Advanced Search
Volume 30 Issue 6
. 
Turn off MathJax
Article Contents
Abstract
References
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2008  >  30(6): 591-595
Zhang Linye. THE PROGRESS ON THE STUDY OF LACUSTRINE SOURCE ROCKS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(6): 591-595. doi: 10.11781/sysydz200806591
Citation: Zhang Linye. THE PROGRESS ON THE STUDY OF LACUSTRINE SOURCE ROCKS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(6): 591-595. doi: 10.11781/sysydz200806591
shu

THE PROGRESS ON THE STUDY OF LACUSTRINE SOURCE ROCKS

doi: 10.11781/sysydz200806591

  • Geological Scientific Research Institute, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China

  • Received Date: 2008-07-01
  • Rev Recd Date: 2008-11-01
  • Publish Date: 2008-12-28
    Abstract
  • There is distinctive heterogeneity in the deposition of lacustrine source rocks.The occurrence of high-quality lacustrine source rocks with rich-organic matter plays an important role in controlling the formation of large oil fields.It has been widely concerned about the mechanism forming rich-organic matter in lacustrine source rock and has achieved significant advance.The deposition of high-quality source rocks has close relationships with the variation of the capacities of lacustrine basins during their evolution,paleolacustrine physicochemical properties,nutrition origin of paleo-productivity,periodic variation of climate and so on.In order to study the formation mechanism of high-quality source rocks,we should try to find out the dependence relations between organic compounds and inorganic elements in sedimentary rhythms in rich-organic matter strata,analyse the coupling relation between cyclicity and incident during geologic succession,inquire into the inherent connection among geologic environment,biogenetic derivation and the formation of rich-organic matter strata.

     

    • FullText(HTML)
    • References(57)
  • [1]
    尚慧芸.我国陆相生油层地球化学指标的探讨[A].见:石油勘探研究报告集(第二辑)[M].北京:中国工业出版社,1963
    [2]
    黄第藩,陈克造.青海湖第四纪沉积物中沥青的形成与陆相石油成因问题[J].地质学报,1964,44(2):171～190
    [3]
    傅家谟,史继扬.石油演化理论与实践Ⅰ:石油演化的机理与石油演化的阶段[J].地球化学,1975,(2)
    [4]
    汪本善,盛国英,栗能先等.正烷烃在石油地球化学中的应用[J].地球化学,1975,(4):258～272
    [5]
    黄第藩.中国陆相油气生成[M].北京:石油工业出版社,1982
    [6]
    Carroll A R,Bohacs K M.Lake-type controls on petroleum source rock potential in nonmarine basins[J].AAPG Bulletin,2001,85(6):1033～1053
    [7]
    王秉海,钱凯.胜利油区地质研究与勘探实践[M].东营:石油大学出版社,1992
    [8]
    邓宏文,钱凯.沉积地球化学与环境分析[M].兰州:甘肃科学技术出版社,1993
    [9]
    Stein R,Rullkötter J,Welte D H.Accumulation of organic-carbon rich sediments in the late Jurassic and Cretaceous Atlantic Ocean:A synthesis[J].Chem Geol,1986,56(1-2):1～32
    [10]
    杨华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气藏富集中的主导作用:地质地球化学特征[J].地球化学,2005,34(2):147～154
    [11]
    张林晔,孔祥星,张春荣等.济阳坳陷第三系优质烃源岩的发育及其意义[J].地球化学,2003,3(1):35～42
    [12]
    张林晔,张春荣.低熟油生成机理及成油体系:以济阳坳陷牛庄洼陷南部斜坡为例[M].北京:地质出版社,1999
    [13]
    张林晔,刘庆,张春荣等.东营凹陷成烃与成藏关系研究[M].北京:地质出版社,2005
    [14]
    朱光有,金强.东营凹陷两套优质烃源岩层地质地球化学特征研究[J].沉积学报,2003,21(3):506～512
    [15]
    张水昌,张宝民,王飞宇等.塔里木盆地两套海相有效烃源岩:Ⅰ有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261～268
    [16]
    刘华,李凌,吴智平.胶莱盆地烃源岩分布及有机地球化学特征[J].石油实验地质,2006,28(6):574～580
    [17]
