河南省侏罗—白垩纪沉积相与古地理研究
|
摘要
河南省中生代侏罗-白垩纪时期,受印支运动后期及燕山运动的影响,沉积了近30余山间坳陷、断陷(坳)小盆地,为全面开展全省侏罗-白垩纪沉积相与古地理研究奠定了基础。本文收集了东部隐伏区侏罗-白垩纪时期沉积的25口钻井资料,实测了包括济源盆地侏罗纪、马市坪晚侏罗-早白垩世、西峡盆地晚白垩世地层等露头较好的7条剖面;较详细地收集了大量野外一手资料,并采集了大量的岩石和化石样品,尤其是遗迹化石。
通过室内对岩样进行显微镜下观测和粒度分析,结合沉积学和遗迹学知识,得出河南省侏罗-白垩纪时期,主要为陆相沉积体系,局部为火山岩建造。研究区陆相沉积主要包括冲积扇、辫状河、曲流河及滨浅湖等4种沉积相,河漫湖泊、湖泊三角洲、深湖浊流及扇三角洲等4种沉积亚相,并建立了冲积扇-河流-湖泊体系沉积模式。
在济源盆地早侏罗世和西峡盆地晚白垩世地层中,详细描述及鉴定了14属21种遗迹化石。根据遗迹化石产状特征,及其与沉积物、沉积环境间的相互关系,在济源盆地中建立了代表湖泊浊流环境的鞍腰遗迹群落;在西峡盆地中建立了代表河流环境的Beaconites-Palaeophycus遗迹组构和代表湖泊环境的Beaconites- Taenidium遗迹组构。
以构造控盆思想为指导,遵循“点-线-面”编图原则,比较全面地恢复了研究区的构造、岩相古地理面貌,研究认为:早-中侏罗世时期,以淅川-桐柏-新县-商城为界,呈现南为山地,北为高地或平原的格局,以河湖相沉积为主;晚侏罗-早白垩世时期,盆地呈狭窄长条状展布,表现明显的走滑拉分盆地的性质,开始出现火山岩沉积;晚白垩世时期,盆地分布在豫西南地区,主要受断裂控制,表现为断陷、走滑性质,沉积以冲积体系为主。
本次研究充分反映了研究区沉积体系的时空演化特征,从而为油气、煤等矿产资源勘探提供了较为可靠的理论依据。
During the Jurassic-Cretaceous period, effected by the later stage of Indosinian orogeny and Yanshan movement, there are more than 30 of small intermountain depressions (fault) basins in Henan Province; it laid the foundation for fully studying the Jurassic-Cretaceous sedimentary facies and paleogeography. This paper has collected 25 drilling data of deposits in Jurassic-Cretaceous strata of concealed areas in the eastern Henan, measured 7 sections including outcrops of Jurassic in Jiyuan Basin, Upper Jurassic-Lower Cretaceous in mashiping Basin, Upper Cretaceous in Xixia Basin. Lots of first-hand field information has been collected in detail, including a large number of rock and fossil samples, especially trace fossils.
After the rock samples observation under a microscope and particle size analysis in laboratory,and combined with knowledges of sedimentology and ichnology, it is clear that there mainly were continental sedimentary system,locally construction of the volcanic rock in Jurassic-Cretaceous period in Henan Province. Continental deposits in the study area have 4 kinds of sedimentary facies including alluvial fan, braided stream, meandering stream, shallow lake;and 4 kinds of sedimentary sub-facies including flood lakes, lake delta, deep lake turbidite and fan delta, and establish a depositional model of alluvial fan -fluvial -lacustrine system.
14 genera and 21 species of trace fossils are described and identified in detail in the Early Jurassic strata in Jiyuan basin and Late Cretaceous strata in Xixia Basin. According to the occurrence features of trace fossils, and its relationship with sediments and sedimentary environment, the Anyao ichnocoenosis represented lake turbidite environment is established in Jiyuan basin; and the Beaconites-Palaeophycus ichnofabric generated in the fluvial environment and the Beaconites-Taenidium ichnofabric occurred in of lake environment are established in Xixia basin.
