收稿日期: 2015-07-13
修回日期: 2015-07-20
网络出版日期: 2019-09-19
基金资助
国家自然科学基金项目“中国南方海相热水沉积区优质烃源岩发育特征与成因机理”(编号:41472108)资助.
Hydrothermal sedimentary discrimination criteria and its coupling relationship with the source rocks
Received date: 2015-07-13
Revised date: 2015-07-20
Online published: 2019-09-19
贾智彬, 侯读杰, 孙德强, 黄奕雄 . 热水沉积判别标志及与烃源岩的耦合关系[J]. 天然气地球科学, 2016 , 27(6) : 1025 -1034 . DOI: 10.11764/j.issn.1672-1926.2016.06.1025
Key words: Hydrothermal sedimentation; Source rocks; Geochemistry
[1]Zhang Wenzheng,Yang Hua,Xie Liqin,et al.Lake-bottom hydrothermal activities and their influence on high-quality source rock development:A case from Chang 7 source rocks in Ordos Basin[J].Petroleum Exploration and Development,2010,37(4):424-429.[张文正,杨华,解丽琴,等.湖底热水活动及其对优质烃源岩发育的影响——以鄂尔多斯盆地长7烃源岩为例[J].石油勘探与开发,2010,37(4):424-429.]
[2]Zhou Yongzhang,Liu Jianming,Chen Duofu.Thread and knowledge to fossil sea-floor hydrothermal sedimentation of South China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2000,19(2):114-118.[周永章,刘建明,陈多福.华南古海洋热水沉积作用研究概述及若干认识[J].矿物岩石地球化学通报,2000,19(2):114-118.]
[3]Xue Chunji,Qi Sijing,Zheng Minghua,et al.Hydrothermalsediment research and associated scientific problems[J].Bulletin of Mineralogy,Petrology and Geochemistry,2000,19(3):155-163.[薛春纪,祁思敬,郑明华,等.热水沉积研究及相关科学问题[J].矿物岩石地球化学通报,2000,19(3):155-163.]
[4]Zhou Wenda,Ye Xifang.The research progress and trends on geology and geochemical of hydrothermal sedimentary deposit[J].Bulletin of Science and Technology,2014,30(1):31-38.[周闻达,叶锡芳.浅谈热水沉积矿床地质地球化学研究进展与趋势[J].科技通报,2014,30(1):31-38.]
[5]Zhou Yongzhang,He Junguo,Yang Zhijun,et al.Hydrothermally sedimentary formations and related mineralization in South China[J].Earth Science Frontiers,2004,11(2):373-377.[周永章,何俊国,杨志军,等.华南热水沉积硅质岩建造及其成矿效应[J].地学前缘,2004,11(2):373-377.]
[6]Tang Yongzhong,Qi Wen,Liu Shuwen,et al.Paleozoic hydrothermal sedimentary basin and hydrothermal sedimentary mineralization in the southern Qinling[J].Geology in China,2007,34(6):1091-1100.[唐永忠,齐文,刘淑文,等.南秦岭古生代热水沉积盆地与热水沉积成矿[J].中国地质,2007,34(6):1091-1100.]
[7]Gao Junbo,Yang Ruidong,Tao Ping,et al.Hydrothermal venting-flowing sedimentation characteristics of Devonian barite deposits from Leji,Zhenning County,Guizhou Province[J].Acta Sedimentologica Sinica,2012,30(3):422-430.[高军波,杨瑞东,陶平,等.贵州镇宁乐纪泥盆系重晶石矿热水沉积特征[J].沉积学报,2012,30(3):422-430.]
[8]Yang Ruidong,Zhu Lijun,Gao Hui,et al.A study on charaeteristics of the hydrothermal vent and relating biota at the Cambrian bottom in Songlin,Zunyi County,Guizhou Province[J].Geological Review,2005,51(5):481-492.[杨瑞东,朱立军,高慧,等.贵州遵义松林寒武系底部热液喷口及与喷口相关生物群特征[J].地质论评,2005,51(5):481-492.]
