辽宁西部义县组地层及古地理特征
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摘要
本文在广泛收集前人资料的基础上,对辽宁西部地区义县组的研究现状进行了归纳和总结。在野外地质调查和综合分析前人资料的基础上,运用地层学、同位素地质学、岩石学、地球化学、构造地质学、古生物学及古地理学等多学科相结合的研究方法,并参考现代生物学和地理学等研究手段,重点对义县、金岭寺—羊山(简称金-羊)、建昌和凌源—三十家子四个盆地义县组发育特征、时空分布及变化规律、化石产出层位、火山岩特征、构造演化特点和其沉积时期的古环境等进行了系统而深入的调查研究。将义县组重新划分为四个岩性段,确定了六个含化石层位,提出了沉积层具有指状分插特征,较好的解决了重要(珍稀)化石层位之间的对比等问题。在北票-义县地区义县组一段首次发现了鹦鹉嘴龙化石,丰富了热河生物群的研究内容;在义县组二段发现了湖相枕状熔岩,确定为同沉积火山喷发。将义县组火山喷发旋回划分为四个亚旋回及若干个小旋回,指出了火山活动具有由两向东迁移的规律性。认为义县组沉积时期总体上反映是一种亚热带-暖温带、半干旱-半潮湿而又富于季节性变化的气候、半～微咸水-淡水及河流相(局部发育冲积扇相)-湖相沉积环境,在此基础上,对义县组进行了岩相古地理分析,并编制了岩相古地理图。
The author has measured a series of typical sections of the Yixian Formation in west Liaoning and collected a lot of samples and fossils through the geological survey for 3 years. This paper makes a comprehensive research on the stratigraphy and paleogeographic characters of the formation by means of petrology, paleontology, structural geology, geochemistry and isotopic chronology. This research focuses on the Mesozoic basins yielding the Yixian Formation, including Yixian Basin, Jinlingsi-Yangshan Basin, Jianchang Basin and Lingyuan-Sanshijiazi Basin. Based on the characters of volcanic cycles, petrology and paleontology of the Yixian Formation, the author makes a systematic division and correlation of the Yixian Formation in the four basins. This paper discusses also the characters of paleostructure and lithofacies paleogeography. The study is significant to the correlation of fossil-bearing strata intercalated with volcanic beds in western Liaoning, and is helpful to the exploration and protection of relevant volcanic mineral resources. The discussion on the paleostructure and lithofacies paleogeography is useful to the study of geological history that is concerned about the origin and evolution of bird and angiosperm. Meanwhile, this will be beneficial for the study of paleogeography, volcanic activity and the evolution of organic-inorganic events.The new subdivisions and paleogeographic comparison of the Yixian Formation in western Liaoning are as follows:The Yixian Formation can be subdivided into four members. The first member of Yixian Formation is the member of sandstone-conglomerate and basic -intermediate-basic volcanic rocks, which are widely distributed in the study area
with the exception of sandstone-conglomerate, only occurred in the Yixian Basin and the Jinlingsi-Yangshan Basin. There are 4 fossil-bearing beds occurred in the first member of Yixian Formation. Two fossil beds with gastropods, bivalves, conchostracnas and ostracods were found in tuffite and tuffaceous sandstones of the Yixian Basin. Four fossil beds were found in the Jinlingsi-Yanshan Basin with the fossils of gastropods, bivalves, conchostraca, ostracods, dinosaurs and fossil wood occurred in the bottom sandstone and conglomerate, including Psittacosaurus occurred in upper part of tuffite, tuff and tuffaceous sandstones. The second member of the Yixian Formation is mainly composed of lacustrine volcanic-sedimentary rocks with broad distributions. There are lot of fossils belonging to the Jehol Biota occurred, including Sinosawopteryx, Confuciusornis and Archeafurctus liaoningensis. The author firstly discovered the pillow lava in the second member, which is interbeded into the fossil beds as "finger" shape. The isotopic data of the pillow lava provided important evidence for the age of the Yixian Formation and for the resolve of the fossil beds comparison problems. The third member of the Yixian Formation is mainly of intermediate-basic -intermediate-acidic volcanic rocks with wide distributions. The fourth member of Yixian Formation is of sedimentary rocks and acidic volcanic rocks that are mainly distributed in the Yixian Basin and Jinlingsi-Yanshan Basin. The upper part of the fourth member in the Yixian Basin, which is mainly of fish fossils, is also important fossil beds of Yixian Formation. It seems to have the characters of migration in the four members of the Yixian Formation from the west to the east influenced by volcanic activity center and the structural position indicated as the various strata thickness between different basins.Based on the study of petrology of volcanic rocks and the regularity of volcanism, the volcanic eruption cycle of the Yixian Formation is subdivided into four sub-cycles correspond respectively to the four lithologic members of the Yixian Formation. The sub-cycles can also further be subdivided into some smaller cycles. The research reveals the regularity for the migration of volcanic eruption in the sequence of basic - intermediate-basic - intermediate - acidic (alkaline) from early to late and from west to east. There is an obvious correlation between the sub-cycles. The Jianchang basin and Lingyuan-Sanshijiazi basin are situated in the transitional zone of the younger Mesozoic northern Hebei-west Liaoning volcanic rock province. In the Jianchang basin, along with the Jin-Yang and Yixian basins in the east, the sub-cycle migrates southeastwards. While in the Lingyuan-Sanshijiazi basin and the Pingquan basin in west, the migration is from southeast to northwest. Geochemical study shows that during the No.I sub-cycle, the magma in the Jianchang basin evolved from basic to intermediate; in No. II
sub-cycle, intermediate magma was dominated; while in No.IlI, it was mainly acidic-alkaline, with intermediate in the east. It is a calc-alkaline volcanic suite in general. In the Jin-Yang basin, the magmatic evolution in No.I sub-cycle was dominated by basic calc-alkaline rock series, the No. II sub-cycle was an intermediate-basic alkaline series, and the No. Ill was a basic calc-alkaline rock series. On the other hand, in the Yixian basin, magma evolved from basic to intermediate calc-alkaline/alkaline volcanic suite during the No.I sub-cycle; the No.II sub-cycle showed an intermediate-basic alkaline suite; in the No.III sub-cycle, it evolved from intermediate to alkaline, from calc-alkaline to alkaline suite; while the No.IV was in intermediate-acidic, calc-alkaline evolving to alkaline. Meanwhile, in the Lingyuan-Sanshijiazi basin, the magma evolution during the No.I sub-cycle presented intermediate and acidic; magmatism was not seen; and the No. Ill was acid. It is generally alkaline rock series. According to the structural environment differentiation by REE, the volcanic rocks were formed by the upward invasion of inner-plate basalt in the continental extension environment. It was derived from the HREE-enriched mantle, most likely from the same magma source. From No.I to No.IV sub-cycles, the hybridization became more and more intensive.By analysis on the paleostructure and lithofacies paleogeography of the Tuchengzi Formation before the Yixian Formation formed, it is concluded that, the regional principle stress field was NWW-SEE compression, which made the NE- or NNE-trending distributions of the Tuchengzi Formation in the studied area. Based on the distributions of the basin-controlling faults and main mobile faults during the developing stage of the Yixian Formation, as well as the regularity of volcanism in the Yixian Formation, the regional principle stress field in that time converted from NWW-SEE to S-N direction, which formed the NW-SE extension. The faulting becomes more intensive from west to east or southeast. From west to east, the types of the basins change from the depression-fault type (such as the Lingyuan-Sanshijiazi basin), though the semi-graben-fault-depression (such as the Jianchang and Jin-Yang basins) to the typical fault-depression type (the Yixian basin). Generally, the basin marginal faults on the east margin evidently control the distributions of the Yixian Formation.Synthetically applying the sedimentary environment, palaeobiological features, combined with the geochemical features of sedimentary rocks, the climate condition is regarded as warm temperate zone with seasonal arid or semi-arid climate condition during the Yixian stage. The climate is obviously different from Tuchengzi stage.The first member of the Yixian Formation mainly consists of fluvial facies