With the thought of Structure-controlled Basin Evolution as the guide, follow the "Point - Line - Area" map compilation principle, a more comprehensive study to restore the tectonic, lithofacies palaeogeography has been finished in the area.During the Early - Middle Jurassic period, take Xichuan - Tongbai - XinXian - Shangcheng for the sector, the mountains in the South, highlands or plains in the north, mainly were fluvial and lacustrine facies; During the Late Jurassic - Early Cretaceous, the basin was a shape of narrow strip distribution, showing characteristics of significant strike-slip pull-apart basin, and the volcanic deposits began to appear; During the Late Cretaceous period, the basin, dominated by the alluvial deposits, was located in southwest Henan, mainly controlled by faults, and had the characteristics of fault and strike-slip.
This study reflects the characteristics of space-time evolution of sedimentary systems in the study area, and provide a more reliable theoretical basis for the exploration of oil and gas, coal and other mineral resources.
通过室内对岩样进行显微镜下观测和粒度分析,结合沉积学和遗迹学知识,得出河南省侏罗-白垩纪时期,主要为陆相沉积体系,局部为火山岩建造。研究区陆相沉积主要包括冲积扇、辫状河、曲流河及滨浅湖等4种沉积相,河漫湖泊、湖泊三角洲、深湖浊流及扇三角洲等4种沉积亚相,并建立了冲积扇-河流-湖泊体系沉积模式。
在济源盆地早侏罗世和西峡盆地晚白垩世地层中,详细描述及鉴定了14属21种遗迹化石。根据遗迹化石产状特征,及其与沉积物、沉积环境间的相互关系,在济源盆地中建立了代表湖泊浊流环境的鞍腰遗迹群落;在西峡盆地中建立了代表河流环境的Beaconites-Palaeophycus遗迹组构和代表湖泊环境的Beaconites- Taenidium遗迹组构。
以构造控盆思想为指导,遵循“点-线-面”编图原则,比较全面地恢复了研究区的构造、岩相古地理面貌,研究认为:早-中侏罗世时期,以淅川-桐柏-新县-商城为界,呈现南为山地,北为高地或平原的格局,以河湖相沉积为主;晚侏罗-早白垩世时期,盆地呈狭窄长条状展布,表现明显的走滑拉分盆地的性质,开始出现火山岩沉积;晚白垩世时期,盆地分布在豫西南地区,主要受断裂控制,表现为断陷、走滑性质,沉积以冲积体系为主。
本次研究充分反映了研究区沉积体系的时空演化特征,从而为油气、煤等矿产资源勘探提供了较为可靠的理论依据。
During the Jurassic-Cretaceous period, effected by the later stage of Indosinian orogeny and Yanshan movement, there are more than 30 of small intermountain depressions (fault) basins in Henan Province; it laid the foundation for fully studying the Jurassic-Cretaceous sedimentary facies and paleogeography. This paper has collected 25 drilling data of deposits in Jurassic-Cretaceous strata of concealed areas in the eastern Henan, measured 7 sections including outcrops of Jurassic in Jiyuan Basin, Upper Jurassic-Lower Cretaceous in mashiping Basin, Upper Cretaceous in Xixia Basin. Lots of first-hand field information has been collected in detail, including a large number of rock and fossil samples, especially trace fossils.
After the rock samples observation under a microscope and particle size analysis in laboratory,and combined with knowledges of sedimentology and ichnology, it is clear that there mainly were continental sedimentary system,locally construction of the volcanic rock in Jurassic-Cretaceous period in Henan Province. Continental deposits in the study area have 4 kinds of sedimentary facies including alluvial fan, braided stream, meandering stream, shallow lake;and 4 kinds of sedimentary sub-facies including flood lakes, lake delta, deep lake turbidite and fan delta, and establish a depositional model of alluvial fan -fluvial -lacustrine system.
14 genera and 21 species of trace fossils are described and identified in detail in the Early Jurassic strata in Jiyuan basin and Late Cretaceous strata in Xixia Basin. According to the occurrence features of trace fossils, and its relationship with sediments and sedimentary environment, the Anyao ichnocoenosis represented lake turbidite environment is established in Jiyuan basin; and the Beaconites-Palaeophycus ichnofabric generated in the fluvial environment and the Beaconites-Taenidium ichnofabric occurred in of lake environment are established in Xixia basin.
With the thought of Structure-controlled Basin Evolution as the guide, follow the "Point - Line - Area" map compilation principle, a more comprehensive study to restore the tectonic, lithofacies palaeogeography has been finished in the area.During the Early - Middle Jurassic period, take Xichuan - Tongbai - XinXian - Shangcheng for the sector, the mountains in the South, highlands or plains in the north, mainly were fluvial and lacustrine facies; During the Late Jurassic - Early Cretaceous, the basin was a shape of narrow strip distribution, showing characteristics of significant strike-slip pull-apart basin, and the volcanic deposits began to appear; During the Late Cretaceous period, the basin, dominated by the alluvial deposits, was located in southwest Henan, mainly controlled by faults, and had the characteristics of fault and strike-slip.
