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《Acta Sedimentologica Sinica》 1988-04
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USEING MOLECULAR FOSSIL INDICATORS FORANALYSIS OF PALEOENVIRONMENTSOF A SEDIMENTARY BASIN,IN EASTEN CHINA

Li Renwei Li Zhe Wang Zhizhen Lin Daxing (Institute of Geology Academia Sinica, Beijing)  
In this paper, not only the already well known molecular fossil indicators have been summarized, but also some new ones are proposed for analysis of pale-oenvironments of a sedimentary basin, and the adaptability of them for this is verified and reviewed. Molecular fossils are biogenic molecules, coming from the remains of organism in sediments and being of a certain implication in sedimentology or/and paleontology. Although experienced changes in diagenesis, yet they keep the carbon skeleton inherited from their biological precursors. Only n-alkanes, isoprenoid hydrocarbons, steranes and terpanes are detailed in this paper. l.Up to now, n-alkanes have been effective indicators of the sourceof organic matter in sedimentary rocks and crude oils. Generally, if the organic matter is made up mainly of the" terrigenous"type, it reflects a sedimentary environment of fluvial, or deltaic, or marginal facies in a basin. On the contrary, if the organic matter is made up mainly of the " autochonous in basin" type, it reflects an environment of central basin facies or lacking terrigenous substances. 2.A preference of even over odd carbon number n-alkanes ( i.e.OEP or CPI1) is an indicator or reducing-even strong reduing environments. It is shown, by a systematic comparison of the contents of pyrite-Fe, a reductive authigeni c mineral indicator, in Fe-containing minerals with the CPI of the rocks from the Lower Tertiary in Dongpu Basin,that there is a quite good correlation between them (Fig.2,a) .For the samples with CPI1, their contents of pyrite-Fe in Fe-con taining minerals all are over 50%. As the CPI values are getting smaller, the contents of pyrite-Fe higher; furthermore the correlation between them is much better. It is indicated by the comparison that the OEP or CPI indicator to reduc-ti on,even strong reduction would be adaptible to paleoenvironmental analysis, least in our cas es. 3.A predominance of n-C22 in a-alkanes may be an indicator of hypersalino environments. There are the predominances of n-C22 in many rocks and crude oils formed in hypersaline environments from the lower Tertiary basins of Dongpu and Subei (Fig.3 ).However, the evaporites (Fig.3,No.84009, 84010 and 84016)and,in a series of the rocks in an order of increasing salinity formed in hypersaline environments(Fig.3, from No. 84052 to 84055), No. 84052 and 48053 have no such a predominance, which shows that the n-C22 predominancn in n-alkanes may be an indicator of hypersalinity only within a certain range. 4.Isoprenoid alkanes such as C20(phytane) , C25,C30 and C40 are the indicators of archaeodacteria activity.In the basins of Dongpu and Subei, as well as some of other Cenozoic and Mesozoic basins of China, strong predominances of phytane have been found, the content of Ph is several to tens times that both of Pr and n-C18 in a rock. Such a strong predominance of phytane probably is a molecular indicator of extreme halophile archaeobacteria activitiy. The C16-C30, esp. the C25, C17 etc. regular isoprenoid alkane have been found in the basins mentioned above (Fig.4) . They may be a molecular indicator of the activities of thermoacidophiles or extreme halophiles. 