    Hunt J M.The generation and migration of petroleum from abnormally pressured fluid compartment[J].AAPG Bull,1990,74(1):1～12
    [18]
    许晓明,刘震,谢启超等.渤海湾盆地济阳坳陷异常高压特征分析[J].石油实验地质,2006,28(4):345～349
    [19]
    秦建中.中国烃源岩[M].北京:科学出版社,2005
    [20]
    Tiercelin J J,Thouin C,Kalala T,et al.Discovery of sublacustrine hydrothgermal activity and associated massive sulfides and hydrocarbons in the north Tanganyika though[J].East Affican Rift Geology,1989,17:1053～1056
    [21]
    Kelts K.湖相烃源岩的沉积环境:绪论[A].见:汪品先,刘传联编.古湖泊论文集[G].北京:海洋出版社,1991.68～77
    [22]
    Talbot M R.湖相生油岩的成因:来自热带非洲湖泊的资料[A].见:汪品先,刘传联编.古湖泊论文集[G].北京:海洋出版社,1991.52～67
    [23]
    刘传联,徐金鲤,汪品先.藻类勃发:湖相油页岩形成的一种重要机制[J].地质论评,2001,47(2):207～210
    [24]
    王慧中,梅洪明.东营凹陷沙三下亚段油页岩中古湖泊学信息[J].同济大学学报,1998,26(3):315～318
    [25]
    姚益民,徐道一,李保利等.东营凹陷牛38井沙三段高分别率旋回地层研究[J].地层学杂志,2007,31(3):229～238
    [26]
    梁狄刚,张水昌,张宝民等.从塔里木盆地看中国海相生油问题[J].地学前缘,2000,7(4):534～537
    [27]
    秦建中.青藏高原羌塘盆地有机相展布与成烃模式[J].石油实验地质,2006,28(3):264～270
    [28]
    张林晔.富集有机质成烃作用再认识:以东营凹陷为例[J].地球化学,2005,34(6):619～625
    [29]
    孟庆强,马亮帮,邹安德等.不同藻类热模拟实验的生烃特征对比[J].石油实验地质,2008,30(3):281～285
    [30]
    刘传联,徐金鲤.生油古湖泊生产力的估算方法及应用实例[J].沉积学报,2002,20(1):144～150
    [31]
    Hobbie J E.Use of nuclepore filters for counting bacteria by fluresence microscopy[J].Appl Environ Microbial,1977,33:1225～1228
    [32]
    Fuhman J A.Bacteriop lankton secondary production estimates for coastal waters of British Columbia and California[J].Appl Environ Microbial,1980,39(6):1085～1095
    [33]
    Murphy L S,Hangen E M.The distribution and abundance of phototrophic ultrapankton in the North Atlantic[J].Limnol Oceanogr,1985,30:47～58
    [34]
    王广利,张林晔,王铁冠.3β-烷基甾烷在中国古近系陆相沉积中的发现及其地质意义[J].科学通报,2006,51(2):1438～1442
    [35]
    王广利,王铁冠,张林晔等.2-甲基藿烷:陆相湖盆中古沉积环境的分子化石[J].地质学报,2006,80(6):902～909
    [36]
    贾国东,彭平安.有机生物地球化学与晚新生代古全球变化研究[J].地学前缘,2005,12(2):179～187
    [37]
    莫晓勇,孙永革.沉积有机质分子地球化学应用于古气候古环境研究[J].地球与环境,2005,33(2):85～90
    [38]
    Föllmi K B.The phosphorus cycle phosphogenesis and marine phosphate rich deposits[J].Earth Science Reviews,1996,40:55～124
    [39]
    Van Beek P,Reyss J L,Bontep,et al.Sr/Ba ratio in the Barite:Aproxy of barite preservation in marine sediments[J].Marine Geology,2003,199:205～220
    [40]
    L Yons T W,Werne J P,Hollander,et al.Contrasting sulfur geochemistry and Fe/Al and Mo/Al ratios across the last oxic-to-anoxic transition in the Cariaco Basin,Venezuela[J].Ghemical Geology,2003,195:131～157
    [41]
    Stoll H M,Schrag D P.Sr/Ca Variations in Cretaceous carbonates:relation to productivity and sea level change[J].Paleogeography Paleoclimatology,Paleoeology,2001,168:311～336
    [42]
    Meyers P A,Lallier-vergēs E.Lacustrine sedimentary organic matter records of Late Quaternary Paleoclimates[J].Journal of Paleolimnology,1999,21:345～372
    [43]
    Halbach M,Koschinsky A,Halbach P.Reporton the discovery of Gallionella ferruginea from an active hydrothermal field in the deep sea[J].International Ridge-Crest Reseach,2001,10(1):18～20
    [44]
    Lein A Y,Gal'Chenko V F,Pimenov N V,et al.Role of bacterial chemosynthesis and methanotrophy in ocean biogeochemistry[J],geochemistry International,1993,30(9):87～104
    [45]
    金强,熊寿生,卢培德.中国断陷盆地主要生油岩中的火山活动及其意义[J].地质论评,1998,44(2):135～142[G].
