[294]杨景林,王启飞,卢辉楠.准噶尔盆地南缘呼2井晚白垩世、古新世轮藻植物群的发现及其意义[J].微体古生物学报,2005,22(3)：251-268.
[295]李伟.渤海湾盆地区中生代盆地演化与前第三系油气勘探：博士学位论文.东营：石油大学,2007.
[296]张增奇,刘明渭.山东省岩石地层[M].武汉：中国地质大学出版社,1996.
[297]刘明渭,张庆玉,宋万千.山东省白垩纪岩石地层序列与火山岩系地层划分[J].地层学杂志,2003,27(3)：248-254.
[298]李浩敏.安徽五河下白垩统被子植物叶化石[J].科学通报,2003，48(4)：375-378.
[299]吴海权,江来利,戴圣潜.安徽霍山-毛坦厂地区中生代地层层序的厘定[J].地层学杂志,2002,26(1)：39-45.
[300]韩树棻,杨有根,朱彬等.安徽北部中、新生代沉积盆地分析[J].安徽地质,1994，4(3)：27-35.
[301]王岳军,范蔚茗,郭锋等.北大别晚中生代火山岩的地球化学特征及对北大别构造属性的启示[J].地学前缘,2003,10(4)：529-538.
[302]王岳军,范蔚茗,郭锋.北淮阳晚中生代火山岩定年及火山砾石地球化学：对大别灰色片麻岩隆升和中生代地层格架的约束[J].科学通报,2002,47(20)：1528-1534.
[303]牛漫兰,朱光,宋传中.郯庐断裂带中生代火山活动与深部过程[J].合肥工业大学学报(自然科学版),2001,24(2)：147-153.
[304]闫峻,刘海泉,宋传中等.长江中下游繁昌-宁芜火山盆地火山岩锆石U-Pb年代学及其地质意义[J].科学通报,2009,54(12)：1716-1724.
[305]张旗,简平,刘敦一等.宁芜火山岩的锆石SHRIMP定年及其意义[J].中国科学(D辑),2003，33(4)：309-314.
[306]张春彬.江苏句容早白垩世孢粉组合[J].古生物学报,1962,10(2)：246-286
[307]宋之琛,郑亚惠,刘金陵等.江苏地区白垩纪一第三纪孢粉组合[M].北京：地质出版社,1981.
[308]张一勇,李建国.江苏白垩纪孢粉组合序列[J].地层学杂志,2000，24(1)：65-71.
[309]周山富,王伟铭.江苏句容白垩纪葛村组花粉-新属及其地史分布[J].古生物学报,2001,40(4)：457-462.
[310]傅强,李益,张国栋等.苏北盆地晚白垩世-古新世海侵湖泊的证据及其地质意义[J].沉积学报,2007,25(3)：380-385.
[311]邢立达；王丰平；潘世刚等.重庆綦江中白垩统夹关组恐龙足迹群的发现及其意义[J].地质学报,2007,81(11)：1591-1604
[312]雷奕振.长江三峡地区生物地层学——白垩纪、第三纪分册[M].北京：地质出版社，1987.
[313]李伟同.中国当阳跑马岗组白垩-古近系界线附近的轮藻组合[J].微体古生物学报,2003,20(2)：183-186.
[314]俞云文,徐步台.浙江中生代晚期火山-沉积岩系层序和时代[J].地学前缘,1999，23(2)：136-145.
[315]张万良,李子颖.相山“流纹英安岩”单颗粒锆石U-Pb年龄及地质意义[J].岩石矿物学杂志,2007,26(1)：21-26.
[316]张家菁,施光海,童贵生等.浙江徐家墩鹅湖岭组含铜多金属矿火山岩的地球化学与年代学[J].地质学报,1999,83(6)：791-799.
[317]张利民.试论我国东部火山岩型铀矿床赋存层位的地质时代[J].铀矿地质,1996，12(3)：139-143.
[318]张万良.盛源盆地火山岩系地层的时代归属[J].铀矿地质,2000,16(2)：99-101.
[319]王勇,管太阳,黄国夫等.赣东北地区燕山晚期火山岩同位素年代学研究[J].地球学报,2002,23(3)：233-236.
[320]李坤英,沈加林,王小平.浙闽赣中生代陆相火山岩同位素年代学[J].中国地质科学院南京地质矿产研究所所刊,1989,(增刊)：87-132.
[321]张利民.江西中生代火山岩系地层划分及时代刍议[J].华东地质学院学报,1990，13(2)：9-14.
[322]余达淦,艾桂根等.江西周潭群同位素年龄特征及其地质意义[J].地球学报,1999,20(2)：195-200.
[323]梁诗经,文斐成,陈润生等.福建泰宁白垩纪红层植物及孢粉化石组合特征[J].福建地质,2006,25(1)：1-9.
[324]巫建华,张树明,周维勋.赣南-粤北版石群及其地质时代[J].地层学杂志,1999,23(3)：226-233.