[9]Liang Digang,Guo Tonglou,Bian Lizeng,et al.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China(Part 3):Controlling factors on the sedimentary facies and development of Palaeozoicmarine source rocks[J].Marine Origin Petroleum Geology,2009,14(2):1-19.[梁狄刚,郭彤楼,边立曾,等.中国南方海相生烃成藏研究的若干新进展(三)南方四套区域性海相烃源岩的沉积相及发育的控制因素[J].海相油气地质,2009,14(2):1-19.]
[10]Zhang Weihua,Jiang Lijun,Gao Hui,et al.Study on sedimentary environment and origin of black siliceous rocks of the Lower Cambrian in Guizhou Province[J].Bulletin of Mineralogy,Petrology and Geochemistry,2003,22(2):174-178.[张位华,姜立君,高慧,等.贵州寒武系底部黑色硅质岩成因及沉积环境探讨[J].矿物岩石地球化学通报,2003,22(2):174-178.]
[11]Peng Jun,Tian Jingchun,Yi Haisheng,et al.The Late Precambrian hot water sedimentation of the southeast Yangtze Plate continental margin[J].Acta Sedimentologica Sinica,2000,18(1):107-113.[彭军,田景春,伊海生,等.扬子板块东南大陆边缘晚前寒武纪热水沉积作用[J].沉积学报,2000,18(1):107-113.]
[12]Deng Yi,Yang Rongfeng,Xiao Zhenghui,et al.Study on reservoir of Cambrian Niutitang Formation and sedimentary characteristics of shale gas reservoirs in Zhangjiajie[J].West-China Exploration Engineering,2013,25(12):119-122.[邓翼,杨荣丰,肖正辉,等.张家界地区下寒武统牛蹄塘组沉积特征与页岩气成藏研究[J].西部探矿工程,2013,25(12):119-122.]
[13]Bostrm K,Kraemer T,Gartner S.Provenance and accumulation rates of opaline silica,Al,Ti,Fe,Mn,Cu,Ni and Co in Pacific pelagic sediments[J].Chemical Geology,1973,11(2):123-148.
[14]Adachi M,Yamamoto K,Sugisaki R.Hydrothermal chert and associated siliceous rocks from thenorthern Pacific their geological significance as indication od ocean ridge activity[J].Sedimentary Geology,1986,47(1):125-148.
[15]Yamamoto K.Geochemical characteristics and depositional environments of cherts and associated rocks in the Franciscan and ShimantoTerranes[J].Sedimentary Geology,1987,52(1):65-108.
[16]Feng Shengbin,Zhou Hongrui,Yan Changhai,et al.Geochemical characteristics of hydrothermal cherts of Erlangping Group in east Qinling and their geologic significance[J].Acta Sedimentologica Sinica,2007,25(4):564-573.[冯胜斌,周洪瑞,燕长海,等.东秦岭二郎坪群硅质岩热水沉积地球化学特征及其地质意义[J].沉积学报,2007,25(4):564-573.]
[17]XuYuetong.The discovery of hydrothermal sediment cherts in Jiande copper deposit and its geological significance[J].Journal of Shandong Normal University:Natural Science,1997,12(1):54-59.[徐跃通.建德铜矿热水沉积硅质岩的发现及其地质意义[J].山东师范大学学报:自然科学版,1997,12(1):54-59.]
[18]Bostrm K,Peterson M N A.The origin of aluminum-poor ferromanganoan sediments in areas of high heat flow on the East Pacific Rise[J].Marine Geology,1969,7(5):427-447.
[19]Bostrm K.Genesis of Ferromanganese Deposits-diagnostic Criteria for Recent and Old Deposits[M].Springer US :Hydrothermal Processes at Seafloor Spreading Centers,1983:473-489.
[20][JP3]Rona P A.Criteria for recognition of hydrothermal mineral deposits in oceanic crust[J].Economic Geology,1978,73(2):135-160.