    [46]
    张文正,杨华,杨奕华等.鄂尔多斯盆地长7湖相优质烃源岩的发育机制[A].见:第十一届全国有机地球化学学术会议论文摘要汇编[G].昆明:会议组委会,2007.104～105
    [47]
    陈践发,张水昌,孙省利等.海相碳酸盐岩优质烃源岩发育的主要影响因素[J].地质学报,2006,80(3):467～472.
    [48]
    石军柱,刘海涛,石娜.海相火山岩高温有助于有机物质的富集[A].见:第十一届全国有机地球化学学术会议论文昆明:会议组委会,2007.56～57
    [49]
    Tissot B P,Welte D H.Petroleum Formation and Occurrence:A New Approach to oil and Gas Exploration[M].Berlin:Springer-Verlag,1978.55～63
    [50]
    Katz B J.Controls on distribution of lacustrine source rocks through time and space[A].In:Katz B J,ed.Lacustrine Basin Exploration:Case Studies and Modern Analogs,AAPG Memoir 50[M].Tusal:AAPG,1990.61～76
    [51]
    Anderson R V,Dean W E.Lacustrine Varve formation through time[J].palaeogeography,Palaeoclimatology,palaeoecology,1988,62(1-4):215～235
    [52]
    胡春燕,刘立.高频湖相沉积节律研究的新进展[J].世界地质,1998,17(2):14～17
    [53]
    Gradstein F M,Ogg J G,Smith A G,et al.A new geological time scale,with special reference to Precambrian and Neogene[J].Episodes,2004,27(2):83～100
    [54]
    Weedon G.Time-series analysis and cyclostratigraphy:examing stratigraphic records of environmental cycles[M].Cambridge:Cambridge University Press,2003.1～259
    [55]
    张海峰.以米氏旋回为标尺进行高级别层系地层划分与对比:以准噶尔盆地中Ⅰ区块为例[J].油气地质与采收率,2006,13(4):18～20
    [56]
    董春梅.基于河水位变化的层序地层模式:以济阳坳陷孤东油田为例[J].石油实验地质,2006,28(3):249～252
    [57]
    王冠民,钟建华.湖泊纹层的沉积机理研究评述与展望[J].岩石矿物学杂志,2004,23(1):43～48
    • Relative Articles

  • Relative Articles

    [1]ZHI Dongming, LENG Junying, XIE An, TANG Yong, HE Jinyi, HE Wenjun, LI Zhiming, ZOU Yang, ZHU Tao. Characteristics and occurrence states of shale biomarker compounds in Fengcheng Formation, Mahu Sag, Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(5): 954-964. doi: 10.11781/sysydz202405954
    [2]ZHAO Yongqiang, NI Chunhua, WU Xiaoqi, ZHU Jianhui, LIU Guangxiang, WANG Fubin, JIA Huichong, ZHANG Wei, QI Rong, AN Chuan. Geochemical characteristics and source of Permian formation water in Hangjinqi area, Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(2): 279-287. doi: 10.11781/sysydz202202279
    [3]RAN Zichao, LI Meijun, LI Youchuan, SHI Yang, WANG Ning, YANG Yongcai, LU Xiaolin, XIAO Hong. Biomarker compositions and geochemical significance of crude oils of Baiyun Sag, Pearl River Mouth Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(6): 1059-1069. doi: 10.11781/sysydz2022061059
    [4]WANG Linlin, FU Yun, FANG Shijie. Elemental geochemical characteristics and geological significance of Majiagou Formation, eastern Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(4): 519-525. doi: 10.11781/sysydz201804519