5.Pr/Ph is an oxidation-reduction indicator. It is found, by a systemtic comp-arision between the Pr/Ph and the contents of pyrite-Fe like section 2, that the Pr/Ph of the rocks from Dongpu Basin arel if their contents of pyrite-Fe50% ( Fig.2,b) .Therefore, the Pr/Phl ( like CPKl ) reflects a reducing environment quite reliably. However, it should be careful in its application to the rocks formed in hypersaline environments. 6.A strong predominance of phytane may bean indicator of hypersaline environ -ments. It has been found indeed that all the eraporites and most of the rocks formed in hypsrsaline envioments as well, from basins of Dongpu, Subei etc. have the strong predominance of phytane(Phn-C18 and Ph籔r) . On the contrary, generally, there is no such a predominance in the rocks forned under relatively freshening conditions. 7.A relativaly high abundance of C25 regular
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【References】
Chinese Journal Full-text Database 10 Hits
1 XIONG Yong zhu, LIN Li, ZHU Li dong, PANG Yan chun, FU Xiu gen (College of Earth Sciences, Chengdu University of Technology, China);AN APPROACH TO THE WEB-BASED INFORMATION SYSTEM OF MOLECULAR FOSSILS[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-03
2 Bao Jianping Wang Tieguan (Jianghan Petroleum Institute) Gan Yinu (Geoscience Institute of Jiangsu Petroleum Exploration Bureau);Biomarker Assemblage and Study on Sedimentary Environments of Member 2 of Funing Formation, Lower Tertiary, Jinhu Sag, Subei Basin[J];Acta Sedimentologica Sinica;1991-04
3 LIN Jin hui 1 YI Hai sheng 2 LI Yong 2 WANG Cheng shan 2 PENG Ping an 3 1(Testing and Analyzing Centre, Chengdu University of Technology, Chengdu 610059) 2(Institute of Sedimentology, Chengdu University of Technology,Chengdu 610059) 3(Gu;Characteristics of Biomarker Compounds and Its Implication of Middle Jurassic Oil Shale Sequence in Shuanghu Area, Northern Tibet Plateau[J];Acta Sedimentologica Sinica;2001-02
4 LIN Jin-hui 1 ,YI Hai-sheng 2 ,ZOU Yan-rong 3 (1.Testing and Analyzing Center,Chengdu University of Technology,Chengd u610059,China;2.Institute of Sedimentology,Chengdu University of Tech nology,Chengdu610059,China;3.State Key Laboratory of Organic Geochemi stry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzho u510640,China);Biomarkers of marine and continental oil shales,the Zangbei Plateau[J];Geochimica;2004-01
5 YANG Wen-guang1,ZHU Li-dong1,MI Wen-tian1,WANG Cheng-shan2 LI Ya-lin2,HUANG Hui1,WU Jing-long1,YANG Lin1,ZHOU Xiao-lin1 1.Instiute of Sedimentary Geology,Chengdu University of Technology, Chengdu 610059,China; 2.Institute of the Qinghai-Tibet Plateau Geology,China University of Geosciences, Beijing 100083,China;Study on the biomarkers characteristics of hydrocarbon source rocks from Cenozoic Yaxicuo Group in the Yanghu basin of Tibet,China[J];Journal of Chengdu University of Technology(Science & Technology Edition);2011-06
6 Bao Jianping Wang Tieguan(Analytical Experiment and Research Center, JPI) Gan Yinu(Geoscience Institute of Jiangsu Petroleum Exploration Bureau);DEHYDROXYTOCOPHEROL AND ITS GEOCHEMICAL SIGNIFICANCES[J];Journal of Jianghan Petroleum Institute;1989-03
7 Zhang Chengjun1 ,Cui Yanli2 ( 1.School of Resources and Environments,Lanzhou University,L anzou,730 0 0 0 ,China; 2 .Prospecting Bureau of Tu- Ha Oil- field,Shanshan,8390 2 9,China);Sedimentary Environment Interpreted by the Characteristics of Organic Matters in Xicheng Ore-field[J];Journal of Lanzhou University;2000-01