[21]Yan Changhai,Peng Yi,Liu Guoyin,et al.Geochemical characteristics of hydrothermal sedimentary chertsin the Erlangping Group,East Qinling Range,China[J].Geological Bulletin of China,2007,26(5):560- 566[燕长海,彭翼,刘国印,等.东秦岭二郎坪群热水沉积硅质岩的地球化学特征[J].地质通报,2007,26(5):560-566.]
[22]Sun Xingli,Chen Jianfa,Liu Wenhui,et al.Geochemical characteristics of cherts of Lower Cambrian in the Tarim Basin and its implication for environment[J].Petroleum Exploration and Development,2004,31(3):45-48.[孙省利,陈践发,刘文汇,等.塔里木盆地下寒武统硅质岩地球化学特征及其形成环境[J].石油勘探与开发,2004,31(3):45-48.]
[23]Rona P A,Bostrom K,Laubier L,et al.Hydrothermal Processes at Seafloor Spreading Centers[M].Plenum Press in cooperation with NATO Scientific Affairs Division,1982.
[24]Fleet A J.Hydrothermal and hydrogenous ferro-manganese deposits:Do they form a continuum:The rare earth element evidence[M]//Rona P A,Bostrom K,Laubier L,et al.Hydrothermal processes at seafloor spreading centers.Plenum Press in cooperation with NATO Scientific Affairs Division,1982:535-555.
[25]Peng Xiaotong,Li Jiwei,Zhou Huaiyang,et al.Characteristics and source of inorganic and organic compounds in the sediments from two hydrothermal fields of the central Indian and Mid-Atlantic Ridges[J].Journal of Asian Earth Sciences,2011.11(1):93-98.
[26]Duanmu Heshun.Geochemical characteristics and hydrothermal deposit cycling of sedimentary eruption ore deposit[J].Journal of Xi’an University of Science and Technology,2003,23(2):151-155.[端木合顺.沉积喷流型矿床热水沉积旋回及其地球化学特征[J].西安科技学院学报,2003,23(2):151-155.]
[27]Clayton R N.High temperature isotope effects in the early solar system[J].Reviews in Mineralogy and Geochemistry,1986,16(1):129-140.
[28]Knauth L P,Epstein S.Hydrogen and oxygen isotope ratios in nodular and bedded cherts[J].Geochimicaet Cosmochimica Acta,1976,40(9):1095-1108.
[29]Xu Yuetong,Zhou Baohua,Huang Fusheng.The geochemical characteristics of hydrothermal sediment for the bedded silicilith in the mesoproterozoic era and their sedimentary environment importance in Pingyin,Shandong Province[J].Acta Scientiarum Naturalium Universitatis Pekinensis,1997,33(2):167-174.[徐跃通,周保华,黄福生.山东平阴地区中元古代层状硅质岩热水沉积地球化学特征及沉积环境意义[J].北京大学学报,1997,33(2):167-174.]
[30]Liu Jiajun,Zheng Minghua.Geochemistry of hydrothermal sedimentary silicalite[J].Acta Geologica Sichuan,1993,13(2):110-118.[刘家军,郑明华.热水沉积硅岩的地球化学[J].四川地质学报,1993,13(2):110-118.]
[31][JP3]Douthitt C B.The geochemistry of the stable isotopes of silicon[J].Geochimicaet Cosmochimica Acta,1982,46(8):1449-1458.
[32]Fang Shiyi,Zheng Dayu.Principal ore-controlling factors and recognition criteria for the hydrothermal sedimentary metallogenesis[J].Uranium Geology,1993,9(4):27-30.[方适宜,郑大瑜.热水沉积成矿的主要控制因素及识别标志[J].铀矿地质,1993,9(4):27-30.]
[33]Yang Yanjun.A Preliminary Study on Exhalative Hydrothermal Deposits in the Lucaogou Formation in Jimusar Sag,Permian,Zhunggar Basin[D].Xi’An:Northwest University,2014.[杨焱钧.准噶尔盆地吉木萨尔凹陷二叠系芦草沟组热液喷流沉积初探[D].西安:西北大学,2014.]