[325]宋之琛,王鑫甫,钟林.三水盆地早白垩世白鹤洞组的被子植物花粉[J].古生物学报,1992,31(4)：501-512
[326]Miall A D. Architectural element analysis:a new method of facies analysis applied to fluvial deposits [J]. Earth-Science Review,1985,22:261-308.
[327]刘朋波,蒲仁海,刘娟霞.十屋断陷火石岭组-营城组沉积微相研究与储层识别[J].石油地球物理勘探,2009,44(3)：347-356.
[328]程日辉,刘万洙,王璞珺等.松辽盆地东缘下白垩统营城组二段火山碎屑沉积的过程、相和结构[J].吉林大学学报(地球科学版),2007,37(6)：1166-1175.
[329]郭峰,陈世悦,胡光明等.松辽盆地北部下白垩统地震相及沉积相分析[J].大庆石油地质与开发,2005,24(6)：20-24.
[330]王国栋,程日辉,王璞珺等.松科1井南孔白垩系泉头组沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：324-338.
[331]高有峰,王璞珺,程日辉等.松科1井南孔白垩系青山口组一段沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：314-323.
[332]王璞珺,高有峰,程日辉等.松科1井南孔白垩系青山口组二、三段沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：288-313.
[333]程日辉,王国栋,王璞珺等.松科1井南孔白垩系姚家组沉积序列精细描述：岩石地层、沉积相与旋回地层[J].地学前缘,2009,16(2)：272-287.
[334]韩建辉,王英民,李树青等.松辽盆地北部湖盆萎缩期层序结构与沉积充填[J].沉积学报.2009,27(3)：479-486
[335]邢德和,孙春林,孙跃武等.辽西金-羊盆地士城子组层序地层学[J].地质与资源,2006,15(3)：166-173.
[336]靳卫广,梅冥相.库车盆地白垩纪沙漠沉积体系的层序地层格架[J].断块油气田,2005,12(5)：17-20.
[337]程宏岗.楚雄中生代盆地原始盆地恢复及其演化：硕士学位论文.西安：西北大学,2004.
[338]李正芳.中扬子区晚侏罗世和白垩纪沉积古地理研究：硕士学位论文.北京：中国地质大学(北京),2009.
[339]李金良.胶莱盆地沉积分析及构造演化：博士学位论文.北京：中国地质科学院,2006.
[340]岳文浙,丁保良.江苏白垩纪陆相层序地层研究[J].资源调查与环境,1999，20(4)：287-344.
[341]白云风,程日辉,孔庆莹等.下扬子地区晚白垩世浦口期沉积古地理及地质背景[J].吉林大学学报(地球科学版),2007,37(4)：684-689.
[342]任红民,陈丽琼,王文军等.苏北盆地晚白垩世泰州期原型盆地恢复[J].石油实验地质,2008,30(1)：52-57.
[343]李思田,路风香,林畅松等.中国东部及临区中、新生代盆地演化及地球动力学背景[M].武汉：中国地质大学出版社,1997.
[344]Olsen, P E. Tectonic, climatic, and biotic modulation of lacustrine ecosystems-examples from Newark supergroup of Eastern North America. Lacustrine Basin Exploration:Case studies and modern analogs [J]. AAPG Memoir,1990,50,209-224.
[345]Carroll A R. Stratigraphic classification of ancient lakes Balancing tectonic and climatic controls [J]. Geology,1999,27 (2):99-102.
[346]Carroll A R. Lake-type controls on petroleum source rock potential in nonmarine basins. AAPG Bulletin [J],2001,85(6):1033-1053.
[347]Bohacs K M, Carroll A R. Lake-Basin type, source potential, and hydrocarbon character:an integrated sequence-stratigraphic geochemical framework [J]. AAPG Studies in Geology, 2000,46:3-34.
[348]A S Cohen. Paleolimnology:the History and Evolution of Lake Systerms [J]. M. New York, Oxford University Press,2003,211-213.
[349]殷洪福.中国古生物地理学[M].中国地质大学出版社：武汉.1988，250-270.
[350]陈丕基,云南中生代红层[M].科学出版社：北京.1975，31-48.
[351]Sha J G, Hiromichi H, Yao X G, et al. Late Mesozoic transgressions of eastern Heilongjiang and their significance in tectonics, and coal and oil accumulation in northeast China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2008,263 (3-4):119-130.
[352]葛肖虹,马文璞.东北亚南区中-新生代大地构造轮廓[J].中国地质,2007，34(2)：212-228.
[353]Sha Jingeng. Cretaceous stratigraphy of northeast China:non-marine and marine correlation [J]. Cretaceous research,2007,28:146-170.
[354]祝幼华,何承全.黑龙江省东部中侏罗世至早白垩世沟鞭藻组合序列[J].地层学杂志,2003,27(4)：282-289.
[355]何承全,孙学坤.黑龙江省东部鸡西盆地城子河组下部早白垩世欧特里夫晚期海相沟鞭藻类[J].古生物学报,2000,39(1)：46-62.
[356]Sha J G, Matsukawa M, Cai H W et al. The Upper Jurassic-Lower Cretaceous of eastern Heilongjiang, northeast China:stratigraphy and regional basin history[J]. Cretaceous research, 2003,24:715-728.