8 XU Yao-hui~(1,2)(1.Department of Geochemistry,Yangzte University,Jingzhou,Hubei,434023;2.Key Laboratory of Exploration Technologies for Oil and Gas Resources(Yangtze University),Ministry of Education,Jingzhou,Hubei,434023);Biomarker Characteristics of Saturated Hydrocarbon of the Source Rocks and Geochemical Significance from the Lower and Middle Jurassic in Tula Basin[J];Inner Mongolia Petrochemical Industry;2006-11
9 Li Shoujun/ / 1999,23(5);SEDIMENTARY ENVIRONMENTAL SIGNIFICANCE OF NORMAL ALKANE AND THE RATIO OF PRISTANE TO PHYTANE[J];JOURNAL OF THE UNIVERSITY OF PETROLEUM,CHINA;1999-05
10 Den Hongwen (China University of Geosciences)Qian Kai (Natural Gas Branch,Scientific Research Institute of Petroleum Exploration and Development,CNPC);GEOCHEMICAL BINARY DIVISION CHARACTER OF LACUSTRINE ARGILLITE[J];Oil & Gas Geology;1993-02
【Citations】
Chinese Journal Full-text Database 1 Hits
1 Lu Songnian Li Weimin Gu Huimin Gao Pinwen (Beijing Postgraduate School,Wuhan College of Geology);BIOMARKERS OF TERTIARY SOURCE ROCKS IN DONGTAI DEPRESSION AND THEIR GEOLOGICAL-GEOCHEMICAL SIGNIFICANCE[J];Oil & Gas Geology;1985-01
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 Fei Fuan (Bureau of Petroleum Geology of East China, Ministry of Geology and Minerals);DISCUSSION ON THE PALEOENVIRONMENT AND PALEOCLIMATE OF LOWER TERTIARY IN THE NORTH JIANGSU PETROLIFEROUS BASIN[J];Acta Sedimentologica Sinica;1988-01
2 ZHU Guang-you JIN Qiang (College of Geo-Resource and Information,University of Petroleum,Dongying Shan dong 257061);Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression[J];Acta Sedimentologica Sinica;2003-03
3 Lu Songnian Li weimin Gao Jianjun ( Wuhan College of Geology, Wuhan 430074 ) Chen Yixian Song Shaoying ( Scientific Technological Institute of Liaohe Oilfield );THE BIOLOGICAL MARKERS IN THE CRUDE OIL AND SOURCE ROCKS OF LOWER TERTIARY FROM WESTERN DEPRESSION, LIAOHE BASIN[J];;1986-03
4 ZHU Guang-you~(1), JIN Qiang~(2), ZHANG Shui-chang~(1), WANG Guan-min~(2), LIANG Ying-bo~(1)1.Research Institute of Petroleum Exploration and Development, PetroChina,Beijing 100083, China 2.College of Geo-resources and Information, China University of Petroleum, Dongying 257061, China;Positive correlation between contents of TOC and Sr in source rocks of the Palaeogene Shahejie Formation in Dongying Sag,eastern China[J];Earth Science Frontiers;2005-04
5 ZHU Guang-you1, JIN Qiang1, ZHOU Jian-lin 2,3, ZHANG Lin-ye4 (1. Faculty of Geo-Resource and Information in the University of Petroleum, Dongying 257061; 2. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002; 3. Shengli Production Factory in Shengli Oil Field, Dongying 257051; 4. Geo-Science Academy in Shengli Oil Field, Donying 257015);STUDY OF THE CONTROLLING FUNCTION OF PACKING PROCESS FOR HYDROCARBON SOURCE ROCKS[J];Geology-geochemistry;2003-02
6 Chen Youfei, Yan Qinshang Xu Shiyuan(East China Ncrmal University);EVOLUTION OF THE SEDIMENTARY ENVIRONMENTS IN NORTH JIANGSU BASIN AND ITS TECTONIC SETTING[J];Chinese Journal of Geology;1993-02
7 Zhu Guangyou 1 Jin Qiang 1 Zhou Jianlin 2 (1. Faculty of Geo resources and Information, University oF Petroleum, Dongying, Shandong257061; 2. Shengli Production Plant of Shengli Administration, Dongying, Shandong257051);SOURCE ROCK CHARACTERS OF CYCLIC DEEP LAKE FACIES IN THE DONGYING DEPRESSION[J];Scientia Geologica Sinica;2003-02