[34]Sun Xingli,Chen Jianfa,Zheng Jianjing,et al.The characteristics of the isotopic composition of noble gas siliceous rocks at Cambrian bottom in Tarim Basin[J].Science in China:Series D, 2008,38 (S2):105-109.[孙省利,陈践发,郑建京,等.塔里木盆地寒武系底部硅质岩的稀有气体同位素组成特征[J].中国科学:D 辑,2008,38 (增刊Ⅱ):105-109.]
[35]Nie Haikuan,Bian Ruikang,Zhang Peixian,et al.Micro-types and characteristics of shale reservoir of the Lower Paleozoic in southeast Sichuan Basin,and their effects on the gas content[J].Earth Science Frontiers,2014,21(4):331-343.[聂海宽,边瑞康,张培先,等.川东南地区下古生界页岩储层微观类型与特征及其对含气量的影响[J].地学前缘,2014,21(4):331-343.]
[36]Liang Yu,Hou Dujie,Zhang Jinchuan,et al.Hydrothermal activities on the seafloor and evidence of organic-rich source rock from the Lower Cambrian Niutitang Formation,northwestern Guizhou[J].Petroleum Geology and Recovery Efficiency,2014,21(4):28-32.[梁钰,侯读杰,张金川,等.海底热液活动与富有机质烃源岩发育的关系——以黔西北地区下寒武统牛蹄塘组为例[J].油气地质与采收率,2014,21(4):28-32.]
[37]Zhao Mingsheng,Wang Yue,Tian Jingchun,et al.A sedimentary environment analysis of black shales based on fossil assemblage characteristics:A case study of Cambrian Niutitang Formation in Changyang area,western Hubei[J].Geology in China,2013,40(5):1484-1492.[赵明胜,王约,田景春,等.从生物化石组合特征剖析黑色页岩的沉积环境——以鄂西长阳地区寒武系牛蹄塘组为例[J].中国地质,2013,40(5):1484-1492.]
[38]Zhang Haiquan,Xu Xiaosong,Liu Wei,et al.Late Ordovician-Early Silurian sedimentary facies and palaeogeographic evolution and its bearings on the black shales in the Middle-Upper Yangtze area[J].Sedimentary Geology and Tethyan Geology,2013,33(2):17-24.[张海全,许效松,刘伟,等.中上扬子地区晚奥陶世_早志留世岩相古地理演化与黑色页岩的关系[J].沉积与特提斯地质,2013,33(2):17-24.]
[39]Yue Laiqun,Kang Yongshang,Chen Qingli,et al.Analysis of shale gas potential of Niutitang Formation of Lower Cambrian in Guizhou,China[J].Xinjiang Petroleum Geology ,2013,34(2):123-128.[岳来群,康永尚,陈清礼,等.贵州地区下寒武统牛蹄塘组页岩气潜力分析[J].新疆石油地质,2013,34(2):123-128.]
[40]Yu Kuanhong,Jin Zhenkui,Su Kui,et al.The sedimentary characteristics and petroleum exploration significance of northern marginin the Middle and Upper Yangtze Platform[J].Scientia Sinica Terrae,2013,43(9):1418-1435.[余宽宏,金振奎,苏奎,等.中、上扬子地台北缘寒武纪沉积特征及油气勘探意义[J].中国科学:地球科学,2013,43(9):1418-1435.]
[41]Yao Xu,Zhou Yaoqi,Li Su,et al.Research status and advances in chert and Permian chert event[J].Advances in Earth Science,2013,28(11):1189-1200.[姚旭,周瑶琪,李素,等.硅质岩与二叠纪硅质沉积事件研究现状及进展[J].地球科学进展,2013,28(11):1189-1200.]
[42]Yong Ziquan,Zhang Xuan,Deng Haibo,et al.Differerces about organic matter enrichment in the shale section of Ediacaran Doushantuo Formation in west Hubei of China[J].Journal of Chengdu University of Technology:Science & Technology Edition ,2012,39(6):567-574.[雍自权,张旋,邓海波,等.鄂西地区陡山沱组页岩段有机质富集的差异性[J].成都理工大学学报:自然科学版,2012,39(6):567-574.]
[43]Li Hong,Liu Yiqun,Liang Hao,et al.Origin of lacustrine dolostones of the Middle Permian Lucaogou Formation in Santanghu Basin of Xinjiang[J].Journal of Palaeogeography,2012,14(1):45-58.[李红,柳益群,梁浩,等.新疆三塘湖盆地中二叠统芦草沟组湖相白云岩成因[J].古地理学报,2012,14(1):45-58.]
[44]Wang Zhengjiang,Wang Jian,Zhuo Jiewen,et al.Crustextensional activity during the transition from Sinian(Ediacaran) to Cambrian in Yangtze Block:Evidences from the depositional sequence and its geochemical data[J].Geological Review,2011,57(5):731-742.[汪正江,王剑,卓皆文,等.扬子陆块震旦纪—寒武纪之交的地壳伸展作用:来自沉积序列与沉积地球化学证据[J].地质论评,2011,57(5):731-742.]
[45]Qiu Zhen,Wang Qingchen,Yan Detian.Geochemistry and sedimentary background of the Middle-Upper Permian chertsin the Penglaitan Section,Laibin,Guangxi Province[J].Acta Petrologica Sinica,2011,27(10):3141-3155.[邱振,王清晨,严德天.广西来宾蓬莱滩剖面中上二叠统硅质岩的地球化学特征及沉积背景[J].岩石学报,2011,27(10):3141-3155.]
[46]Pang Weihua,Ding Xiaozhong,Gao Linzhi,et al.Characteristics ofsequence stratigraphy and plaeoenvironmental evolution of Lower Cambrian strata in Hunan Province[J].Geology in China,2011,38(3):560-576.[庞维华,丁孝忠,高林志,等.湖南下寒武统层序地层特征与古环境演化变迁[J].中国地质,2011,38(3):560-576.]
[47]Ma Wenxin,Liu Shugen,Chen Cuihua,et al.Geochemicalcharacteristics of the siliceous rock in the Upper Sinian Dengying Formation in the eastern Chongqing,China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2011,30(2):160-171.[马文辛,刘树根,陈翠华,等.渝东地区震旦系灯影组硅质岩地球化学特征[J].矿物岩石地球化学通报,2011,30(2):160-171.]
[48]Liu Jiaqi.Characteristics of lacustrine Carbonate Reservoirs of the Upper Es4 in Western Zhanhua Sag[D].Beijing:China University of Geosciences(Beijing),2011.[柳佳期.沾化凹陷西部地区沙四上亚段湖相碳酸盐岩储层特征[D].北京:中国地质大学(北京),2011.]
[49]Hou Dongzhuang.Researchon Geochemical Characteristics and Sedimentary Environments of Black ShalesintheEastern Guizhou[D].Changsha:Central South University,2011[侯东壮.黔东地区黑色岩系地球化学特征及沉积环境研究[D].长沙:中南大学,2011.]
[50]Qiu Zhen,Wang Qingchen.Geochemistry and sedimentary background of the Middle-Upper Permian cherts in the Xiang-Qian-Gui region[J].Acta Petrologica Sinica,2010,26(12):3612-3628.[邱振,王清晨.湘黔桂地区中上二叠统硅质岩的地球化学特征及沉积背景[J].岩石学报,2010,26(12):3612-3628.]
[51]Cai Wen.Geochemical Characteristics and Ancient Environment Analysis of the Upper Paleozoic in Midu Area[D].Kunming:Kunming University of Science and Technology,2010.[蔡稳.弥渡地区上古生界沉积地球化学特征及古环境分析[D].昆明:昆明理工大学,2010.]