This study reflects the characteristics of space-time evolution of sedimentary systems in the study area, and provide a more reliable theoretical basis for the exploration of oil and gas, coal and other mineral resources.
引文
[1]冯增昭,曾允孚.岩相古地理基础和工作方法[M].地质出版社,1985,1-442
[2]冯增昭.我国古地理学的形成、发展与展望[J].古地理学报,1999,1(2):1-7
[3]李通艺.东亚地体构造演化研究的回顾与展望[J].科学发展月刊,2000,28(10):754-763
[4]王鸿祯.地史学教程[M].北京:地质出版社,1965.1-396
[5]王鸿祯.中国古地理图集[M].北京:地图出版社,1985.1-85(中文),1-28(英文)
[6]王鸿祯,刘本培.地史学教程[M].北京:地质出版社,1980.1-352
[7]刘本培.地史学教程[M].北京:地质出版社,1986.1-408
[8]王竹泉.北华地台上古生代含煤地层分布之规律及其古地理.见:中国煤田地质总局选辑.王竹泉选集[M].北京:煤炭工业出版社,1959.267-283
[9]王竹泉.华北地台石炭纪岩相古地理[M].见:中国煤田地质局选辑.王竹泉选集.北京:煤炭工业出版社,1964.284-300
[10]冯增昭主编.沉积岩石学,上下册[M].北京:中国工业出版社,1993.1-368(上册),1-327(下册)
[11]关士聪.中国海陆变迁海域沉积相与油气[M].北京:科学出版社,1984.1-104,图1-25
[12]刘宝珺,许效松.中国南方岩相古地理图集[M].北京:科学出版社,1994.1-188
[13]孟祥化,葛铭.中朝板块层序,事件,演化[M].北京:科学出版社,2005.6
[14]河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1989.215-378,676-677
[15]胡斌,王冠忠,齐永安.痕迹学理论与应用[M].北京:中国矿业大学出版社,1997,1-209
[16]张国成,李继亮.陆相遗迹相研究的新进展[J].地质科技情报,1997,16(4):49-54
[17]吴贤涛.豫西济源—义马盆地浊流沉积中的痕迹化石及其环境意义[J].沉积学报,1985,3(3):23-31
[18] Buatois L A, Mangano M G, Wu Xiantao,Zhang Guocheng. Trace fossils from Jurassic lacustrine turbidites of the Anyao Formation (central China) and their environmental and evolutionary significance[J]. Ichnos,1996,5(4):287-301
[19]胡斌,黄长春,张宏敏,徐亚福.豫西济源晚三叠世河流沉积类型及生物痕迹组构特征[J].河南地质,2000,18(3):176-180
[20]胡斌,张国成,郭卫星,齐永安,张利伟.豫西济源谭庄组河流沉积中的Stipsellus遗迹组构[J].煤田地质与勘探,2004,32(3):1-5
[21]张国成,曾玉凤,Buatois LA,Mangano MG.济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征[J].沉积学报,2005,23(1):100-107
[22]齐永安,胡斌,张国成,龚一鸣.豫西济源地区中三叠世油房庄组遗迹组构及其环境解释[J].沉积学报,2007.25(3):372-379
[23]张国成,郭卫星,曾玉凤.河南西峡盆地上白垩统河流及湖泊沉积中的遗迹组构[J].古地理学报,2004,6(4):434-441
[24]宋慧波,胡斌,王德有,刘顺喜,高勇,钟明洋.河南西峡盆地上白垩统高沟组沉积特征与沉积环境[J].石油地质与工程,2007,22(4):1-3
[25]胡斌,吴贤涛,潘丽敏.川西峨眉晚古生代和中生代河流沉积中的痕迹化石群落[J].沉积学报,1991,9(4):128-135
[26]胡斌,吴贤涛.川西峨眉晚白垩世夹关期河流沉积中的痕迹化石群落[J].古生物学报,1993,32(4):478-489
[27]张建平,薛叔浩,杨式溥,吴因业.新疆吐哈盆地侏罗纪湖相动物遗迹化石的发现及古环境意义[J].现代地质,2000,14(3):373-378
[28]郑玉龙,陈春瑞,任林伟.松辽盆地上白垩统陆相遗迹化石及其沉积环境[J].古地理学报,2005,7(3):337-346
[29]蔡雄飞,李长安,占车生.民和盆地下白垩统遗迹化石的类型与气候的关系[J].沉积与特提斯地质.2001,21(2):84-90
[30]李日辉,张光威.山东莱阳盆地早白垩世莱阳群的遗迹化石[J].古生物学报,2001,40(2):252-261
[31]王慧中.东营凹陷沙河街组生物扰动构造半定量分析试验[J].地质科学,1996,31(3):287-296
[32]李应暹,卢宗盛,王丹等.辽河盆地陆相遗迹化石与沉积环境研究[M].石油工业出版社,1997,1-145
[33] Bin Hu,Jiang zaixing,Qi yongan,Zhang guocheng.Paleogene ichnocoenoses of lacustrine deposits in Jiyang Depression of Shandong Province,Eastern China.Journal of University of Geosciences,2007,18(special issue):404-405
[34]胡斌,齐永安,张国成,姜在兴.中国中-新生代陆相沉积中的遗迹群落[J].沉积学报,2002,20(4):547-581
[35]河南省地质矿产厅编著(席文祥、裴放主编).河南省岩石地层[M],武汉:中国地质大学出版社,1997,1-299
[36]周世全,赵树林,朱广彬,王保湘.中国南阳恐龙蛋[M].武汉:中国地质大学出版社,2005,1-97
[37]王德有,冯进城等著.中国河南恐龙蛋和恐龙化石[M].地质出版社,2008,1-320
[38]潘泽成,徐莉,席运宏,贾松海.河南省地层古生物研究(第五分册中生代)[M].黄河水利出版社:2008,1-821
[39]陈传诗,苏现波,曹运兴.河南省中生代聚煤盆地分析[M].北京:地质出版社,1995.3-56
[40]刘司红,刘西宁,李平和.洛阳一伊川盆地构造演化特征及含油气远景评价[J],地质与资源,2003,12(4):228-232
[41]王定一,王立宝.留山、马市坪盆地构造特征及其形成演化[J].石油与天然气地质,1993.14(1):53-60
[42]陈传诗,苏现波.断块运动与中生代济源盆地的演化[J].岩相古地理,1995. 1(15):18-23
[43]张功成.济源凹陷盆地结构构造特征与油气勘探前景[J].断块油气田,1997,4(5),5-11
[44]吴富强,程哲等.河南省侏罗纪盆地初探[J].河南石油,1997.4
[45]王德有,罗铭玖,周世全等.西峡盆地晚白垩世古气候初探[J].河南地质,1994. 9(12)
[46]周世全,梁新权,冯祖杰.河南西南部含恐龙蛋化石盆地沉积及构造特征[J].大地构造与成矿学,2002,26(3):306-313
[47]张国成.河南西峡晚白垩世盆地的沉积演化[J].焦作工学院学报(自然科学版),2002,21(2):85-90
[48]孙家振,韦必则,熊保贤,郑用华.周口凹陷形成机制及其与大别造山带的耦合关系[J].地学前缘,1995,2(3-4):248-251
[49]孙自明.周口坳陷的反转构造与构造演化[J].石油地球物理勘探,1998,33(2):251-257
[50]孙自明,熊保贤.周口坳陷的逆冲推覆构造特征[J].石油勘探与开发,1999,26(3):22-24
[51]黄杏珍,何明喜等.中国河南省白湾盆地的白垩系特征[J].沉积学报,1996,14增刊:38-48
[52]胡斌,张利伟,齐永安,郭卫星.济源下侏罗统鞍腰组沉积构造特征及环境解释[J].焦作工学院学报(自然科学版),2004.1(23)
[53]胡斌,钟明洋,宋慧波,刘顺喜.豫西南马市坪盆地上侏罗统-下白垩统沉积特征及演化序列[J].石油地质与工程,2009,23(5):1-3
[54]黄长春,胡斌.济源上三叠统含煤含油地层中的痕迹组构[J].河南石油,1998,(5):5-7
[55]徐汉林,赵宗举,吕福亮,杨以宁,汤祖伟,孙国忠,徐云俊.南华北地区的构造演化与含油气性[J].大地构造与成矿学,2004,28(4):450-463
[56]董树文,张岳桥,龙长兴,杨振宇,季强,王涛,胡建民,陈宣华.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
[57]任纪舜,王作勋,陈炳蔚,姜春发,牛宝贵,李锦轶,谢广连,和政军,刘志刚.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.
[58]崔盛芹,李锦蓉,吴珍汉,易明初,沈淑敏,尹华仁,马寅生.燕山地区中新生代陆内造山[M].北京:地质出版社:2002,1-386.
[59]陈传诗,曹运兴.河南义马盆地侏罗—白垩纪充填形变史[J].河南地质,1989,7(3):37-43
[60]郑求根,张育民,赵德勇,刘志勤,彭国力.豫西地区构造演化与上三叠统地层保存和分析[J].河南石油,1998,2:6-10
[61]孔庆莹,程日辉,胡艳飞.周口坳陷谭庄-沈丘凹陷早白垩世沉积相类型和层序地层特征[J].吉林大学学报(地球科学版),2006,36(4):557-562
[62]王德有,罗铭玖,周世全等.河南西峡盆地晚白垩世古气候[A].见罗铭玖主编:河南地质矿产环境文集[C].北京:中国环境科学出版社.1996.41-47
[63]周世全,罗铭玖,王德有,张克伟,李俊峰.豫西南晚白垩世时代研究的进展[J].地层学杂志,1997,21(2):151-155
[64]陈金华,王德有,冯进城,符光宏,朱世刚.河南西峡盆地晚白垩世含恐龙蛋地层中的双壳类[J].古生物学报,2007,46(3):299-313
[65]潘华璋,王德有,冯进城,符光宏,朱世刚.河南西峡盆地晚白垩世含恐龙蛋地层中的腹足类[J].古生物学报,2007,46(3):293-298
[66]席文祥,巴光进,亢进法.豫西卢氏县朱阳关组的建立[J].中国区域地质,1994,(4):298-299
[67]朱广彬,周世全.河南卢氏五里川盆地晚白垩世地层[J].华南地质与矿产,2002,(4):28-34
[68]周世全,朱广彬,冯祖杰,河南内乡夏馆—高丘盆地的夏馆组及其时代[J].资源调查与环境,2003,24(1):69-74
[69] Seilacher, A. . Biogenic sedimentary structures. in Imbrie, J. and Newe11[J], N. (eds), Approaches to Plaeoecology. New York: Wiley, 1964: p. 296-316.
[70] Frey, R. W. (ed).The Study of Trace Fossils. Sprinter-Verlag, New York. 1975
[71] Bromley,R. G. .Trace Fossils Biology and Taphonomy. Unwin, Hyman,London. 1990
[72] Ekdale, A. A. ,Bromley,R. G. and Pemberton,S. G., Ichnology. Soc. Econ. Paleontol. Mineral. Tulsa, Oklahoma. 1984
[73] Curran, H. A. (ed).Biogenic Structures; Their Use in Interpreting Depositional Environments. SEPM Spec. 1985 Publs. 35.
[74] Bottjer, D. J. ,Droser,M. L. and Jablonski,D.Bathymetric trends in the history of trace fossils.in Bottjer,D.J.(ed), New concepts in the use of biogenic sedimentary structures for paleoenvironmental interpretation. Los Angeles: Pacific Section SEPM. 1987, 57-65.
[75] Wetzel, A.Ecologic interpretation of deep-sea trace fossil communitites. Palaeogeogr.,Palaeoclimatol. Palaeoecol. 1991, 85:47-69.
[76]杨式溥.遗迹化石的古环境和古地理意义[J].古地理学报,1999,1(1):7-19
[77]杨式溥.遗迹化石及其古环境分析的意义[J].沉积学报,1984a,2(4):8-180
[78]晋慧娟,李育慈.准噶尔盆地晚古生代深水斜坡沉积中的遗迹相及其环境分析[J].中国科学,B辑,1991,(4):408-415
[79]周志澄.生物成因的构造在环境解释中的应用[J].古生物学报,1995,34(2):228-249
[80] Buatois L A,Mangano M G.The paleoenvironmental and paleoecological significance of the lacustrine Mermia ichnofacies:an archethpical subaqueous nonmarine trace fossil assemblage[J].Ichnos,1995,4:151-161
[81]齐永安,王敏.遗迹组构研究现状及进展[J].河南理工大学学报(自然科学版),2007,26(5):509-519
[82] Bin Hu,Guanzhong Wang,Roland Goldring.Nereites or Neonereites from Lower Jurassic lacustrine turbidites of Henan,central China[J].Ichnos,1998(2):1-7.