    [5]ZHAO Yue, CAI Jingong, XIE Aobo, DONG Zhe, ZHOU Qisheng, LEI Tianzhu, YANG Yan. Geochemical investigation of organic matter of various occurrences released via sequential treatments of two argillaceous source rock samples from fresh and saline lacustrine environments[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(5): 705-715. doi: 10.11781/sysydz201805705
    [6]Liu Qing. Composition and geologic significance of carbon and oxygen isotopes in hydrocarbon source rocks, Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(2): 247-252. doi: 10.11781/sysydz201702247
    [7]Wang Yongwei, Li Rongxi, Gao Shengli, Gao Pengpeng, Li Zemin, Gao Chao, Fu Mingyi. Trace element characteristics and sedimentary environment of lacustrine carbonate rocks in the Huanghua Depression, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(6): 849-857. doi: 10.11781/sysydz201706849
    [8]Diao Fan, Jin Fengming, Hao Fang, Sun Yehua, Zou Huayao, Wang Yuanjie, Zhang Jinfeng, Cao Yijun. Palaeolake environment and organic matter enrichment mechanism of Paleogene Shahejie Formation in Langgu Sag[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 479-486. doi: 10.11781/sysydz201404479
    [9]Song Fan, Yang Shaochun, Su Nina, Xiang Kui, Zhao Yongfu. New understanding of sedimentary facies of Shawan Formation in Chunfeng Oilfield, Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 238-242. doi: 10.11781/sysydz201303238
    [10]Zhang Yunxia, Chen Chunfang, Song Yanbo, Tao Ye, Li Song. Features of Mesozoic source rocks and oil-source correlation in southern Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(2): 173-177. doi: 10.11781/sysydz201202173
    [11]Gao Shengli, Wang lianmin, Wu Xi, Gao Pengpeng. Geochemical characteristics of lacustrine carbonate rocks in lower part of first member of Shahejie Formation in Qijiawu area of Huanghua Depression, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(3): 309-313. doi: 10.11781/sysydz201203309
    [12]Yi Shiwei, Jiang Youlu, Fan Bingda, Xu Haoqing, Zheng Ronghua. NEOGENE PETROLEUM SOURCE AND CHARACTERISTIC OF PALEOGENE HYDROCARBON SOURCE ROCK IN THE RAOYANG SAG, BOHAI BAY BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 475-479. doi: 10.11781/sysydz201005475
    [13]Li Zhongxiong, He Jianglin, Du Baiwei, Wang Zhengjiang. CHARACTERISTICS OF BIOMARKER COMPOUNDS IN THE MIDDLE JURASSIC CARBONATE SEQUENCE OF THE BUQU FORMATION AND THEIR IMPLICATION IN THE QIANGTANG BASIN, THE NORTHERN TIBET[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(2): 175-180. doi: 10.11781/sysydz201002175
    [14]Wang Huitong, Wei Caiyun, Zhang Shuichang, Zhang Dajiang, Wang Hui. THE STUDY ON BIOMARKERS SEPARATION AND ITS CSIA BY MOY MOLECULAR SIEVE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 513-516. doi: 10.11781/sysydz201005513
    [15]Zhang Zhirong, Song Xiaoying, Zhang Qu. GC-MS QUANTITATIVE ANALYSIS OF BIOMARKERS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(4): 405-407. doi: 10.11781/sysydz200804405