[52]Li Hongjing.Sequeneestratigraphy Analysis and High Quality Source Rock Identification in Typical Permian sections,Yangtze Area[D].Wuhan:China University of Geosciences,2009.[李红敬.扬子地区二叠系典型剖面层序地层分析及优质烃源岩判识[D].武汉:中国地质大学,2009.]
[53]Xiong Yaping.Sedimentary Geochemistry and Ore-bearing Potentiality of the Early Cambrian Black Rock Series in Shitai County,Anhui Province[D].Hefei:Hefei University of Technology,2008[熊亚平.安徽石台早寒武世黑色岩系沉积地球化学及含矿性[D].合肥:合肥工业大学,2008.]
[54]Wen Huaguo,Zheng Rongcai,Qing Hairuo,et al.Primary dolostone related to the Cretaceous lacustrine hydrothermal sedimentation in Qingxi Sag,Jiuquan Basin on the northern Tibetan Plateau[J].Scientia Sinica Terrae,2014,44(4):591-604.[文华国,郑荣才,Qing Hairuo,等.青藏高原北缘酒泉盆地青西凹陷白垩系湖相热水沉积原生白云岩[J].中国科学:地球科学,2014,44(4):591-604]
[55]Luo Chao,Liu Shugen,Sun Wei,et al.Basiccharacteristics of shale gas in the Lower Cambrian Niutitang Formation in the Upper Yangtze Region:Taking Nangaosection in Danzhai as anexample[J].Natural Gas Geoscience,2014,25(3):453-470.[罗超,刘树根,孙玮,等.上扬子区下寒武统牛蹄塘组页岩气基本特征研究——以贵州丹寨南皋剖面为例[J].天然气地球科学,2014,25(3):453-470.]
[56]Li Shuangying,Meng Qingren,Wan Qiu,et al.Deposition of carbonate slope and ore-forming in Permian strata in the Middle-Lower reaches of the Yangzte River,East China[J].Acta Petrologica Sinica,2008,24(8):1733-1744.[李双应,孟庆任,万秋,等.长江中下游地区二叠纪碳酸盐斜坡沉积及其成矿意义[J].岩石学报,2008.24(8):1733-1744.]
[57]Qiao Gengbiao,Yang Zhongtang,Li Zhiming,et al.REE geochemical characteristics of the Cambrian carbonaceous rock series in the Mian-Lǜe Region and their genetical implications[J].Journal of Jilin University:Earth Science Edition,2011.41(4):1067-1076.[乔耿彪,杨钟堂,李智明,等.勉略地区寒武纪含碳岩系稀土元素地球化学特征及成因意义[J].吉林大学学报:地球科学版,2011,41(4):1067-1076.]
[58]Liu An,Li Xubing,Wang Chuanshang,et al.Analysisof geochemical feature and sediment environment for hydrocarbon source rocks of Cambrian in west Hunan-Hubei area[J].Acta Sedimentologica Sinica,2013.31(6):1122-1132.[刘安,李旭兵,王传尚,等.湘鄂西寒武系烃源岩地球化学特征与沉积环境分析[J].沉积学报,2013.31(6):1122-1132.]
[59]Zhao Zhan,Xie Yuan,Liu Jianqing,et al.REE geochemical signatures and sedimentary environments of the Lower Cambrian black rock series in Southeastern Chongqing and its adjacent areas[J].Sedimentary Geology and Tethyan Geology,2011,31(2):49-54.[赵瞻,谢渊,刘建清,等.渝东南下寒武统黑色岩系稀土元素地球化学特征与沉积环境[J].沉积与特提斯地质,2011,31(2):49-54.]
[60]Li Tianyi,He Sheng,Yang Zhi.The marine source rock formation conditions and control factors[J].Geological Science and Technology Information,2008,27 (6):63-70.[李天义,何生,杨智.海相优质烃源岩形成环境及其控制因素分析[J].地质科技情报,2008,27 (6):63-70.]
[61]Chen Jianfa,Zhang Shuichang,Bao Zhidong,et al.Main sedimentary environments and influencing factors for development of marine organic-rich source rocks[J].Marine Origin Petroleum Geology,2006,11(3):49-53.[陈践发,张水昌,鲍志东,等.海相优质烃源岩发育的主要影响因素及沉积环境[J].海相油气地质,2006,11(3):49-53.]
[62]Akande S O,Egenhoff S O,Obaje N G,et al.Hydrocarbon potential of Cretaceous sediments in the Lower and Middle Benue Trough,Nigeria insights from new source rock faciesevaluation[J].Journal of African Earth Sciences,2012.64(64):34-47.
[63]Jiang Jianjun.The status quo of the sea level changes in the Paleozoic and Mesozoic Era[J].Acta Oceanologica Sinica,1991,13(5):715-720.[姜建军.古生代、中生代海平面变化现状[J].海洋学报,1991,13(5):715-720.]
[64]Wu Xiaoqi,Tao Xiaowan,Liu Jingdong.Geochemical characteristics and genetic types of natural gas from Lunnanarea in Tarim Basin[J].Natural Gas Geoscience,2014,25(1):53-61.[吴小奇,陶小晚,刘景东.塔里木盆地轮南地区天然气地球化学特征和成因类型[J].天然气地球科学,2014,25(1):53-61.]
[65]Gu Zhidong,Wang Zecheng,Hu Suyun,et al.Tectonicsetting of global marine carbonate giant fields and exploration signficance[J].Natural Gas Geoscience,2012,23(1):106-117.[谷志东,汪泽成,胡素云,等.全球海相碳酸盐岩巨型油气田发育的构造环境及勘探启示[J].天然气地球科学,2012,23(1):106-117.]
[66]Yang Xin,Xu Xuhui,Chen Qianglu,et al.Palaeotectonicspattern in Pre-Cambrian and its control on the depositon of the Lower Cambrian source rocks in Tarim Basin,NW China[J].Natural Gas Geoscience,2014,25(8):1164-1171.[杨鑫,徐旭辉,陈强路,等.塔里木盆地前寒武纪古构造格局及其对下寒武统烃源岩发育的控制作用[J].天然气地球科学,2014,25(8):1164-1171.]
[67]Leng Jigao,Han Jianhui,Li Fei,et al.Exploration potential of shale gas in Huayuan block,northwest Hunan Province[J].Natural Gas Geoscience,2014,25(4):624-631.[冷济高,韩建辉,李飞,等.湘西北地区花垣页岩气区块勘探潜力[J].天然气地球科学,2014,25(4):624-631.
[68]Chen Jianfa,Sun Xingli,Liu Wenhui,et al.Geochemical characteristics and genesis of the organic layer in the bottom of the Lower Cambrian in Tarim Basin[J].Science in China:Series D,2004,34(supplement1):107-113.[陈践发,孙省利,刘文汇,等.塔里木盆地下寒武统底部富有机质层段地球化学特征及成因探讨[J].中国科学:D 辑,2004,34(增刊1):107-113.]
[69]Sun Xingli,Chen Jianfa,Liu Wenhui,et al.Hydrothermal venting on the seafloor and formation of organic-rich sediments:Evidence from the Neo Proterozoic Xiamaling Formation,North China[J].Geological Review,2004,49(6):588-595.[孙省利,陈践发,刘文汇,等.海底热水活动与海相富有机质层形成的关系——以华北新元古界青白口系下马岭组为例[J].地质论评,2004,49(6):588-595.]
[70]Sun Xingli,Chen Jianfa.Prelminary study of geochemical characteristics and formation of organic matter rich stratigraphy of Xiamaling Formation of Later Proterozoic innorth China[J].Natural Gas Geoscience,2004,15(2):110-114.[孙省利,陈践发.华北新元古界下马岭组富有机质层段的地球化学特征及成因初探[J].天然气地球科学,2004,15(2):110-114.]
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