[83]蒋维红,董春梅,闫家宁.岩相古地理学研究现状及发展趋势[J].断块油气田,2007,14(3):1-3
[2]冯增昭.我国古地理学的形成、发展与展望[J].古地理学报,1999,1(2):1-7
[3]李通艺.东亚地体构造演化研究的回顾与展望[J].科学发展月刊,2000,28(10):754-763
[4]王鸿祯.地史学教程[M].北京:地质出版社,1965.1-396
[5]王鸿祯.中国古地理图集[M].北京:地图出版社,1985.1-85(中文),1-28(英文)
[6]王鸿祯,刘本培.地史学教程[M].北京:地质出版社,1980.1-352
[7]刘本培.地史学教程[M].北京:地质出版社,1986.1-408
[8]王竹泉.北华地台上古生代含煤地层分布之规律及其古地理.见:中国煤田地质总局选辑.王竹泉选集[M].北京:煤炭工业出版社,1959.267-283
[9]王竹泉.华北地台石炭纪岩相古地理[M].见:中国煤田地质局选辑.王竹泉选集.北京:煤炭工业出版社,1964.284-300
[10]冯增昭主编.沉积岩石学,上下册[M].北京:中国工业出版社,1993.1-368(上册),1-327(下册)
[11]关士聪.中国海陆变迁海域沉积相与油气[M].北京:科学出版社,1984.1-104,图1-25
[12]刘宝珺,许效松.中国南方岩相古地理图集[M].北京:科学出版社,1994.1-188
[13]孟祥化,葛铭.中朝板块层序,事件,演化[M].北京:科学出版社,2005.6
[14]河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1989.215-378,676-677
[15]胡斌,王冠忠,齐永安.痕迹学理论与应用[M].北京:中国矿业大学出版社,1997,1-209
[16]张国成,李继亮.陆相遗迹相研究的新进展[J].地质科技情报,1997,16(4):49-54
[17]吴贤涛.豫西济源—义马盆地浊流沉积中的痕迹化石及其环境意义[J].沉积学报,1985,3(3):23-31
[18] Buatois L A, Mangano M G, Wu Xiantao,Zhang Guocheng. Trace fossils from Jurassic lacustrine turbidites of the Anyao Formation (central China) and their environmental and evolutionary significance[J]. Ichnos,1996,5(4):287-301
[19]胡斌,黄长春,张宏敏,徐亚福.豫西济源晚三叠世河流沉积类型及生物痕迹组构特征[J].河南地质,2000,18(3):176-180
[20]胡斌,张国成,郭卫星,齐永安,张利伟.豫西济源谭庄组河流沉积中的Stipsellus遗迹组构[J].煤田地质与勘探,2004,32(3):1-5
[21]张国成,曾玉凤,Buatois LA,Mangano MG.济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征[J].沉积学报,2005,23(1):100-107
[22]齐永安,胡斌,张国成,龚一鸣.豫西济源地区中三叠世油房庄组遗迹组构及其环境解释[J].沉积学报,2007.25(3):372-379
[23]张国成,郭卫星,曾玉凤.河南西峡盆地上白垩统河流及湖泊沉积中的遗迹组构[J].古地理学报,2004,6(4):434-441
[24]宋慧波,胡斌,王德有,刘顺喜,高勇,钟明洋.河南西峡盆地上白垩统高沟组沉积特征与沉积环境[J].石油地质与工程,2007,22(4):1-3
[25]胡斌,吴贤涛,潘丽敏.川西峨眉晚古生代和中生代河流沉积中的痕迹化石群落[J].沉积学报,1991,9(4):128-135
[26]胡斌,吴贤涛.川西峨眉晚白垩世夹关期河流沉积中的痕迹化石群落[J].古生物学报,1993,32(4):478-489
[27]张建平,薛叔浩,杨式溥,吴因业.新疆吐哈盆地侏罗纪湖相动物遗迹化石的发现及古环境意义[J].现代地质,2000,14(3):373-378
[28]郑玉龙,陈春瑞,任林伟.松辽盆地上白垩统陆相遗迹化石及其沉积环境[J].古地理学报,2005,7(3):337-346