The author has measured a series of typical sections of the Yixian Formation in west Liaoning and collected a lot of samples and fossils through the geological survey for 3 years. This paper makes a comprehensive research on the stratigraphy and paleogeographic characters of the formation by means of petrology, paleontology, structural geology, geochemistry and isotopic chronology. This research focuses on the Mesozoic basins yielding the Yixian Formation, including Yixian Basin, Jinlingsi-Yangshan Basin, Jianchang Basin and Lingyuan-Sanshijiazi Basin. Based on the characters of volcanic cycles, petrology and paleontology of the Yixian Formation, the author makes a systematic division and correlation of the Yixian Formation in the four basins. This paper discusses also the characters of paleostructure and lithofacies paleogeography. The study is significant to the correlation of fossil-bearing strata intercalated with volcanic beds in western Liaoning, and is helpful to the exploration and protection of relevant volcanic mineral resources. The discussion on the paleostructure and lithofacies paleogeography is useful to the study of geological history that is concerned about the origin and evolution of bird and angiosperm. Meanwhile, this will be beneficial for the study of paleogeography, volcanic activity and the evolution of organic-inorganic events.The new subdivisions and paleogeographic comparison of the Yixian Formation in western Liaoning are as follows:The Yixian Formation can be subdivided into four members. The first member of Yixian Formation is the member of sandstone-conglomerate and basic -intermediate-basic volcanic rocks, which are widely distributed in the study area
with the exception of sandstone-conglomerate, only occurred in the Yixian Basin and the Jinlingsi-Yangshan Basin. There are 4 fossil-bearing beds occurred in the first member of Yixian Formation. Two fossil beds with gastropods, bivalves, conchostracnas and ostracods were found in tuffite and tuffaceous sandstones of the Yixian Basin. Four fossil beds were found in the Jinlingsi-Yanshan Basin with the fossils of gastropods, bivalves, conchostraca, ostracods, dinosaurs and fossil wood occurred in the bottom sandstone and conglomerate, including Psittacosaurus occurred in upper part of tuffite, tuff and tuffaceous sandstones. The second member of the Yixian Formation is mainly composed of lacustrine volcanic-sedimentary rocks with broad distributions. There are lot of fossils belonging to the Jehol Biota occurred, including Sinosawopteryx, Confuciusornis and Archeafurctus liaoningensis. The author firstly discovered the pillow lava in the second member, which is interbeded into the fossil beds as "finger" shape. The isotopic data of the pillow lava provided important evidence for the age of the Yixian Formation and for the resolve of the fossil beds comparison problems. The third member of the Yixian Formation is mainly of intermediate-basic -intermediate-acidic volcanic rocks with wide distributions. The fourth member of Yixian Formation is of sedimentary rocks and acidic volcanic rocks that are mainly distributed in the Yixian Basin and Jinlingsi-Yanshan Basin. The upper part of the fourth member in the Yixian Basin, which is mainly of fish fossils, is also important fossil beds of Yixian Formation. It seems to have the characters of migration in the four members of the Yixian Formation from the west to the east influenced by volcanic activity center and the structural position indicated as the various strata thickness between different basins.Based on the study of petrology of volcanic rocks and the regularity of volcanism, the volcanic eruption cycle of the Yixian Formation is subdivided into four sub-cycles correspond respectively to the four lithologic members of the Yixian Formation. The sub-cycles can also further be subdivided into some smaller cycles. The research reveals the regularity for the migration of volcanic eruption in the sequence of basic - intermediate-basic - intermediate - acidic (alkaline) from early to late and from west to east. There is an obvious correlation between the sub-cycles. The Jianchang basin and Lingyuan-Sanshijiazi basin are situated in the transitional zone of the younger Mesozoic northern Hebei-west Liaoning volcanic rock province. In the Jianchang basin, along with the Jin-Yang and Yixian basins in the east, the sub-cycle migrates southeastwards. While in the Lingyuan-Sanshijiazi basin and the Pingquan basin in west, the migration is from southeast to northwest. Geochemical study shows that during the No.I sub-cycle, the magma in the Jianchang basin evolved from basic to intermediate; in No. II
sub-cycle, intermediate magma was dominated; while in No.IlI, it was mainly acidic-alkaline, with intermediate in the east. It is a calc-alkaline volcanic suite in general. In the Jin-Yang basin, the magmatic evolution in No.I sub-cycle was dominated by basic calc-alkaline rock series, the No. II sub-cycle was an intermediate-basic alkaline series, and the No. Ill was a basic calc-alkaline rock series. On the other hand, in the Yixian basin, magma evolved from basic to intermediate calc-alkaline/alkaline volcanic suite during the No.I sub-cycle; the No.II sub-cycle showed an intermediate-basic alkaline suite; in the No.III sub-cycle, it evolved from intermediate to alkaline, from calc-alkaline to alkaline suite; while the No.IV was in intermediate-acidic, calc-alkaline evolving to alkaline. Meanwhile, in the Lingyuan-Sanshijiazi basin, the magma evolution during the No.I sub-cycle presented intermediate and acidic; magmatism was not seen; and the No. Ill was acid. It is generally alkaline rock series. According to the structural environment differentiation by REE, the volcanic rocks were formed by the upward invasion of inner-plate basalt in the continental extension environment. It was derived from the HREE-enriched mantle, most likely from the same magma source. From No.I to No.IV sub-cycles, the hybridization became more and more intensive.By analysis on the paleostructure and lithofacies paleogeography of the Tuchengzi Formation before the Yixian Formation formed, it is concluded that, the regional principle stress field was NWW-SEE compression, which made the NE- or NNE-trending distributions of the Tuchengzi Formation in the studied area. Based on the distributions of the basin-controlling faults and main mobile faults during the developing stage of the Yixian Formation, as well as the regularity of volcanism in the Yixian Formation, the regional principle stress field in that time converted from NWW-SEE to S-N direction, which formed the NW-SE extension. The faulting becomes more intensive from west to east or southeast. From west to east, the types of the basins change from the depression-fault type (such as the Lingyuan-Sanshijiazi basin), though the semi-graben-fault-depression (such as the Jianchang and Jin-Yang basins) to the typical fault-depression type (the Yixian basin). Generally, the basin marginal faults on the east margin evidently control the distributions of the Yixian Formation.Synthetically applying the sedimentary environment, palaeobiological features, combined with the geochemical features of sedimentary rocks, the climate condition is regarded as warm temperate zone with seasonal arid or semi-arid climate condition during the Yixian stage. The climate is obviously different from Tuchengzi stage.The first member of the Yixian Formation mainly consists of fluvial facies
引文
1.丁秋红,郑少林,张武.东北地区中生代木化石异木属及其古生态.古生物学报,2000,39(2):237～249.
2.丁秋红、张立东、郭胜哲、陈树旺等.辽西北票地区义县组古气候环境标志及其意义.地质通报,2003,22(3):186～191.
3.丁秋红、张立东等.辽西北票地区义县组地层层序及化石层位.地质与资源,2001,(4):193～198.
4.丁秋红.辽宁西部义县组化石木材的研究(英文).古生物学报,2000,39(增刊):209-219.
5.刁乃昌.辽西地区中生代火山岩K—Ar同位素地质年龄的确定.辽宁地质学报,1983,(1):71～83
6.于青珊,李子舜,王思恩等.中国北部晚侏罗-早白垩世地层层序及地质对比.地质科学研究论文集,北京,中国经济出版社.1996,37～38.
7.马寅生,吴满路,曾庆利.燕山及邻区中新生代挤压与伸展作用.地质学报,2002,23(2):115～122.
8.中国科学院古脊椎动物与古人类研究所.古脊椎动物学报—辽西热河生物群综合研究专辑.1998,36(2):81～172.
9.中国科学院地球化学所编.高等地球化学.北京:科学出版社,2000,300～301.
10.中国科学院地球化学所编.高等地球化学.北京:科学出版社,1998,293-300.
11.王中刚,于学元,赵振华等编著.稀土元素地球化学.北京:科学出版社,1989,247～272.
12.王五力,郑少林,张立君等.中国东北环太平洋带构造地层学.北京:地质出版社,1995,187～259.
13.王五力,郑少林,张立君等.中国东北部环太平洋带构造地层学.北京:地质出版社,1995.
14.王五力,郑少林等.辽宁西部中生代叶肢介化石.辽宁西部中生代地层古生物(三).北京:地质出版社,1987,134～201.
15.王开发.根据孢粉组合推论轮坡拉盆地第三纪地层时代及古地理.地质科学,1975,(4):366～374.
16.王东方 辽西热河群的时代归属问题.中国地质科学院院报,1983,(7):57～63.
17.王东方,刁乃昌.辽西侏罗—白垩纪火山岩系统的同位素年龄测定—兼测侏罗系与白垩系的底界年龄.地质矿产部编,国际交流地质学论文集1.北京:地质出版社,1984,1～12.
18.王发祥,梁惠波.中国苏铁.广东:广东科技出版社,1996,225～228.
19.王松山,王元青,胡华光等.辽西四合屯脊椎动物生存时代:锆石U-Pb年龄证据,科学通报,2001,17(4):663～668.
20.王宪曾,任东,王宇飞.辽宁西部义县组被子植物花粉的首次发现.地质学报,2000,74(3):265～272.
21.王思恩,张志诚,姚培毅等.中国侏罗—白垩纪含煤地层与聚煤规律.北京:地质出版社,1994.
22.王思恩.热河动物群的起源、演化与机制.地质学报,1990,64(4):350～359.
23.王思恩.中国北部陆相侏罗系与英国海陆交互相侏罗系的对比研究—兼论中国北部 志留系的划分与对比.地质学报,1998,72(1):11～21.