[357]Jiang B Y, Cai H W, Sha J G. Early Cretaceous Aucellina (bivalvia) from the Dajiashan area, northeastern China[J]. Journal of Asian Earth Sciences,2004,23:365-371.
[358]张松海,程立人,刘典涛.胶南地区莱阳群绒枝藻化石的发现[J].长春科技大学学报,2001,31(3)：209-212.
[359]李玉文.四川盆地白垩纪半咸水有孔虫和介形虫的发现及其意义[J].地质论评,1979,25(1)：2-11.
[360]Okada H. High sea-level vs. high sedimentation rates during the Cretaceous [J]. Geological Society of Japan Memoirs,1997,48,1-6.
[361]冯晓杰,张川燕,王春修等.东海陆架和台西南盆地中生界及其油气勘探潜力[J].中国海上油气(地质),2001,15(5)：306-311.
[362]郑绵平,赵元艺,刘俊英.第四纪盐湖沉积与古气候[J].第四纪研究,1998，4：297-307.
[363]Yaalon D H, Ward G D. Observations on calcrete and Recent calcic horizons in relation to landforms, central Namib Desert [J]. Palaeoecology of Africa and of the Surrounding Islands and Antarctica,1982,15:183-186.
[364]Glennie K W. Desert sedimentary environments, present and past [J]. Sedimentary Geology, 1987,50(1-3):135-165.
[365]江新胜,蔡习尧,潘忠习等.塔里木盆地西南部早白垩世风成沙丘古风向测量与古风带恢复[J].沉积与特提斯地质,2009,29(4)：1-4.
[366]江新胜,潘忠习,徐金沙等.江西信江盆地晚白垩世风成沙丘的发现及其古风向[J].地质通报,2006,25(7)：833-838.
[367]M Matsukawa, K Saiki, M Ito et al. Early Cretaceous terrestrial ecosystems in East Asia based on food-web and energy-flow models [J]. Cretaceous Research,2006,27:285-307.
[368]张旗,王元龙,金惟俊等.晚中生代的中国东部高原：证据、问题和启示[J].地质通报,2008,27(9)：1404-1430.
[369]邵济安,张履桥,肖庆辉,等.中生代大兴安岭的隆起：一种可能的陆内造山机制[J].岩石学报,2005,21(3)：789-794.
[370]刘训.中国西北盆山地区中-新生代古地理及地壳构造演化[J].古地理学报,2004，6(4)：448-458.
[371]李伍平,李献华.燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报,2004,20(3)：501-510.
[372]Hendrix M, Graham S, Caxroll A et al. Sedimentary record and climatic implication of recurrent deformation in the Tianshan:evidence from Mesozoic strata of the north Tarim, south Junggar, and Turpan basins, northwest China[J]. Geological Society of Ameriea Bulletin,1992,104(1):53-79
[373]Graham S, Hendrix M, Wang Z et al. Collisional successor basins of western China:impact of tectonic inheritance on sand composition [J]. Geological Society of America Bulletin, 1993,105 (3):323-344.
[374]吴根耀.白垩纪：中国及邻区板块构造演化的一个重要变换期[J].中国地质,2006，33(1)：64-77.
[375]袁四化,刘永江,葛肖虹等.阿尔金山中新生代隆升历史研究进展[J].世界地质,2006,25(2)：164-171.
[376]郑德文,张培震,万景林等.西秦岭北缘中生代构造活动的~(40)Ar/~(39)Ar、FT热年代学证据[J].岩石学报,2004，20(3)：697-706.
[377]唐玉虎,戴霜,黄永波等.兰州-民和盆地河口群沉积相和岩石磁化率——祁连山白垩纪隆升的记录[J].地学前缘,2008,15(2)：261-271.
[378]陈正乐,李丽,刘健等,西天山隆升-剥露过程初步研究[J].岩石学报,2008，24(4)：625-636.
[379]张传恒,刘典波,张传林等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1)：294-302.
[380]沈传波,梅廉夫,徐振平等.大巴山中-新生代隆升的裂变径迹证据[J].岩石学报,2007,23(11)：2901-2910.
[381]赵红格,刘池洋,王锋等.贺兰山隆升时限及其演化[J]中国科学(D辑),2007,37(增刊)：185-192.
[382]吴中海,吴珍汉.大青山晚白垩世以来的隆升历史[J].地球学报,2003，24(3)：205-210.
[383]郑德文,张培震,万景林等.六盘山盆地热历史的裂变径迹证据[J].地球物理学报,2005,48(1)：157-164.
[384]陈正乐,万景林,刘健等.西天山山脉多期次隆升-剥露的裂变径迹证据[J].地球学报,2006,27(2)：97-106.
[385]彭兆蒙,彭仕宓,吴智平等.华北东部侏罗-白垩纪盆地演化及其对构造运动的响应[J].西安石油大学学报(自然科学版).2009，24(5)：7-13.
[386]李小明,王岳军,谭凯旋等.云开地块中新生代隆升剥露作用的裂变径迹研究[J].科学通报,50(6)：577-583.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |