天然气地球科学 ›› 2012, Vol. 23 ›› Issue (4): 626–635.doi: 10.11764/j.issn.1672-1926.2012.04.626

• 天然气地球化学 • 上一篇    下一篇

川西地区二叠系烃源岩发育环境及控制因素

 张长江, 刘光祥, 曾华盛, 张关龙   

  1. 1.中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所,江苏 无锡 214126;
    2.中国石油化工股份有限公司胜利油田分公司西部新区研究中心,山东 东营 257015
  • 收稿日期:2012-01-13 修回日期:2012-04-23 出版日期:2012-08-10 发布日期:2012-08-10
  • 通讯作者: 张长江zcj.syky@sinopec.com. E-mail:zcj.syky@sinopec.com.
  • 作者简介:张长江(1968-),女,河北宣化人,高级工程师,硕士,主要从事石油地质与油气地球化学研究. E-mail:zcj.syky@sinopec.com.
  • 基金资助:

    中国石化股份公司科技开发部“四川盆地二叠系烃源岩及其资源潜力研究” 项目(编号:P08065)资助.

Depositional Environments and Controlling Factors ofPermian Source Rocks in Western Sichuan Basin

ZHANG  Chang-Jiang, LIU  Guang-Xiang, ZENG  Hua-Cheng, ZHANG  Guan-Long   

  1. 1.Wuxi Research Institute of Petroleum Geology,Petroleum Exploration and Production Research Institute,SINOPEC,Wuxi 214126,China;2.Research Center for New Blocks in West  China,Shengli Oilfield Company,SINOPEC,Dongying 257015,China
  • Received:2012-01-13 Revised:2012-04-23 Online:2012-08-10 Published:2012-08-10

摘要:

通过对川西地区什邡剖面二叠系进行系统的采样研究,发现不同沉积相对应不同的微量元素地球化学特征。P、Ba、Cr、Ni、Cu、Zn等生物发育的营养型元素富集,反映出具高的生物生产率;V/(V+Ni)值、V/Cr值、Sr/Ba值可以很好地指示有机质保存环境。二叠系烃源岩发育层段有机质丰度、沉积相与海侵―海退旋回的关系、有机质保存环境及生物繁茂程度等反映的地球化学特征相互吻合。微量元素地球化学特征对判别沉积相有重要的指示意义。

关键词: 二叠系, 微量元素, 控制因素, 烃源岩, 沉积环境, 地球化学特征, 川西地区

Abstract:

After sedimentary facies and trace elements geochemistry of Permian source rock in Shifang profile of the western Sichuan province is illustrated,we find out that different sedimentary facies have various characteristics of trace elements.The enrichment of nutritional elements such as P,Ba,Cr,Ni,Cu and Zn,indicates the high biological productivity.The ratios of V/(V+Ni),V/Cr and Sr/Ba take a indicator for organic matter preservation.The geochemistry of trace element is consistent with organic matters abundance,sedimentary facies,transgression and regression cycle,organic matter preservation,and organism flourishing.Therefore,the geochemistry of trace element is a potential parameter for distinguishing sedimentary facies.

Key words: Permian, Trace elements, Control factors, Source rock, Sedimentary environment, Geochemical characteristics, Western Sichuan area

中图分类号: 

  • TE122.1

[1]Zhai Guangming.Petroleum Geology of China(vol.10):Sichuan Area[M].Beijing:Petroleum Industry Press,1989.
[翟光明.中国石油地质志(卷十):四川油气区[M].北京:石油工业出版社,1989.]
[2]Wei Guoqi,Liu Delai,Zhang Lin,et al.The exploration region and natural gas accmulation in Sichuan basin[J].Natural Gas Geoscience,2005,16(4):437-442.[魏国齐,刘德来,张林,等.四川盆地天然气分布规律与有利勘探领域[J].天然气地球科学,2005,16(4):437-442.]
[3]Wei Guoqi,Yang Wei,Zhu Yonggang,et al.Depositional system of the middle Permian Qixia Formation in the western Sichuan basin[J].Oil & Gas Geology,2010,31(4):442-448.[魏国齐,杨威,朱永刚,等.川西地区中二叠统栖霞组沉积体系[J].石油与天然气地质,2010,31(4):442-448.]
[4]Dai Shaowu,He Ziai,Wang Jinyi.Thinking of Meso-Paleozoic hydrocarbon exploration in south China[J].Oil & Gas Geology,2001,22(3):195-202.[戴少武,贺自爱,王津义.中国南方中、古生界油气勘探的思路[J].石油与天然气地质,2001,22(3):195-202.]
[5]Tian Haiqin,Wo Yujin,Zheng Lei,et al.Target of Meso-Paleozoic hydrocarbon exploration in Jiangsu-Anhui lower Yangtze region in south China[J].Southern China Oil & Gas,2002,15(3):236-243.[田海芹,沃玉进,郑磊,等.中国南方中、古生界油气勘探方向之思考——近源深埋逆断带可能是今后中国南方中、古生界油气勘探的主战场[J].南方油气,2002,15(3):236-243.]
[6]Ma Li,Chen Huanjiang,Gan Kewen,et al.Geostructure and Marine Facies Hydrocarbon Geology of South China(volume one)[M].Beijing:Geological Publishing House,2004:502-567.[马力,陈焕疆,甘克文,等.中国南方大地构造和海相油气地质(卷一)[M].北京:地质出版社,2004:502-567.]
[7]Zhang Yonggang,Ma Zongjin,Wang Guoli,et al.Hydrocarbon reservoir mode of marine sedimentary rock in south China[J].Acta Geologica Sinica,2007,81(2):236-243.[张永刚,马宗晋,王国力,等.中国南方海相油气成藏模式分析[J].地质学报,2007,81(2):236-243.]
[8]Feng Zengzhao,Yang Yuqing,Jin Zhenkui,et al.Lithofacies Palaeo-Geography of Permian in South China[M].Beijing:The Press of the University of Petroleum,China,1997:1-242.[冯增昭,杨玉卿,金振奎,等.中国南方二叠纪岩相古地理[M].北京:石油大学出版社,1997:1-242.]
[9]Hu Shuyi,Tian Haiqin.A comprehensive study on petroleum geologic conditions in Permian,Yangtze area[J].Geoscience,1999,13(2):162-168.[胡书毅,田海芹.扬子地区二叠系油气地质条件综合研究[J].现代地质,1999,13(2):162-168.]
[10]Yan Jiaxin,Zhao Kun.Permo-Triassic paleogeographic,paleoclimatic and paleoceanographic evolutions in eastern Tethys and their coupling[J].Science in China:Series D,2002,32(9):751-759.[颜佳新,赵坤.二叠—三叠纪东特提斯地区古地理、古气候和古海洋演化与地球表层多圈层事件藕合[J].中国科学:D辑,2002,32(9):751-759.]
[11]Tenger,Qin Jianzhong,Zheng Lunju.Spatiotemporal distribution of Sinian-Permian excellent marine source rocks in southeastern Guizhou province[J].Marine Origin Petroleum Geology,2008,13(2):37-44.[腾格尔,秦建中,郑伦举.黔东南地区震旦系—二叠系海相优质烃源层的时空分布[J].海相油气地质,2008,13(2):37-44.]
[12]Xiao Kaihua,Wo Yujin,Zhou Yan,et al.Petroleum reservoiring characteristics and exploration direction in marine strata in southern China[J].Oil & Gas Geology,2006,27(3):316-325.[肖开华,沃玉进,周雁,等.中国南方海相层系油气成藏特点与勘探方向[J].石油与天然气地质,2006,27(3):316-325.]
[13]Li Shuangjian,Xiao Kaihua,Wo Yujin,et al.Palaeo-environment restoration of upper Ordovician-lower Silurian hydrocarbon source rock in middle-upper Yangtze area[J].Acta Petrologica et Mineralogica,2009,28(5):450-458.[李双建,肖开华,沃玉进,等.中上扬子地区奥陶统—下志留统烃源岩发育的古环境恢复[J].岩石矿物学杂志,2009,28(5):450-458.]
[14]
[KG*4/5]Li Shuangjian,Xiao Kaihua,Wo Yujin,et al.Developmental controlling factors of upper Ordovician-lower Silurian high quality source rocks in marine sequence,south China[J].Acta Sedimentolgica Sinica,2008,26(5):872-880.[李双建,肖开华,沃玉进,等.南方海相上奥陶统—下志留统优质烃源岩发育的控制因素[J].沉积学报,2008,26(5):872-880.]
[15]Zhao Zongju,Zhu Yan,Xu Yunjun.Formation rules and prediction of exploration targets of Paleozoic-Mesozoic oil-gas reservoirs in southern China[J].Acta Geologica Sinica,2004,78(5):710-720.[赵宗举,朱琰,徐云俊.中国南方古生界—中生界油气藏成藏规律及勘探方向[J].地质学报,2004,78(5):710-720.]
[16]Peng Haiyan,Chen Hongde,Xiang Fang,et al.Application of trace elements analysis on sedimentary environment identification[J].Xinjiang Geology,2006,24(2):202-205.[彭海艳,陈洪德,向芳,等.微量元素分析在沉积环境识别中的应用[J].新疆地质,2006,24(2):202-205.]
[17]Li Hongjing,Xie Xinong,Lin Zhengliang,et al.Organic matter enrichment of Dalong Formation in Guangyuan area of the Sichuan basin[J].Geological Science and Technology Information,2009,28(2):98-103.[李红敬,解习农,林正良,等.四川盆地广元地区大隆组有机质富集规律研究[J].地质科技情报,2009,28(2):98-103.]
[18]Li Hongjing,Xie Xinong,Yan Jiaxin,et al.Geochemical characteristics of different facies of Permian typical sections in the Yangtze region[J].Geological Science and Technology Information,2010,29(2):16-23.[李红敬,解习农,颜佳新,等.扬子地区典型剖面二叠系不同沉积相地球化学特征[J].地质科技情报,2010,29(2):16-23.]
[19]Miao Yao,Sang Shuxun,Lin Huixi,et al.Trace element signatures of the Carboniferous-Permian deposits in the Bohai Gulf basin and their facies significance[J].Sedimentary Geology and Tethyan Geology,2007,27(4):27-32.[苗耀,桑树勋,林会喜,等.渤海湾盆地石炭系—二叠系微量元素特征及其指相意义[J].沉积与特提斯地质,2007,27(4):27-32.]
[20]Tenger,Liu Wenhui,Xu Yongchang,et al.The discussion anoxic environments and its geochemical identifying indices[J].Acta Sedimentologica Sinica,2004,22(2):365-372.[腾格尔,刘文汇,徐永昌,等.缺氧环境及地球化学判识标志的探讨——以鄂尔多斯盆地为例[J].沉积学报,2004,22(2):365-372.]
[21]Chen Yanjing,Deng Jian,Hu Guixing.The control over of the environments on content and distribution types of trace element in sediments[J].Geology Geochemistry,1996,(3):97-105.[陈衍景,邓健,胡桂兴.环境对沉积物微量元素含量和分配型式的制约[J].地质地球化学,1996,(3):97-105.]
[22]Miao Jianyu,Zhou Lifa,Zhang Hongfu,et al.The relationship between the geochemical characteristics and sedimentary environments of the middle Permian hydrocarbon source rocks in northern Xinjiang China[J].Acta Geologica Sinica,2004,78(4):534-541.[苗建宇,周立发,张宏福,等.新疆北部中二叠统烃源岩地球化学特征与沉积环境[J].地质学报,2004,78(4):534-541.]
[23]Chen Jianfa,Tang Youjun,Xu Liheng,et al.Comparison of geochemical characteristics of Carboniferous and Permian-Triassic natural gas in northeast Sichuan[J].Natural Gas Geoscience,2008,19(6):741-747.[陈践发,唐友军,徐立恒,等.川东北地区石炭系与二叠系—三叠系天然气地球化学特征对比研究[J].天然气地球科学,2008,19(6):741-747.]
[24]Liu Quanyou,Jin Zhijun,Gao Bo,et al.Characterization of gas pyrolysates from different types of Permian source rocks in Sichuan basin[J].Natural Gas Geoscience,2010,21(5):700-704.[刘全有,金之钧,高波,等.四川盆地二叠系不同类型烃源岩生烃热模拟实验[J].天然气地球科学,2010,21(5):700-704.]
[25]Yao Weijiang,Dang Yufang,Zhang Shuncun,et al.Formation of Carboniferous reservoir in Hongche fault belt,northwestern margin of Junggar basin[J].Natural Gas Geoscience,2010,12(6):917-923.[姚卫江,党玉芳,张顺存,等.准噶尔盆地西北缘红车断裂带石炭系成藏控制因素浅析[J].天然气地球科学,2010,12(6):917-923.]
[26]Li Shuangjian,Xiao Kaihua,Wo Yujin,et al.REE geochemical characteristics and their geological signification in Silurian,west of Hunan province and north of Guizhou province[J].Geoscience,2008,22(2):273-280.[李双建,肖开华,沃玉进,等.湘西、黔北地区志留系稀土元素地球化学特征及其地质意义[J].现代地质,2008,22(2):273-280.]
[27]Lu Hongbo,Jiang Zaixing.Application of geochemical analysis of rare earth elements in the study of lithofacies paleogeography[J].Journal of the University of Petroleum,China,1999,23(1):6-8.[鲁洪波,姜在兴.稀土元素地球化学分析在岩相古地理研究中的应用[J].石油大学学报:自然科学版,1999,23(1):6-8.]
[28]Yang Haisheng,Zhou Yongzhang,Yang Zhijun,et al.REE geochemical characteristics of hydrothermal cherts from south China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2003,22(1):61-64.[杨海生,周永章,杨志军,等.华南热水成因硅质岩建造的稀土元素地球化学特征[J].矿物岩石地球化学通报,2003,22(1):61-64.]
[29]Liu Ning,Fan Dehua,Hao Yunqing,et al.Ree analysis method and application[J].Petroleum Geology & Experiment,2009,31(4):427-432.[刘宁,樊德华,郝运轻,等.稀土元素分析方法研究及应用[J].石油实验地质,2009,31(4):427-432.]
[30]Wright J,Holscr W T.Paleoredox variationsin ancient ocenans recorded by rare earth elements in fossil apatite[J].Geochimica et Cosmochimica Acta,1987,51:631-644.
[31]Wignall P B,Maynard J R.The sequence stratigraphy of transgressive black shales[C]∥Katz B J,Pratt L M,eds.Source Rocks in ASequence Stratigraphic Framework.AAPG Study in Geology 37,1993:35-47.
[32]Hatch J R,Leventhal J S.Relationship between inferred redox potential of the depositional environment and geochemistry of the upper Pennsylvanian stark shale member of Dennis limestone,Wabaunsee county,Kansas.U.S.A[J].Chemical Geology,1992,99:65-82.
[33]Freudenthal T,Wagner T,Wenzhfer F,et al.Early diagenesis of organic matter from sediments of the eastern subtropical Atlantic:Evidence from stable nitrogen and carbon isotopes[J].Geochimica et Cosmochimica Acta,2001,65(11):1795-1808.
[34]Dymond J,Collier R,McManus J,et al.Can the aluminum and titanium contents of ocean sediments be used to determine the paleoproductivity of the ocean[J].Paleoceanography,1997,12(4):586-593.
[35]Breit G N,Wanty R B.Vanadium accumulation in Carbonaceous rocks:A review of geochemical controls during deposition and diagenesis[J].Chemical Geology,1991,91:83-97.
[36]Tribovillard N,Algeo T J,Lyons T,et al.Trace metals as paleoredox and paleoproductivity proxies:An update[J].Chemical Geology,2006,232:12-32.

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