24.王思恩.热河生物群的古生态与古环境—冀北、辽西叶肢介群落古生态与古环境重建.地质学报,1999,73(4):295～301.
25.王思恩等.中国的侏罗系.北京:地质出版社,1985,1～350.
26.王鸿祯,刘本陪.中国中元古代以来古地理的发展.地层学杂志,1981,5(2):72～89.
27.王鸿祯.中国古地理图集.北京:地质出版社,1987.
28.王鸿祯等.中国古地理图集.北京:地图出版社,1985.
29.王鸿祯等.中国晚元古代构造与古地理.地质科学,1980,(2):103～110.
30.王鸿祯等.中国震旦系的古地理.国际交流地质学术论文集(二).地层古生物,北京:地质出版社,1979,28～35.
31.瓦赫拉梅耶夫B.A.著,孙革,张志诚,郑少林译.侏罗—白垩纪全球植物群及气候.南京:南京大学出版社,1990,22～85.
32.贝克夫著,B.A.,付子祯,译.地植物学.北京:科学出版社,1957.
33.邓晋福,苏尚国,赵海玲等.华北地区燕山期岩石圈减薄的深部过程.地学前缘,2003,10(3):41～50.
34.邓晋福,莫宣学,赵海玲等.中国大陆根—柱构造.北京:地质出版社,1996.
35.冯增昭.华北早奥陶世岩相古地理新探.地质科学,1979,(4):302～313.
36.北京师范大学,上海师范大学.植物地理学.北京:人民教育出版社,1979.
37.卢立伍.辽宁凌源晚侏罗世鲟类化石的发现.古脊椎动物学报,1994,32(2):134～142.
38.卢崇海.义县组时代及解体.辽宁地质,2000,17(1):51～56.
39.叶美娜等.中国侏罗纪含植物化石地层的划分与对比,中国各纪地层对比表及说明书.北京:科学出版社,1982,241～253.
40.辽宁省区域地层表编写组.东北地区区域地层表,辽宁分册.北京:地质出版社,1978.
41.辽宁省地质矿产局.辽宁省区域地质志,地质矿产部地质专报(14).北京:地质出版社,1989,252～280.
42.任东,尹继才,黄伯衣.河北丰宁中生代晚期昆虫群落与生态地层的初步研究.地质科技情报,1999,18(1):39～44.
43.任东,卢立伍,姬书安,郭子光,尹继才,韩迎健.燕辽地区晚中生代动物群及其古生态和古地理意义.地球学报,1996,17(增刊):148～154.
44.任东,郭子光,卢立伍等.辽宁西部上侏罗统义县组研究新认识.地质论评,1997,43(5):449～459.
45.任东.辽宁北票晚侏罗世蛇蛉化石(昆虫纲)的新发现.地层古生物论文集,第二十五辑,1994,131～136.
46.任东.辽宁晚侏罗世里阿斯期箭蜓科一新属(昆虫纲,蜻蜓目).现代地质,1994,8(3):254～259.
47.任东.蚊蝎蛉科化石在我国的首次发现.地质学报,1993,67(4):376～381.
48.任东等.北京与邻区侏罗白垩纪动物群及其地层.北京:地震出版社,1995,1～222.
49.刘本培,张世红.侏罗-白垩纪地球圈层演化节律及相互关系.地学前缘(中国地质大学北京),1997,4(3-4):65～74.
50.刘本培,陈芬,王五力.从事件地层学角度探讨东亚陆相侏罗-白垩系界线.地球科学,1986,11(5):465～472.
51.刘宪亭、苏德造等.华北的狼鳍鱼化石\中国科学院古脊椎动物与古人类研究所甲种专刊.第六号.北京:科学出版社,1963.
52.刘鸿允.中国古地理图.北京:科学出版社,1955.
53.匡少平,徐仲等.运用地球化学方法研究中、新生代环境气候演替—兼论四川盆地侏罗纪气候变化.青岛化工学院学报(自然科学版),2002,3(1):4～9.
54.地质矿产部情报所.地质科技资料选编(七十一)国外沉积相及古地理资料汇编(二)古地理研究方法,1982.
55.孙安建.世界气候.北京:气象出版社,1986,13～30.
56.孙克勤.山东淄博地区晚石炭世和早二叠世植物群、古生态及沉积环境.长春:吉林大学出版社,1992,1～143.
57.孙革,Dilcher D L..迄今世界最早被子植物花序化石的首次发现.古生物学报,1997,36(2):135～142.
58.孙革,郑少林,D.迪尔切,王永栋,梅盛吴.辽西早期被子植物及其伴生植物群.上海:上海教育出版社,2001.
59.孙革,郑少林,梅盛吴.辽宁枝(新属)Lioningocladus gen.nov.在辽西义县组下部(晚侏罗世)的发现[J].古生物学报,2000,39(增刊):200～208.
60.孙革,郑少林.中国东北中生代地层划分之新见.地层学杂志,2000,24(1):60～64.
61.孙革,郭双兴,郑少林,朴太元,孙学坤.世界最早的被子植物化石群的首次发现.中国科学(B辑),1992,(5):543～548.
62.孙革,曹正尧,李浩敏,王鑫甫.白垩纪植物群.李星学主编.中国地质时期植物群(中文版).广州:广东科技出版社,1995,260～331.
63.朱为庆.辽西义县组古气候初探.植物学通报,2000,17(专辑):292～294.
64.江永、金帆等.长头狼鳍鱼(Lycoptera longicephalus)的重新认识.古脊椎动物学报,1994,32(1):41～59.
65.米家榕,孙春林,孙跃武,崔尚森,艾永亮.冀北辽西早、中侏罗世植物古生态学及聚煤环境.北京:地质出版社,1996,1～169.
66.邢德和,孙春林,孙跃武等.义县组研究的新认识.地球学报,2005,26(1):25～30.
67.邢德和,孙春林,张立东等.辽宁北票地区义县组地层划分与对比.吉林大学学报(地球科学版),2004,34(3):326～332.
68.余素华,郑洪汉.宁夏中卫长流水剖面沉积物中稀土元素及其环境意义.沉积学报,1999,17(1):150～155.
69.余静贤.冀北、辽西早白垩世孢粉组合序列.中国东部构造—岩浆演化及成矿规律(二),中国东部侏罗纪—白垩纪古生物及地层.北京:地质出版社.1989,21～51.
70.余静贤等.辽西热河群上亚群胞粉组合.中国地质科学院院报,1986,13:93～115.
71.吴舜卿.辽西热河植物群初步研究.Palaeoworld,热河生物群,1999,11:7～57.
72.吴舜卿.试论中国晚三叠世和早、中侏罗纪的植物群及其地理分区.北京:科学出版社,1983,121～131.
73.张文堂,陈丕基,沈炎彬.中国的叶肢介化石.北京:科学出版社,1976,1～325.
74.张长厚,王根厚,王国胜等.辽西地区燕山板内造山带东段中生代逆冲推覆构造.地质学报,2002,76(1):64～76.
75.张长厚.初论板内造山的带.地学前缘,1999.6(4):213-306
76.张立东,郭胜哲,张长捷,邢德和等.义县组底部层位发现恐龙化石.地质与资源, 2002,11(1):13～15.
77.张立东、郭胜哲、陈树旺,邢德利等.辽宁省四合屯—上园地区含珍稀化石沉积层的特点和形成环境.中国地质,2001,28(6):10～20.
78.张弥曼,周家健.浙江中生代晚期鱼化石\中国科学院古脊椎动物与古人类研究所甲种专刊,第十二号.北京:科学出版社,1977.
79.张弥曼,周家健,刘智成.东北白垩纪含鱼化石地层时代和沉积环境.古脊椎动物学报,1977,15(3):194～197.
80.张武、郑少林.辽宁西部地区早中生代植物化石.见于希汉.王五力等著:辽宁西部中生代地层古生物(3).北京:地质出版社,1987,239～368.
81.张俊峰.衍蜓类昆虫化石的再研究.Palaeoworld.1999,11:150～174.
82.张俊峰.山东莱阳中生代晚期昆虫群及其古生态特征.科学通报,1992,37(3):5～16.
83.张俊峰.稚虫的发现.科学通报,2000,45(2):192～199.
84.李亚平,董国义,范国清.辽西中生代含鸟层及上下层位的划分和时代.辽宁地质,1988,(3):175～184.
85.李亚平,董国义,范国清.辽西中生代含鸟层及上下层位的划分和时代.辽宁地质,1998,(3):175～184.
86.李伍平,李献华,路凤香等,辽西早白垩世义县组火山岩的地质特征及其构造背景.岩石学报.2002,18(2):193～204
87.李有生,孙灵权,董国义.辽西晚侏罗世魏家岭组的建立及其意义.辽宁地质,2000,17(4):280～283.
88.李佩贤,苏德英,李友桂等.狼鳍鱼(Lycoptera)岩层的时代归属.地质学报,1994,68(1):87～100.
89.李佩贤,程政武,庞其清.辽西北票孔子鸟Confuciusornis的层位及时代.地质学报,2001,(1):1～13
90.杨庚、柴育成,吴正文.燕山造山带东段-辽西地区薄皮逆冲推覆构造.地质学报,75(3):24～37.
91.汪筱林,王元青,王原等:辽西四合屯及周遍地区义县组下部地层层序与脊椎动物化石层位.古脊椎动物学报,1998,36(2):81～101.
92.汪筱林,王元青,徐星,王原,张江永,张福成,金帆.辽西四合屯脊椎动物集群死亡事件:火山爆发的灾变记录.地质论评,1999,45卷(增刊):458～467.
93.汪筱林、王元青、金帆、徐星、王原.辽西热河生物群脊椎动物化石组合序列与地层层序.第七届中国古脊椎动物学学术年会论文集.北京:海洋出版社.1999,1～12.
94.汪筱林等.义县组同位素年代新证据及土城子组Ar~(40)/Ar~(39)年龄测定[J].科学通报,2001,46(23):2009～2012.
95.汪筱林等.辽西北票四合屯脊椎动物化石组合及其地质背景.热河生物群.安徽:中国科学技术出版社,1999(11):310～327.
96.沈炎彬,Frederick R.Schram Rod S.Taylor.热河生物群四节辽宁洞虾及其古生态.Palaeoworld,热河生物群,1999.11:175～187.
97.沈梅,金帆等.华夏鱼科(Huashiidae)的系统关系及分类学意义.古脊椎动物学报,1991,29(4):245～263.
98.陈义贤.辽西及邻区中生代火山岩—年代学、地球化学和构造背景.北京:地质出版社,1997,1～279.
99.陈丕基,文世宣,周志炎,等.辽宁西部晚中生代陆相地层的研究.中国科学院南京地质古生物研究所所刊,1980,(1):22～55.
100.陈丕基,吴舜卿.热河生物群研究的现状与展望.北京大学国际地质科学学术研讨会论文集.北京:地震出版社,1998,355～395.
101.陈丕基,黎文本,陈金华,叶春辉,王振等.中国侏罗、白垩纪化石群序列.中国科学(B),1982,(6):558～565;(7):651～664.
102.陈丕基.辽西义县组的叶肢介化石.Palaeoworld,热河生物群.1999,11:114～130.
103.陈丕基.热河生物群的分布与扩展.陈丕基,金帆主编:热河生物群.Palaeoworld 11(专辑).安徽:中国科学技术大学出版社,1999,1～6.
104.陈丕基.热河动物群的分布与迁移.古生物学报,1988,20(6):659～683.
105.陈好寿,同位素地球化学研究.杭州:浙江大学出版社.1994.
106.陈金华.热河生物群的双壳类组合研究.Palaeoworld,热河生物群.1999,11:92～11.
107.周志炎,李佩娟.从古植物学观点讨论中国中生代陆相地层的划分、对比利时代[C].国际交流地质学术论文集(4):地层古生物.北京:地质出版社,1980,82～91.
108.周志炎、李佩娟.从古植物学观点讨论中国中生代陆相地层的划分、对比利时代.地质部书刊编辑室编辑,国际交流地质学术论文集—为二十六届国际地质大会撰写,4.地层古生物.北京:地质出版社,1980,82～91.
109.周忠和.潘氏北票鲟的新材料及鲟类系统关系.古脊椎动物学报,1992,30(2):85～101.
110.周忠和.鸟类起源研究的进展与现状.古脊椎动物学报,2000,38(1):72～78.
111.周明镇,程政武,王元青.记辽西-侏罗纪哺乳动物下颌骨.古脊椎动物学报,1991,29(3):165～175.
112.国家地质总局宜昌地质研究所主编.中南地区白垩—第三纪岩相古地理.北京:地质出版社,1979.
113.季强等.中国辽西中生代热河生物群.北京:地质出版社,2004.
114.季强,姬书安,任东等.论辽西北票四合屯-尖山沟一带含原始鸟类地层的层序及时代.地层古生物论文集.北京:地质出版社.1998(27):74～80.
115.季强,姬书安.原始祖鸟(Protarchaeopteryx gen. nov.)—中国的始祖鸟类化石.中国地质,1997(3):38～41.
116.林启彬.辽西侏罗系的昆虫化石.古生物学报,1976,15(1):97～117.
117.武汉地质学院,青海地质研究所.青海省三叠纪地层及古地理特征.国际交流地质学术论文集(二).1979,124～142.
118.武汉地质学院地球化学教研室编.地球化学.北京:地质出版社,1979,40～41.
119.武春生.中国福利祝蛾属研究及新种记述(鳞翅目:祝蛾科),1997,37(4):25～28.
120.罗林逊(Hugh R. Rollison)著.1992.(杨学明,杨晓勇,陈双喜译).岩石地球化学.安徽:中国科学技术大学出版社.2000,106～110.
121.罗修泉,李佩贤.侏罗系-白垩系界线年代研究.地球学报,1997,18(3):242～247.
122.罗清华,陈丕基,邹东羽等.中华龙鸟与孔子鸟类的时代—辽宁义县组火山凝灰岩激光Ar~(40)/Ar~(39)年龄测定.地球化学,1999,28(4):405～409
123.罗清华、陈丕基、邹东羽等.中华鸟龙与孔子鸟类的时代—辽西义县组火山凝灰岩激光40Ar/39Ar年龄测定.地球化学,1999,28(4):406～409.
124.郑少林,郑月娟,邢德和.辽西晚侏罗世义县期植物群性质、时代及气候.地层学 杂志,2003,27 (3):233～241.
125.郑亚东,Davis G A,王琮等.燕山带中生代主要构造事件与板块构造背景问题.地质学报,2000,74(4):289～302.
126.金帆,张江永等.隆德鱼的新材料及其系统关系的初步分析.古脊椎动物学报.1993,31 (4):241～256.
127.金帆.辽宁西部晚中生代地层研究之进展及存在问题.古脊椎动物学报,1996,34(2):102～122.
128.侯连海,陈丕基.最小的早期鸟类—娇小辽西鸟.科学通报,1999,44 (3):311～315.
129.侯连海,周忠和,顾玉才,孙玉铁.辽宁中生代鸟类综述.古脊椎动物学报,1995,33 (4):261～271.
130.侯连海,周忠和,顾玉才,张和.侏罗纪鸟类化石在中国的首次发现.科学通报,1995,40 (8):726～729.
131.南京大学地理系地貌教研室.中国第四纪冰川及冰期问题.北京:科学出版社,1974.
132.南京农学院,华南农学院主编.植物学.上海:上海科学技术出版社,1978.
133.姚兆奇.大羽羊齿植物的生态和埋藏学.古生物学报,1983,17 (1):171～191.
134.室井渡.满州地质见学旅行.阜新、凌源方面.1940,28～46.
135.段淑英.最古早老的被子植物-具三心皮的生殖器官化石的发现.中国科学(D辑),1997,42 (6):519～523.
136.洪友崇.中国北方昆虫群的建立与演化序列.地质学报,1998,72 (1):1～10.
137.洪友崇.东亚古陆中生代晚期热河生物群的起源、发展、鼎盛与衰亡.现代地质,1993,7 (4):373～383.
138.洪友崇.北方中侏罗世昆虫化石.北京:地质出版社,1983.
139.祝廷成,钟章成,李建东等合编.植物生态学.北京:高等教育出版社,1988.
140.胡耀明,王元清等.张和兽(Zhangheotyerium)齿列和前肢形态.古脊椎动物学报,1998,36 (2):102～125.
141.姬书安,季强.记辽宁一新翼龙化石(缘嘴龙亚日).江苏地质,1998,22 (4):199～206.
142.姬书安,季强.辽宁西部翼龙类化石的首次发现.地质学报,1997,71 (1):1～6.
143.姬书安.中国的翼龙化石综述.第七届中国古脊椎动物学学术年会论文集.1999,81～88.
144.徐星,汪筱林.辽西义县组鹦鹉嘴龙(鸟臀类,角龙亚日)新材料及其地层学意义.古脊椎动物学报,1998,36 (2):147～158.
145.殷鸿福.三叠纪古地理及大陆漂移.地质科学,1980,(3):265～278.
146.殷鸿福等.中国古生物地理学.北京:中国地质大学出版社,1988.
147.郭双兴,吴向午.辽宁西部晚侏罗世晚期义县组的似麻黄植物.古生物学报,2000,39 (1):81～91.
148.郭洪中,张招崇.辽宁西部中生代火山岩的基本特征.岩石矿物学杂志,1992,3:193～204.
149.郭胜哲、张立东,邢德利等.辽宁西部义县组研究新进展.中国地质,2001,(8):1～8.
150.郭胜哲、张立东,邢德和等.辽宁西部义县组湖相枕状熔岩的发现及其意义.地球学报,2002,23 (6):491～494.
151.顾知微.中国的侏罗系和白垩系.见:全国地层会议学术论文汇编,北京:科学出 版社,1962,1～84.
152.顾知微.热河动物化石群地质时代的研究.王鸿祯主编,中国地质学科发展的回顾—孙云铸教授百年诞辰纪念文集.武汉:中国地质大学出版社.1995,93～99.
153.高克勤,唐治路,汪筱林.辽宁晚侏罗世-早白垩世一长颈双弓类爬行动物.古脊椎动物学报,1999,37 (1):1～8.
154.曹正尧,吴舜卿,张平安,李杰儒.辽宁义县组单子叶植物化石的发现.科学通报,1997,42 (16):1764～1776.
155.曹正尧.辽西早白垩世义县组Rufforfia和Nageiopsis的发现及其地层意义.古生物学报,2001,40 (2):214～218.
156.曹军骥,张小曳,王丹等.晚新生代风尘沉积的稀土元素地球化学特征及其古气候意义.海洋地质与第四纪地质,2001,21 (1):97～101.
157.曹美珍.辽宁西部四合屯地区义县组西部介形类.Palaeoworld,热河生物群,1999,11:131～149.
158.梁鸿德、许坤.冀北-辽西地区侏罗-白垩系界线.第三届全国地层会议论文集,北京:地质出版社,2000,237～242.
159.黄本宏.东北北部石炭二叠纪陆相地层及古地理概况.地质论评,1982,28(5):396～401.
160.蒲荣干,吴洪章.辽宁西部中生界孢粉组合及其地层意义.辽宁西部中生代地层古生物(2)[M],北京:地质出版社,1985,121～212.
161.臧尧龄,刘志英,姜应星等.中国东北部火山岩带多重岩系迭加性及其成因和演化.李兆乃,王碧香主编:火山岩火山作用及有关矿产(中国地质学会论文集第1集).北京:地质出版社,1993,85～91.
162.潘华璋,朱祥根.辽宁北票四合屯地区义县组下部的腹足类化石.Palaeoworld,热河生物群.1999,11:80～91.
163.黎文本,刘兆生.辽西北票义县组底部的孢粉组合及其时代.Palaeoworld.1999,11:68～7.
164.黎文本、刘兆生.辽西北票义县组底部的孢粉组合及其时代.陈丕基,金帆主编:热河生物群,Palaeoworld 11(专辑).安徽:中国科学技术大学出版社,1999,11:68～79.
165.黎文本.中国早白垩世孢粉植物群及其地理分区.古生物学基础理论丛书编委会编辑,中国古生物地理区系.北京:科学出版社,1983,142～151.
166.魏菊英.地球化学.北京:科学技术出版社,25～58.
167. Axelrod D. I. , Bailey H. P. Palaeotemperature analysis of Tertiary flora[A]. Palaeogeog. Palaeoclimatol. Palaeoecol. , 1969, 6 (3) : 193～195.
168. Bailey I. W. , Sinnot E W. The climatic distribution of certain types of angiosperm leaves [J]. Am J Bot. 1916, (3) : 24～39.
169. Swisher C. C. Ⅲ. Yuan-qing Wang, Xiao-lin Wang. Cretaceous age for the ferthered dinosaurs of Liaoning, China. NATURE, 1999, 401 (1) : 58～51.
170. Dimichele, W. A. , Ecological Patterns in Time and Space. Paleobiology, 1994, 20 (2) : 89～92.
171. Dolph G E, Dilcher D L. . Foliar physiognomy as an aid in determining paleoclimate [J]. Palaeontographica B, 1979, 170: 151～172.
172. Doludenko M P, Orlovskaya E R. Jurassic flora of the Karatau Range, southern Kazakhstan[J]. Palaeontology, 1976, 19 (4) : 627～640.
173. Doludenko M P, Orlovskaya E R. Jurassic flora of the Karatau[M]. M. : Nauka, 1976, 1～260.
174. Dong Ren, Ziguang Guo. Three New Gerera and Three New Spicies of Dragonfles from the late Jurassic of Northeast China (Anisoptera: Aeshnidae, Gomphidae, corduliidae). Entomologia Sinica, 1996, 3 (2) : 95～105.
175. Dong Ren, Ziguang Guo. A New genus and Two new species of short-horned files of upper Jurassic from northeast China. Entomologia Sinica, 1995, 2 (4) : 300-307.
176. Ge Sun, David L. Dilcher, Shaoling Zheng, Zhekun Zhou. In Search of the First Flower: A Jurassic Angiosperm, Archaefructus, from Northeast China. Science, 1998, 282 (5394) : 1601～1772.
177. Grabau A W. Stratigraphy of China Ⅱ (Mesozoic)[M]. Peiking: Geol Surv China, 1928, 1～774.
178. Grabau, A W. . Cretaceous mollusca from North China. Bull. Surv. China. 1923, No. 5, pt. 2. : 179～183.
179. Huo Lian-hai, Zhou Zhonghe et al. A beaked bird from the Jurassic of China. Nature, 1995, 377 (6550) : 616～618.
180. Jane E. Francis, Imogen Poole. Cretaceous and early Tertiary climates of Antarctica: evidence from fossil wood[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 182 (1～2) : 47～64.
181. Krassilov V A. Paleoecology of terrestrial plants[M]. Vladivostok: Far-East Cent Acad Sci, USSR, 1972, 1～208.
182. Krassilov V A. Angiosperm origins. Morphological and ecological aspects[M]. Sofia: Pensoft, 1997, 1～270.
183. L. D. Martin, Z. Zhou, L. Hou, A. Feduccia. Confuciusornis sanctus Compared to Archaeopteryx lithographica. Naturwissenschaften. 1998, 85: 286～289.
184. Lianhai Hou, Larry D. Martin, Zhonghe Zhou, Alan Feduccia, Fucheng Zhang. A diapsid skull in a new species of the primitive bird Confuciusornis. Nature, 1999, 399 (17) : 679～682.
185. Lianhai Hou, Larry D. Martin, Zhonghe Zhou, and Alan Feduccia. Early Adaptive Radiation of Birds: Evidence from Fossil from Northeastern china. Sciense, 1996, 274 (15) : 1164～1167.
186. Lian-hai Hou, Zhonghe Zhou, Larry D. Martin, Alan Feduccia. A beaked bird from the Jurassic of China. Nature, 1995, 377 (19) : 616～618.
187. Miki S. Mesozoic flora of Lycoptera beds in South Manchuria. Bull Mukogawa Woman's Univ. 1964, 12: S13～S22. (in Japanese with English abstract)
188. Norris G. . Misopores from the Purbeck beds and Marine upper Jurassic of Southern England. Palaeontology. 1969, (12) : 574～620.
189. Pei-ji Cheng, zhi-ming Dong, Shuo-nan Zhen. An exceptionally well-preserved theropod dinosaur from the Yixian Formation of China. Nature, 1998, 391 (8) : 147～152.
190. Qi-gao Sun, Margaret E. Collinson, Cheng-Sen Li, Yu-fei Wang, David J. Beerling. Quantitative reconstruction of palacoclimate from the Middle
2.丁秋红、张立东、郭胜哲、陈树旺等.辽西北票地区义县组古气候环境标志及其意义.地质通报,2003,22(3):186～191.
3.丁秋红、张立东等.辽西北票地区义县组地层层序及化石层位.地质与资源,2001,(4):193～198.
4.丁秋红.辽宁西部义县组化石木材的研究(英文).古生物学报,2000,39(增刊):209-219.
5.刁乃昌.辽西地区中生代火山岩K—Ar同位素地质年龄的确定.辽宁地质学报,1983,(1):71～83
6.于青珊,李子舜,王思恩等.中国北部晚侏罗-早白垩世地层层序及地质对比.地质科学研究论文集,北京,中国经济出版社.1996,37～38.
7.马寅生,吴满路,曾庆利.燕山及邻区中新生代挤压与伸展作用.地质学报,2002,23(2):115～122.
8.中国科学院古脊椎动物与古人类研究所.古脊椎动物学报—辽西热河生物群综合研究专辑.1998,36(2):81～172.
9.中国科学院地球化学所编.高等地球化学.北京:科学出版社,2000,300～301.
10.中国科学院地球化学所编.高等地球化学.北京:科学出版社,1998,293-300.
11.王中刚,于学元,赵振华等编著.稀土元素地球化学.北京:科学出版社,1989,247～272.
12.王五力,郑少林,张立君等.中国东北环太平洋带构造地层学.北京:地质出版社,1995,187～259.