[29]蔡雄飞,李长安,占车生.民和盆地下白垩统遗迹化石的类型与气候的关系[J].沉积与特提斯地质.2001,21(2):84-90
[30]李日辉,张光威.山东莱阳盆地早白垩世莱阳群的遗迹化石[J].古生物学报,2001,40(2):252-261
[31]王慧中.东营凹陷沙河街组生物扰动构造半定量分析试验[J].地质科学,1996,31(3):287-296
[32]李应暹,卢宗盛,王丹等.辽河盆地陆相遗迹化石与沉积环境研究[M].石油工业出版社,1997,1-145
[33] Bin Hu,Jiang zaixing,Qi yongan,Zhang guocheng.Paleogene ichnocoenoses of lacustrine deposits in Jiyang Depression of Shandong Province,Eastern China.Journal of University of Geosciences,2007,18(special issue):404-405
[34]胡斌,齐永安,张国成,姜在兴.中国中-新生代陆相沉积中的遗迹群落[J].沉积学报,2002,20(4):547-581
[35]河南省地质矿产厅编著(席文祥、裴放主编).河南省岩石地层[M],武汉:中国地质大学出版社,1997,1-299
[36]周世全,赵树林,朱广彬,王保湘.中国南阳恐龙蛋[M].武汉:中国地质大学出版社,2005,1-97
[37]王德有,冯进城等著.中国河南恐龙蛋和恐龙化石[M].地质出版社,2008,1-320
[38]潘泽成,徐莉,席运宏,贾松海.河南省地层古生物研究(第五分册中生代)[M].黄河水利出版社:2008,1-821
[39]陈传诗,苏现波,曹运兴.河南省中生代聚煤盆地分析[M].北京:地质出版社,1995.3-56
[40]刘司红,刘西宁,李平和.洛阳一伊川盆地构造演化特征及含油气远景评价[J],地质与资源,2003,12(4):228-232
[41]王定一,王立宝.留山、马市坪盆地构造特征及其形成演化[J].石油与天然气地质,1993.14(1):53-60
[42]陈传诗,苏现波.断块运动与中生代济源盆地的演化[J].岩相古地理,1995. 1(15):18-23
[43]张功成.济源凹陷盆地结构构造特征与油气勘探前景[J].断块油气田,1997,4(5),5-11
[44]吴富强,程哲等.河南省侏罗纪盆地初探[J].河南石油,1997.4
[45]王德有,罗铭玖,周世全等.西峡盆地晚白垩世古气候初探[J].河南地质,1994. 9(12)
[46]周世全,梁新权,冯祖杰.河南西南部含恐龙蛋化石盆地沉积及构造特征[J].大地构造与成矿学,2002,26(3):306-313
[47]张国成.河南西峡晚白垩世盆地的沉积演化[J].焦作工学院学报(自然科学版),2002,21(2):85-90
[48]孙家振,韦必则,熊保贤,郑用华.周口凹陷形成机制及其与大别造山带的耦合关系[J].地学前缘,1995,2(3-4):248-251
[49]孙自明.周口坳陷的反转构造与构造演化[J].石油地球物理勘探,1998,33(2):251-257
[50]孙自明,熊保贤.周口坳陷的逆冲推覆构造特征[J].石油勘探与开发,1999,26(3):22-24
[51]黄杏珍,何明喜等.中国河南省白湾盆地的白垩系特征[J].沉积学报,1996,14增刊:38-48
[52]胡斌,张利伟,齐永安,郭卫星.济源下侏罗统鞍腰组沉积构造特征及环境解释[J].焦作工学院学报(自然科学版),2004.1(23)
[53]胡斌,钟明洋,宋慧波,刘顺喜.豫西南马市坪盆地上侏罗统-下白垩统沉积特征及演化序列[J].石油地质与工程,2009,23(5):1-3
[54]黄长春,胡斌.济源上三叠统含煤含油地层中的痕迹组构[J].河南石油,1998,(5):5-7
[55]徐汉林,赵宗举,吕福亮,杨以宁,汤祖伟,孙国忠,徐云俊.南华北地区的构造演化与含油气性[J].大地构造与成矿学,2004,28(4):450-463
[56]董树文,张岳桥,龙长兴,杨振宇,季强,王涛,胡建民,陈宣华.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
[57]任纪舜,王作勋,陈炳蔚,姜春发,牛宝贵,李锦轶,谢广连,和政军,刘志刚.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.