8 ZHU Guangyou 1), JIN Qiang 2), ZHANG Shuichang 1), DAI Jinxing 1), ZHANG Linye 3), LI Jian 1) 1) Research Institute of Petroleum Exploration and Development, CNPC, Beijing, 100083 2) Faculty of Earth Resources and Information, China University of Petroleum, Dongying, 257061 3) Geoscience Academe of the Shengli Oil Field, Donying, Shandong, 257015;Combination Characteristics of Lake Facies Source Rock in the Shahejie Formation, Dongying Depression[J];Acta Geologica Sinica;2004-03
9 CAO Jian1),BIAN Lizeng1),HU Kai1),LIU Yuntian1,2),WANG Liqun2),YANG Shaoyong2),CHEN Yan2)1) Department of Earth Sciences,Nanjing University,Nanjing,210093;2) PetroChina Qinghai Oilfield Company,Dunhuang,Gansu,736202;Biomarker Features of Jurassic Mudstone Source Rock from Different Sedimentary Environments in the Northern Qaidam Basin and Its Applications[J];Acta Geologica Sinica;2008-08
10 ZHU Guang-you 1,JIN Qiang 2,DAI Jin-xing 1,ZHANG Shui-chang 1,ZHANG Lin-ye 3,LI Jian 1 (1.Research Instiute os Petroleum Exploration and Development,CNPC,Beijing 100083,China;2.Collgeg of Georesource and Information,University of Petroleum, Dongying,257061 China;3.Geoscience academy,Shengli Oil Field,Donying,257015 China);Investigation on the Salt Lake Source Rocks for Middle Shasi Column of Dongying Depression[J];Geological Journal of China Universities;2004-02
【Co-references】
Chinese Journal Full-text Database 10 Hits
1 E. Derbyshire (Geography Department, Keele University, England) J. Shaw (Geology Deportment, Cardiff Universitry, England) Wang Jingtai (Lanzhou Institute of Glaciology and Geocryology, Academia Sinica );Palaeomagnetic Age of the Borehole No.1 of Dabuxun Lake, Qaidam Basin[J];Journal of Glaciology and Geocryology;1985-03
2 YUAN Lin wang, CHEN Ye, ZHOU Chun lin, LIU Ze chun (Geo-Science School of Nanjing Normal University, Nanjing Jiangsu 210097, China) [HT];Correlation of Environmental and Climatic Change Between Qaidam Basin Gamma Ray Logging Curve and Guliya Ice Core δ~(18) O Record Since the Last Interglacial Cycle[J];Journal of Glaciolgy and Geocryology;2000-04
3 CHEN Tuo~ 1, 2\},\ QIN Da\|he~ 1,\ HE Yuan\|qin~ 1,\ REN Jia\|wen~ 1,\ LIU Xiao\|hong~ 1 (1.Key Laboratory of Ice Core and Cold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000, China; 2.National Laboratory of Western Chinas Environmental;The Pattern of Stable Carbon Isotope Ratios in \%Sabina przewalskii\%[J];Journal of Glaciolgy and Geocryology;2002-05
4 CHEN Tuo 1, 2 , YANG Mei-xue 1, FENG Hu-yuan 1, 3, XU Shi-jian 3,QIANG Wei-ya 3, HE Yuan-qing 1, AN Li-zhe 1, 3 (1.Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China; 2.National Laboratory of Western Chinas Environmental Systems, MOE, Lanzhou University, Lanzhou Gansu 730000, China; =3.School of Life Sciences, Lanzhou University, Lanzhou Gansu 730000, China)=;Spatial Distribution of Stable Carbon Isotope Compositions of Plant Leaves in the North of the Tibetan Plateau[J];Journal of Glaciology and Geocryology;2003-01
5 WANG Peng-ling,JIA Yu-lian,ZHU Cheng,MA Chun-mei(Urban and Resources Department of Nanjing University, Nanjing Jiangsu 210093, China);Climatic Evolution of the Tibetan Plateau during the Last Deglaciation: Correlation with Europe and Greenland[J];Journal of Glaciology and Geocryology;2004-01
6 YUAN Lin-wang,LIU Ze-chun,CHEN Ye (Geo-Science School of Nanjing Normal University, Nanjing Jiangsu 210097, China);Paleoclimatic Change Derived from Natural Gamma-Logging Curve in Qaidam Basin and Its Relation to the Solar Insolation[J];Journal of Glaciology and Geocryology;2004-03
7 WU Chaodong\ YANG Chengyun (Department of Geology,Peking University,Beijing,100871) CHEN\ Qiying (Institute of Geology,Chinese Academy of Sciences,Beijing,100029);The Hydrothermal Sedimentary Genesis of Barite Deposits in West Hunan and East Guizhou[J];ACTA SCICENTIARUM NATURALUM UNIVERSITIS PEKINESIS;1999-06
8 LI Duoli GUAN Ping (School of Earth and Space Sciences ,Peking University, Beijing, 100871);Research Situation and Prospect of Hydrocarbon Migration in China[J];Acta Scicentiarum Naturalum Universitis Pekinesis;2004-04
9 MU Nan WU Chaodong(Department of Geology,School of Earth and Space Sciences,Peking University,Beijing,100871);Characteristics and Phosphogenesis of Phosphorite of the Sinian-Cambrian,West Yangtze Area[J];Acta Scicentiarum Naturalum Universitis Pekinesis;2005-04
10 YIN\ Chungu (Department of Geology,Peking Univer sity,Beijing,100871) ZHANG\ Yun (College of Life Science,Peking University,Beijing,100871) JIANG\ Naihuang (Research Institute of Petroleum Exploration & Development,Beijing,100083);Organic Matters from the Fossil bearing Phosphorites of the Neoproterozoic Doushantuo Formation in Guizhou,South China[J];ACTA SCICENTIARUM NATURALUM UNIVERSITIS PEKINESIS;1999-04
【Secondary References】
Chinese Journal Full-text Database 10 Hits
1 WANG Shi-hui~(1,2),CHEN Chun-rui~2,ZHENG Yu-long~2,LIU Sheng-ying~(2,3)1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China2.The Oilfield Exploration and Development Research Institute,Daqing Oilfield Co.Ltd,Daqing,Heilongjiang 163712,China3.School of Energy Resources,China University of Geosciences,Beijing 100083,China;Study on Geochemical Characteristics and Genesis of the Dalianhe Oil Shale in Heilongjiang Province[J];Journal of Jilin University(Earth Science Edition);2006-06
2 LI Zhong-xiong1,2,HE Jiang-lin2,3,XIONG Xing-guo4,WU Tao4,BAI Pei-rong41.Institute of Resources,China University of Geosciences,Wuhan 430074,China2.Chengdu Institute of Geology and Mineral Resources,Chengdu 610082,China3.Graduate Department,Chinese Academy of Geological Sciences(CAGS),Beijing 100037,China4.Institute of Geological Survey of Guizhou,Guiyang 550005,China;The Upper Jurassic-Lower Cretaceous Shenglihe Oil Shales and Their Formation in the Qiangtang Basin,Northern Xizang[J];Journal of Jilin University(Earth Science Edition);2010-02
3 Tonger LIU Wen-hui XU Yong-chang (Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Lanzhou 730000);The Discussion on Anoxic Environments and Its Geochemical Identifying Indices[J];Acta Sedimentologica Sinica;2004-02
4 DUAN Yi ZHANG Hui ZHENG Chao-yang WU Bao-xiang (Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 73000);Study on Genesis of Crude Oil from Qaidam Basin[J];Acta Sedimentologica Sinica;2004-S1
5 LIU Jun-hai~(1)CHEN Xiao-hong~(1)YANG Xiang-hua~(2)LV Xin-hua~(3)(1.China University of Petroleum,Beijing 102249;2.China University of Geosciences,Wuhan 430074;3.Zhongyuan Oilfield Company,SINOPEC,Puyang,Henan457001);Geochemical Characteristics of Carbazole Compounds in Lacustrine Oilsin Huqing Oilfield[J];Acta Sedimentologica Sinica;2006-01
6 HU Ying~(1) ZHANG Zhi-huan~(1) LI Wei~(1) WU Shui-ping~(2)(1.Key Laboratory for Hydrocarbon Accumulation,Ministry of Education,Faculty of Natural Resources & Information Technology,China University of Petroleum,Beijing 102249;2.Key Laboratory for Earth Surface Processes,Peking University,Beijing 100871);Molecular Biomarkers Characteristics of Source Rocks from Tanhai Sanma Area in the Huanghua Depression and Its Signification for Sedimentary Facies[J];Acta Sedimentologica Sinica;2006-03
7 CHEN Wen-bin LIAO Zhong-li FU Xiu-gen ZHANG Yu-jie PENG Zhi-min(Chengdu Institute of Geology and Mineral Resources,Chengdu 610082);Biomarker Characteristics and Significance of Hydrocarbon Source Rocks in Buqu Formation of the North Qiangtang Basin[J];Acta Sedimentologica Sinica;2007-05
8 SUN Min-zhuo1,2 MENG Qian-xiang1 FANG Xuan1 WANG Guo-cang1HUANG Xiang-bo3 Wang Zuo-dong1,2 XU Yin1(1.Key Laboratory of Gas Geochemistry,Chinese Academy of Sciences, Lanzhou 730000;2.Graduate University of Chinese Acadomy of Sciences, Beijing 100039;3.Tuha Petroleum Exploration and Development Corporation Natural-Gas Chemical Plant,Shanshan Xinjiang 838202);Geochemical Significance of the Microbial Function of Saturation Hydrocarbon of Calcilutites from the Sebei Well 1 of Qaidam Basin[J];Acta Sedimentologica Sinica;2009-01
9 WANG Li-cheng1,2 WANG Cheng-shan1,2 LI Ya-lin1,2 WEI Yu-shuai2,3 ZHU Li-dong4 CAO Ke1,2(1.China University of Geosciences,School of Earth Sciences and Resources,Beijing 100083;2.Research Center for Tibetan Plateau Geology,China University of Geosciences,Beijing 100083;3.Tibet Institute of Geological Survey,Lhasa 8500004.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059);Molecular Organic Geochemistry of Langshan Formation in Selincuo Sag,Coqen Basin,Central Tibet,China[J];Acta Sedimentologica Sinica;2009-06
10 HE Jiang-lin1,2 WANG Jian2 FU Xiu-gen2 SUN Tao3 SHEN Jia-nian4(1.Graduate Department,Chinese Academy of Geological Sciences(CAGS),Beijing 100037;2.Chengdu Institute of Geology and Mineral Resources,Chengdu 610082;3.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000;4.Daqing Petroleum Institute,Daqing,Heilongjiang 163318);Geochemical Characteristics and Geological Significance of Shengli River Oil Shale in Qiangtang Basin,Northern Tibet,China[J];Acta Sedimentologica Sinica;2010-03
China Proceedings of conference Full-text Database 2 Hits
1 LIU JiaJun, LIU ZhenJiang, YANG Yan, XIE Hui, WANG JianPing, MAO GuangJian and FENG CaiXia (State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China;Faculty of Geosciences and Resources, China University of Geosciences, Beijing 100083, China);Organic geochemical characteristics of the large barium ore belt in the Daba mountain[A];[C];2006
2 ZHANG Liping~*,ZENG Rongshu and XU Wendong Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;Preliminary Study on PAHs Distribution in High-grade Oil Shale and Its Spontaneous Combustion Product in Fushun,Liaoning Province[A];[C];2008
【Secondary Citations】
Chinese Journal Full-text Database 3 Hits
1 Shi Jiyang(Institute of Geochemistry, Academia Sinica)A. S. Mackenzie G. Bglinton, A. P. Gowar J. K. Maxwell (Organic Geochemistry Unit, School of Chemistry, University of Bristol, UK);BIOLOGICAL MARKERS FOR PETROLEUM AND SHALES IN SHENGLI OILFIELD AND THEIR GEOCHEMICAL IMPLICATIONS[J];Geochimica;1982-01
2 Li Renwei,Tian Xingyou and Lin Daxing(Institute of Geology,Academia Sinica,Beijing);THE AMINO ACIDS IN MUDSTONE FROM THE MEZO-CENOZOIC SEDIMENTARY BASINS,EAST CHINA[J];Chinese Journal of Geology;1983-02
3 Fei Fuan Liu Peihua (The Petroleum Exploration Headquarters of Jiangsu Province);THE RELATION BETWEEN PETROLEUM AND GEOTHERM IN THE DONGTAI DEPRESSION,NORTHERN JIANGSU[J];Oil & Gas Geology;1981-01
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