13.王五力,郑少林,张立君等.中国东北部环太平洋带构造地层学.北京:地质出版社,1995.
14.王五力,郑少林等.辽宁西部中生代叶肢介化石.辽宁西部中生代地层古生物(三).北京:地质出版社,1987,134～201.
15.王开发.根据孢粉组合推论轮坡拉盆地第三纪地层时代及古地理.地质科学,1975,(4):366～374.
16.王东方 辽西热河群的时代归属问题.中国地质科学院院报,1983,(7):57～63.
17.王东方,刁乃昌.辽西侏罗—白垩纪火山岩系统的同位素年龄测定—兼测侏罗系与白垩系的底界年龄.地质矿产部编,国际交流地质学论文集1.北京:地质出版社,1984,1～12.
18.王发祥,梁惠波.中国苏铁.广东:广东科技出版社,1996,225～228.
19.王松山,王元青,胡华光等.辽西四合屯脊椎动物生存时代:锆石U-Pb年龄证据,科学通报,2001,17(4):663～668.
20.王宪曾,任东,王宇飞.辽宁西部义县组被子植物花粉的首次发现.地质学报,2000,74(3):265～272.
21.王思恩,张志诚,姚培毅等.中国侏罗—白垩纪含煤地层与聚煤规律.北京:地质出版社,1994.
22.王思恩.热河动物群的起源、演化与机制.地质学报,1990,64(4):350～359.
23.王思恩.中国北部陆相侏罗系与英国海陆交互相侏罗系的对比研究—兼论中国北部 志留系的划分与对比.地质学报,1998,72(1):11～21.
24.王思恩.热河生物群的古生态与古环境—冀北、辽西叶肢介群落古生态与古环境重建.地质学报,1999,73(4):295～301.
25.王思恩等.中国的侏罗系.北京:地质出版社,1985,1～350.
26.王鸿祯,刘本陪.中国中元古代以来古地理的发展.地层学杂志,1981,5(2):72～89.
27.王鸿祯.中国古地理图集.北京:地质出版社,1987.
28.王鸿祯等.中国古地理图集.北京:地图出版社,1985.
29.王鸿祯等.中国晚元古代构造与古地理.地质科学,1980,(2):103～110.
30.王鸿祯等.中国震旦系的古地理.国际交流地质学术论文集(二).地层古生物,北京:地质出版社,1979,28～35.
31.瓦赫拉梅耶夫B.A.著,孙革,张志诚,郑少林译.侏罗—白垩纪全球植物群及气候.南京:南京大学出版社,1990,22～85.
32.贝克夫著,B.A.,付子祯,译.地植物学.北京:科学出版社,1957.
33.邓晋福,苏尚国,赵海玲等.华北地区燕山期岩石圈减薄的深部过程.地学前缘,2003,10(3):41～50.
34.邓晋福,莫宣学,赵海玲等.中国大陆根—柱构造.北京:地质出版社,1996.
35.冯增昭.华北早奥陶世岩相古地理新探.地质科学,1979,(4):302～313.
36.北京师范大学,上海师范大学.植物地理学.北京:人民教育出版社,1979.
37.卢立伍.辽宁凌源晚侏罗世鲟类化石的发现.古脊椎动物学报,1994,32(2):134～142.
38.卢崇海.义县组时代及解体.辽宁地质,2000,17(1):51～56.
39.叶美娜等.中国侏罗纪含植物化石地层的划分与对比,中国各纪地层对比表及说明书.北京:科学出版社,1982,241～253.
40.辽宁省区域地层表编写组.东北地区区域地层表,辽宁分册.北京:地质出版社,1978.
41.辽宁省地质矿产局.辽宁省区域地质志,地质矿产部地质专报(14).北京:地质出版社,1989,252～280.
42.任东,尹继才,黄伯衣.河北丰宁中生代晚期昆虫群落与生态地层的初步研究.地质科技情报,1999,18(1):39～44.
43.任东,卢立伍,姬书安,郭子光,尹继才,韩迎健.燕辽地区晚中生代动物群及其古生态和古地理意义.地球学报,1996,17(增刊):148～154.
44.任东,郭子光,卢立伍等.辽宁西部上侏罗统义县组研究新认识.地质论评,1997,43(5):449～459.
45.任东.辽宁北票晚侏罗世蛇蛉化石(昆虫纲)的新发现.地层古生物论文集,第二十五辑,1994,131～136.
46.任东.辽宁晚侏罗世里阿斯期箭蜓科一新属(昆虫纲,蜻蜓目).现代地质,1994,8(3):254～259.
47.任东.蚊蝎蛉科化石在我国的首次发现.地质学报,1993,67(4):376～381.
48.任东等.北京与邻区侏罗白垩纪动物群及其地层.北京:地震出版社,1995,1～222.
49.刘本培,张世红.侏罗-白垩纪地球圈层演化节律及相互关系.地学前缘(中国地质大学北京),1997,4(3-4):65～74.
50.刘本培,陈芬,王五力.从事件地层学角度探讨东亚陆相侏罗-白垩系界线.地球科学,1986,11(5):465～472.
51.刘宪亭、苏德造等.华北的狼鳍鱼化石\中国科学院古脊椎动物与古人类研究所甲种专刊.第六号.北京:科学出版社,1963.
52.刘鸿允.中国古地理图.北京:科学出版社,1955.
53.匡少平,徐仲等.运用地球化学方法研究中、新生代环境气候演替—兼论四川盆地侏罗纪气候变化.青岛化工学院学报(自然科学版),2002,3(1):4～9.
54.地质矿产部情报所.地质科技资料选编(七十一)国外沉积相及古地理资料汇编(二)古地理研究方法,1982.
55.孙安建.世界气候.北京:气象出版社,1986,13～30.
56.孙克勤.山东淄博地区晚石炭世和早二叠世植物群、古生态及沉积环境.长春:吉林大学出版社,1992,1～143.
57.孙革,Dilcher D L..迄今世界最早被子植物花序化石的首次发现.古生物学报,1997,36(2):135～142.
58.孙革,郑少林,D.迪尔切,王永栋,梅盛吴.辽西早期被子植物及其伴生植物群.上海:上海教育出版社,2001.
59.孙革,郑少林,梅盛吴.辽宁枝(新属)Lioningocladus gen.nov.在辽西义县组下部(晚侏罗世)的发现[J].古生物学报,2000,39(增刊):200～208.
60.孙革,郑少林.中国东北中生代地层划分之新见.地层学杂志,2000,24(1):60～64.
61.孙革,郭双兴,郑少林,朴太元,孙学坤.世界最早的被子植物化石群的首次发现.中国科学(B辑),1992,(5):543～548.
62.孙革,曹正尧,李浩敏,王鑫甫.白垩纪植物群.李星学主编.中国地质时期植物群(中文版).广州:广东科技出版社,1995,260～331.
63.朱为庆.辽西义县组古气候初探.植物学通报,2000,17(专辑):292～294.
64.江永、金帆等.长头狼鳍鱼(Lycoptera longicephalus)的重新认识.古脊椎动物学报,1994,32(1):41～59.
65.米家榕,孙春林,孙跃武,崔尚森,艾永亮.冀北辽西早、中侏罗世植物古生态学及聚煤环境.北京:地质出版社,1996,1～169.
66.邢德和,孙春林,孙跃武等.义县组研究的新认识.地球学报,2005,26(1):25～30.
67.邢德和,孙春林,张立东等.辽宁北票地区义县组地层划分与对比.吉林大学学报(地球科学版),2004,34(3):326～332.
68.余素华,郑洪汉.宁夏中卫长流水剖面沉积物中稀土元素及其环境意义.沉积学报,1999,17(1):150～155.
69.余静贤.冀北、辽西早白垩世孢粉组合序列.中国东部构造—岩浆演化及成矿规律(二),中国东部侏罗纪—白垩纪古生物及地层.北京:地质出版社.1989,21～51.
70.余静贤等.辽西热河群上亚群胞粉组合.中国地质科学院院报,1986,13:93～115.
71.吴舜卿.辽西热河植物群初步研究.Palaeoworld,热河生物群,1999,11:7～57.
72.吴舜卿.试论中国晚三叠世和早、中侏罗纪的植物群及其地理分区.北京:科学出版社,1983,121～131.
73.张文堂,陈丕基,沈炎彬.中国的叶肢介化石.北京:科学出版社,1976,1～325.
74.张长厚,王根厚,王国胜等.辽西地区燕山板内造山带东段中生代逆冲推覆构造.地质学报,2002,76(1):64～76.
75.张长厚.初论板内造山的带.地学前缘,1999.6(4):213-306
76.张立东,郭胜哲,张长捷,邢德和等.义县组底部层位发现恐龙化石.地质与资源, 2002,11(1):13～15.
77.张立东、郭胜哲、陈树旺,邢德利等.辽宁省四合屯—上园地区含珍稀化石沉积层的特点和形成环境.中国地质,2001,28(6):10～20.
78.张弥曼,周家健.浙江中生代晚期鱼化石\中国科学院古脊椎动物与古人类研究所甲种专刊,第十二号.北京:科学出版社,1977.
79.张弥曼,周家健,刘智成.东北白垩纪含鱼化石地层时代和沉积环境.古脊椎动物学报,1977,15(3):194～197.
80.张武、郑少林.辽宁西部地区早中生代植物化石.见于希汉.王五力等著:辽宁西部中生代地层古生物(3).北京:地质出版社,1987,239～368.
81.张俊峰.衍蜓类昆虫化石的再研究.Palaeoworld.1999,11:150～174.
82.张俊峰.山东莱阳中生代晚期昆虫群及其古生态特征.科学通报,1992,37(3):5～16.
83.张俊峰.稚虫的发现.科学通报,2000,45(2):192～199.
84.李亚平,董国义,范国清.辽西中生代含鸟层及上下层位的划分和时代.辽宁地质,1988,(3):175～184.
85.李亚平,董国义,范国清.辽西中生代含鸟层及上下层位的划分和时代.辽宁地质,1998,(3):175～184.
86.李伍平,李献华,路凤香等,辽西早白垩世义县组火山岩的地质特征及其构造背景.岩石学报.2002,18(2):193～204
87.李有生,孙灵权,董国义.辽西晚侏罗世魏家岭组的建立及其意义.辽宁地质,2000,17(4):280～283.
88.李佩贤,苏德英,李友桂等.狼鳍鱼(Lycoptera)岩层的时代归属.地质学报,1994,68(1):87～100.
89.李佩贤,程政武,庞其清.辽西北票孔子鸟Confuciusornis的层位及时代.地质学报,2001,(1):1～13
90.杨庚、柴育成,吴正文.燕山造山带东段-辽西地区薄皮逆冲推覆构造.地质学报,75(3):24～37.
91.汪筱林,王元青,王原等:辽西四合屯及周遍地区义县组下部地层层序与脊椎动物化石层位.古脊椎动物学报,1998,36(2):81～101.
92.汪筱林,王元青,徐星,王原,张江永,张福成,金帆.辽西四合屯脊椎动物集群死亡事件:火山爆发的灾变记录.地质论评,1999,45卷(增刊):458～467.
93.汪筱林、王元青、金帆、徐星、王原.辽西热河生物群脊椎动物化石组合序列与地层层序.第七届中国古脊椎动物学学术年会论文集.北京:海洋出版社.1999,1～12.
94.汪筱林等.义县组同位素年代新证据及土城子组Ar~(40)/Ar~(39)年龄测定[J].科学通报,2001,46(23):2009～2012.
95.汪筱林等.辽西北票四合屯脊椎动物化石组合及其地质背景.热河生物群.安徽:中国科学技术出版社,1999(11):310～327.
96.沈炎彬,Frederick R.Schram Rod S.Taylor.热河生物群四节辽宁洞虾及其古生态.Palaeoworld,热河生物群,1999.11:175～187.
97.沈梅,金帆等.华夏鱼科(Huashiidae)的系统关系及分类学意义.古脊椎动物学报,1991,29(4):245～263.
98.陈义贤.辽西及邻区中生代火山岩—年代学、地球化学和构造背景.北京:地质出版社,1997,1～279.
99.陈丕基,文世宣,周志炎,等.辽宁西部晚中生代陆相地层的研究.中国科学院南京地质古生物研究所所刊,1980,(1):22～55.
100.陈丕基,吴舜卿.热河生物群研究的现状与展望.北京大学国际地质科学学术研讨会论文集.北京:地震出版社,1998,355～395.
101.陈丕基,黎文本,陈金华,叶春辉,王振等.中国侏罗、白垩纪化石群序列.中国科学(B),1982,(6):558～565;(7):651～664.
102.陈丕基.辽西义县组的叶肢介化石.Palaeoworld,热河生物群.1999,11:114～130.
103.陈丕基.热河生物群的分布与扩展.陈丕基,金帆主编:热河生物群.Palaeoworld 11(专辑).安徽:中国科学技术大学出版社,1999,1～6.
104.陈丕基.热河动物群的分布与迁移.古生物学报,1988,20(6):659～683.
105.陈好寿,同位素地球化学研究.杭州:浙江大学出版社.1994.
106.陈金华.热河生物群的双壳类组合研究.Palaeoworld,热河生物群.1999,11:92～11.
107.周志炎,李佩娟.从古植物学观点讨论中国中生代陆相地层的划分、对比利时代[C].国际交流地质学术论文集(4):地层古生物.北京:地质出版社,1980,82～91.
108.周志炎、李佩娟.从古植物学观点讨论中国中生代陆相地层的划分、对比利时代.地质部书刊编辑室编辑,国际交流地质学术论文集—为二十六届国际地质大会撰写,4.地层古生物.北京:地质出版社,1980,82～91.
109.周忠和.潘氏北票鲟的新材料及鲟类系统关系.古脊椎动物学报,1992,30(2):85～101.
110.周忠和.鸟类起源研究的进展与现状.古脊椎动物学报,2000,38(1):72～78.
111.周明镇,程政武,王元青.记辽西-侏罗纪哺乳动物下颌骨.古脊椎动物学报,1991,29(3):165～175.
112.国家地质总局宜昌地质研究所主编.中南地区白垩—第三纪岩相古地理.北京:地质出版社,1979.
113.季强等.中国辽西中生代热河生物群.北京:地质出版社,2004.
114.季强,姬书安,任东等.论辽西北票四合屯-尖山沟一带含原始鸟类地层的层序及时代.地层古生物论文集.北京:地质出版社.1998(27):74～80.
115.季强,姬书安.原始祖鸟(Protarchaeopteryx gen. nov.)—中国的始祖鸟类化石.中国地质,1997(3):38～41.
116.林启彬.辽西侏罗系的昆虫化石.古生物学报,1976,15(1):97～117.
117.武汉地质学院,青海地质研究所.青海省三叠纪地层及古地理特征.国际交流地质学术论文集(二).1979,124～142.
118.武汉地质学院地球化学教研室编.地球化学.北京:地质出版社,1979,40～41.
119.武春生.中国福利祝蛾属研究及新种记述(鳞翅目:祝蛾科),1997,37(4):25～28.
120.罗林逊(Hugh R. Rollison)著.1992.(杨学明,杨晓勇,陈双喜译).岩石地球化学.安徽:中国科学技术大学出版社.2000,106～110.
121.罗修泉,李佩贤.侏罗系-白垩系界线年代研究.地球学报,1997,18(3):242～247.
122.罗清华,陈丕基,邹东羽等.中华龙鸟与孔子鸟类的时代—辽宁义县组火山凝灰岩激光Ar~(40)/Ar~(39)年龄测定.地球化学,1999,28(4):405～409
123.罗清华、陈丕基、邹东羽等.中华鸟龙与孔子鸟类的时代—辽西义县组火山凝灰岩激光40Ar/39Ar年龄测定.地球化学,1999,28(4):406～409.
124.郑少林,郑月娟,邢德和.辽西晚侏罗世义县期植物群性质、时代及气候.地层学 杂志,2003,27 (3):233～241.
125.郑亚东,Davis G A,王琮等.燕山带中生代主要构造事件与板块构造背景问题.地质学报,2000,74(4):289～302.
126.金帆,张江永等.隆德鱼的新材料及其系统关系的初步分析.古脊椎动物学报.1993,31 (4):241～256.
127.金帆.辽宁西部晚中生代地层研究之进展及存在问题.古脊椎动物学报,1996,34(2):102～122.
128.侯连海,陈丕基.最小的早期鸟类—娇小辽西鸟.科学通报,1999,44 (3):311～315.
129.侯连海,周忠和,顾玉才,孙玉铁.辽宁中生代鸟类综述.古脊椎动物学报,1995,33 (4):261～271.
130.侯连海,周忠和,顾玉才,张和.侏罗纪鸟类化石在中国的首次发现.科学通报,1995,40 (8):726～729.
131.南京大学地理系地貌教研室.中国第四纪冰川及冰期问题.北京:科学出版社,1974.
132.南京农学院,华南农学院主编.植物学.上海:上海科学技术出版社,1978.
133.姚兆奇.大羽羊齿植物的生态和埋藏学.古生物学报,1983,17 (1):171～191.
134.室井渡.满州地质见学旅行.阜新、凌源方面.1940,28～46.
135.段淑英.最古早老的被子植物-具三心皮的生殖器官化石的发现.中国科学(D辑),1997,42 (6):519～523.
136.洪友崇.中国北方昆虫群的建立与演化序列.地质学报,1998,72 (1):1～10.
137.洪友崇.东亚古陆中生代晚期热河生物群的起源、发展、鼎盛与衰亡.现代地质,1993,7 (4):373～383.
138.洪友崇.北方中侏罗世昆虫化石.北京:地质出版社,1983.
139.祝廷成,钟章成,李建东等合编.植物生态学.北京:高等教育出版社,1988.
140.胡耀明,王元清等.张和兽(Zhangheotyerium)齿列和前肢形态.古脊椎动物学报,1998,36 (2):102～125.
141.姬书安,季强.记辽宁一新翼龙化石(缘嘴龙亚日).江苏地质,1998,22 (4):199～206.
142.姬书安,季强.辽宁西部翼龙类化石的首次发现.地质学报,1997,71 (1):1～6.
143.姬书安.中国的翼龙化石综述.第七届中国古脊椎动物学学术年会论文集.1999,81～88.
144.徐星,汪筱林.辽西义县组鹦鹉嘴龙(鸟臀类,角龙亚日)新材料及其地层学意义.古脊椎动物学报,1998,36 (2):147～158.
145.殷鸿福.三叠纪古地理及大陆漂移.地质科学,1980,(3):265～278.
146.殷鸿福等.中国古生物地理学.北京:中国地质大学出版社,1988.
147.郭双兴,吴向午.辽宁西部晚侏罗世晚期义县组的似麻黄植物.古生物学报,2000,39 (1):81～91.
148.郭洪中,张招崇.辽宁西部中生代火山岩的基本特征.岩石矿物学杂志,1992,3:193～204.
149.郭胜哲、张立东,邢德利等.辽宁西部义县组研究新进展.中国地质,2001,(8):1～8.
150.郭胜哲、张立东,邢德和等.辽宁西部义县组湖相枕状熔岩的发现及其意义.地球学报,2002,23 (6):491～494.
151.顾知微.中国的侏罗系和白垩系.见:全国地层会议学术论文汇编,北京:科学出 版社,1962,1～84.
152.顾知微.热河动物化石群地质时代的研究.王鸿祯主编,中国地质学科发展的回顾—孙云铸教授百年诞辰纪念文集.武汉:中国地质大学出版社.1995,93～99.
153.高克勤,唐治路,汪筱林.辽宁晚侏罗世-早白垩世一长颈双弓类爬行动物.古脊椎动物学报,1999,37 (1):1～8.
154.曹正尧,吴舜卿,张平安,李杰儒.辽宁义县组单子叶植物化石的发现.科学通报,1997,42 (16):1764～1776.
155.曹正尧.辽西早白垩世义县组Rufforfia和Nageiopsis的发现及其地层意义.古生物学报,2001,40 (2):214～218.
156.曹军骥,张小曳,王丹等.晚新生代风尘沉积的稀土元素地球化学特征及其古气候意义.海洋地质与第四纪地质,2001,21 (1):97～101.
157.曹美珍.辽宁西部四合屯地区义县组西部介形类.Palaeoworld,热河生物群,1999,11:131～149.
158.梁鸿德、许坤.冀北-辽西地区侏罗-白垩系界线.第三届全国地层会议论文集,北京:地质出版社,2000,237～242.
159.黄本宏.东北北部石炭二叠纪陆相地层及古地理概况.地质论评,1982,28(5):396～401.
160.蒲荣干,吴洪章.辽宁西部中生界孢粉组合及其地层意义.辽宁西部中生代地层古生物(2)[M],北京:地质出版社,1985,121～212.
161.臧尧龄,刘志英,姜应星等.中国东北部火山岩带多重岩系迭加性及其成因和演化.李兆乃,王碧香主编:火山岩火山作用及有关矿产(中国地质学会论文集第1集).北京:地质出版社,1993,85～91.
162.潘华璋,朱祥根.辽宁北票四合屯地区义县组下部的腹足类化石.Palaeoworld,热河生物群.1999,11:80～91.
163.黎文本,刘兆生.辽西北票义县组底部的孢粉组合及其时代.Palaeoworld.1999,11:68～7.
164.黎文本、刘兆生.辽西北票义县组底部的孢粉组合及其时代.陈丕基,金帆主编:热河生物群,Palaeoworld 11(专辑).安徽:中国科学技术大学出版社,1999,11:68～79.
165.黎文本.中国早白垩世孢粉植物群及其地理分区.古生物学基础理论丛书编委会编辑,中国古生物地理区系.北京:科学出版社,1983,142～151.
166.魏菊英.地球化学.北京:科学技术出版社,25～58.
167. Axelrod D. I. , Bailey H. P. Palaeotemperature analysis of Tertiary flora[A]. Palaeogeog. Palaeoclimatol. Palaeoecol. , 1969, 6 (3) : 193～195.
168. Bailey I. W. , Sinnot E W. The climatic distribution of certain types of angiosperm leaves [J]. Am J Bot. 1916, (3) : 24～39.
169. Swisher C. C. Ⅲ. Yuan-qing Wang, Xiao-lin Wang. Cretaceous age for the ferthered dinosaurs of Liaoning, China. NATURE, 1999, 401 (1) : 58～51.
170. Dimichele, W. A. , Ecological Patterns in Time and Space. Paleobiology, 1994, 20 (2) : 89～92.
171. Dolph G E, Dilcher D L. . Foliar physiognomy as an aid in determining paleoclimate [J]. Palaeontographica B, 1979, 170: 151～172.
172. Doludenko M P, Orlovskaya E R. Jurassic flora of the Karatau Range, southern Kazakhstan[J]. Palaeontology, 1976, 19 (4) : 627～640.
173. Doludenko M P, Orlovskaya E R. Jurassic flora of the Karatau[M]. M. : Nauka, 1976, 1～260.
174. Dong Ren, Ziguang Guo. Three New Gerera and Three New Spicies of Dragonfles from the late Jurassic of Northeast China (Anisoptera: Aeshnidae, Gomphidae, corduliidae). Entomologia Sinica, 1996, 3 (2) : 95～105.
175. Dong Ren, Ziguang Guo. A New genus and Two new species of short-horned files of upper Jurassic from northeast China. Entomologia Sinica, 1995, 2 (4) : 300-307.
176. Ge Sun, David L. Dilcher, Shaoling Zheng, Zhekun Zhou. In Search of the First Flower: A Jurassic Angiosperm, Archaefructus, from Northeast China. Science, 1998, 282 (5394) : 1601～1772.
177. Grabau A W. Stratigraphy of China Ⅱ (Mesozoic)[M]. Peiking: Geol Surv China, 1928, 1～774.
178. Grabau, A W. . Cretaceous mollusca from North China. Bull. Surv. China. 1923, No. 5, pt. 2. : 179～183.
179. Huo Lian-hai, Zhou Zhonghe et al. A beaked bird from the Jurassic of China. Nature, 1995, 377 (6550) : 616～618.
180. Jane E. Francis, Imogen Poole. Cretaceous and early Tertiary climates of Antarctica: evidence from fossil wood[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 182 (1～2) : 47～64.
181. Krassilov V A. Paleoecology of terrestrial plants[M]. Vladivostok: Far-East Cent Acad Sci, USSR, 1972, 1～208.
182. Krassilov V A. Angiosperm origins. Morphological and ecological aspects[M]. Sofia: Pensoft, 1997, 1～270.
183. L. D. Martin, Z. Zhou, L. Hou, A. Feduccia. Confuciusornis sanctus Compared to Archaeopteryx lithographica. Naturwissenschaften. 1998, 85: 286～289.
184. Lianhai Hou, Larry D. Martin, Zhonghe Zhou, Alan Feduccia, Fucheng Zhang. A diapsid skull in a new species of the primitive bird Confuciusornis. Nature, 1999, 399 (17) : 679～682.
185. Lianhai Hou, Larry D. Martin, Zhonghe Zhou, and Alan Feduccia. Early Adaptive Radiation of Birds: Evidence from Fossil from Northeastern china. Sciense, 1996, 274 (15) : 1164～1167.
186. Lian-hai Hou, Zhonghe Zhou, Larry D. Martin, Alan Feduccia. A beaked bird from the Jurassic of China. Nature, 1995, 377 (19) : 616～618.
187. Miki S. Mesozoic flora of Lycoptera beds in South Manchuria. Bull Mukogawa Woman's Univ. 1964, 12: S13～S22. (in Japanese with English abstract)
188. Norris G. . Misopores from the Purbeck beds and Marine upper Jurassic of Southern England. Palaeontology. 1969, (12) : 574～620.
189. Pei-ji Cheng, zhi-ming Dong, Shuo-nan Zhen. An exceptionally well-preserved theropod dinosaur from the Yixian Formation of China. Nature, 1998, 391 (8) : 147～152.
190. Qi-gao Sun, Margaret E. Collinson, Cheng-Sen Li, Yu-fei Wang, David J. Beerling. Quantitative reconstruction of palacoclimate from the Middle
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