[58]崔盛芹,李锦蓉,吴珍汉,易明初,沈淑敏,尹华仁,马寅生.燕山地区中新生代陆内造山[M].北京:地质出版社:2002,1-386.
[59]陈传诗,曹运兴.河南义马盆地侏罗—白垩纪充填形变史[J].河南地质,1989,7(3):37-43
[60]郑求根,张育民,赵德勇,刘志勤,彭国力.豫西地区构造演化与上三叠统地层保存和分析[J].河南石油,1998,2:6-10
[61]孔庆莹,程日辉,胡艳飞.周口坳陷谭庄-沈丘凹陷早白垩世沉积相类型和层序地层特征[J].吉林大学学报(地球科学版),2006,36(4):557-562
[62]王德有,罗铭玖,周世全等.河南西峡盆地晚白垩世古气候[A].见罗铭玖主编:河南地质矿产环境文集[C].北京:中国环境科学出版社.1996.41-47
[63]周世全,罗铭玖,王德有,张克伟,李俊峰.豫西南晚白垩世时代研究的进展[J].地层学杂志,1997,21(2):151-155
[64]陈金华,王德有,冯进城,符光宏,朱世刚.河南西峡盆地晚白垩世含恐龙蛋地层中的双壳类[J].古生物学报,2007,46(3):299-313
[65]潘华璋,王德有,冯进城,符光宏,朱世刚.河南西峡盆地晚白垩世含恐龙蛋地层中的腹足类[J].古生物学报,2007,46(3):293-298
[66]席文祥,巴光进,亢进法.豫西卢氏县朱阳关组的建立[J].中国区域地质,1994,(4):298-299
[67]朱广彬,周世全.河南卢氏五里川盆地晚白垩世地层[J].华南地质与矿产,2002,(4):28-34
[68]周世全,朱广彬,冯祖杰,河南内乡夏馆—高丘盆地的夏馆组及其时代[J].资源调查与环境,2003,24(1):69-74
[69] Seilacher, A. . Biogenic sedimentary structures. in Imbrie, J. and Newe11[J], N. (eds), Approaches to Plaeoecology. New York: Wiley, 1964: p. 296-316.
[70] Frey, R. W. (ed).The Study of Trace Fossils. Sprinter-Verlag, New York. 1975
[71] Bromley,R. G. .Trace Fossils Biology and Taphonomy. Unwin, Hyman,London. 1990
[72] Ekdale, A. A. ,Bromley,R. G. and Pemberton,S. G., Ichnology. Soc. Econ. Paleontol. Mineral. Tulsa, Oklahoma. 1984
[73] Curran, H. A. (ed).Biogenic Structures; Their Use in Interpreting Depositional Environments. SEPM Spec. 1985 Publs. 35.
[74] Bottjer, D. J. ,Droser,M. L. and Jablonski,D.Bathymetric trends in the history of trace fossils.in Bottjer,D.J.(ed), New concepts in the use of biogenic sedimentary structures for paleoenvironmental interpretation. Los Angeles: Pacific Section SEPM. 1987, 57-65.
[75] Wetzel, A.Ecologic interpretation of deep-sea trace fossil communitites. Palaeogeogr.,Palaeoclimatol. Palaeoecol. 1991, 85:47-69.
[76]杨式溥.遗迹化石的古环境和古地理意义[J].古地理学报,1999,1(1):7-19
[77]杨式溥.遗迹化石及其古环境分析的意义[J].沉积学报,1984a,2(4):8-180
[78]晋慧娟,李育慈.准噶尔盆地晚古生代深水斜坡沉积中的遗迹相及其环境分析[J].中国科学,B辑,1991,(4):408-415
[79]周志澄.生物成因的构造在环境解释中的应用[J].古生物学报,1995,34(2):228-249
[80] Buatois L A,Mangano M G.The paleoenvironmental and paleoecological significance of the lacustrine Mermia ichnofacies:an archethpical subaqueous nonmarine trace fossil assemblage[J].Ichnos,1995,4:151-161
[81]齐永安,王敏.遗迹组构研究现状及进展[J].河南理工大学学报(自然科学版),2007,26(5):509-519
[82] Bin Hu,Guanzhong Wang,Roland Goldring.Nereites or Neonereites from Lower Jurassic lacustrine turbidites of Henan,central China[J].Ichnos,1998(2):1-7.
[83]蒋维红,董春梅,闫家宁.岩相古地理学研究现状及发展趋势[J].断块油气田,2007,14(3):1-3