    [16]Liu Gang, Zhou Dongsheng. APPLICATION OF MICROELEMENTS ANALYSIS IN IDENTIFYING SEDIMENTARY ENVIRONMENT——TAKING QIANJIANG FORMATION IN THE JIANGHAN BASIN AS AN EXAMPLE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(3): 307-310. doi: 10.11781/sysydz200703307
    [17]Gao Fuhong, Gao Hongmei, Fan Fu. GEOCHEMICAL CHARACTERISTICS OF BIOMARKERS EXTRACTED FROM THE LOWER CRETACEOUS COAL MEASURES ROCKS IN JIXI BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(2): 188-191. doi: 10.11781/sysydz200702188
    [18]JIN Qiang, TIAN Haiqin, DAI Junsheng. APPLICATION OF MICROELEMENT COMPOSITION TO THE CORRELATION OF SOLID BITUMEN WITH SOURCE ROCKS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(3): 285-290. doi: 10.11781/sysydz200103285
    [19]Li Shuangying, Jin Fuquan, Wang Daoxuan. GEOCHEMICAL CHARACTERISTICS OF CARBONATE ROCK DIAGENESIS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 55-62. doi: 10.11781/sysydz199501055
    [20]Tang Feilong. STUDY ON BIOMARKERS IN THE MARINE SEQUENCES OF THE MID-YANGTZ AREA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1994, 16(4): 366-373. doi: 10.11781/sysydz199404366
    • Supplements(0)
    • Cited By
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-072024-082024-092024-102024-112024-122025-012025-022025-032025-042025-052025-06051015202530
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 23.7 %FULLTEXT: 23.7 %META: 71.6 %META: 71.6 %PDF: 4.7 %PDF: 4.7 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 8.3 %其他: 8.3 %其他: 0.7 %其他: 0.7 %China: 0.4 %China: 0.4 %Joliet: 0.4 %Joliet: 0.4 %United Kingdom: 0.6 %United Kingdom: 0.6 %[]: 0.3 %[]: 0.3 %三亚: 1.2 %三亚: 1.2 %上海: 0.8 %上海: 0.8 %东京都: 0.1 %东京都: 0.1 %东莞: 0.4 %东莞: 0.4 %保定: 0.6 %保定: 0.6 %兰州: 0.3 %兰州: 0.3 %北京: 8.9 %北京: 8.9 %十堰: 0.1 %十堰: 0.1 %南京: 0.1 %南京: 0.1 %南昌: 0.1 %南昌: 0.1 %合肥: 0.3 %合肥: 0.3 %嘉兴: 0.3 %嘉兴: 0.3 %天津: 0.7 %天津: 0.7 %安顺: 0.4 %安顺: 0.4 %宣城: 0.7 %宣城: 0.7 %巴音郭楞: 0.1 %巴音郭楞: 0.1 %常州: 0.1 %常州: 0.1 %平顶山: 0.3 %平顶山: 0.3 %延安: 0.1 %延安: 0.1 %张家口: 8.4 %张家口: 8.4 %徐州: 0.1 %徐州: 0.1 %成都: 0.3 %成都: 0.3 %扬州: 0.6 %扬州: 0.6 %无锡: 0.3 %无锡: 0.3 %昆明: 0.1 %昆明: 0.1 %武汉: 1.5 %武汉: 1.5 %汕头: 0.1 %汕头: 0.1 %沈阳: 0.1 %沈阳: 0.1 %济南: 0.3 %济南: 0.3 %海口: 0.8 %海口: 0.8 %淄博: 0.1 %淄博: 0.1 %温州: 0.1 %温州: 0.1 %漯河: 1.1 %漯河: 1.1 %玉林: 0.3 %玉林: 0.3 %盐城: 0.1 %盐城: 0.1 %石家庄: 1.2 %石家庄: 1.2 %芒廷维尤: 39.3 %芒廷维尤: 39.3 %芝加哥: 1.9 %芝加哥: 1.9 %莫斯科: 0.4 %莫斯科: 0.4 %西宁: 10.0 %西宁: 10.0 %西安: 0.3 %西安: 0.3 %贵阳: 0.6 %贵阳: 0.6 %运城: 0.3 %运城: 0.3 %遵义: 0.1 %遵义: 0.1 %郑州: 0.1 %郑州: 0.1 %银川: 0.1 %银川: 0.1 %锦州: 0.1 %锦州: 0.1 %镇江: 0.3 %镇江: 0.3 %长春: 0.4 %长春: 0.4 %长沙: 2.4 %长沙: 2.4 %青岛: 1.2 %青岛: 1.2 %鞍山: 0.1 %鞍山: 0.1 %马鞍山: 0.1 %马鞍山: 0.1 %其他其他ChinaJolietUnited Kingdom[]三亚上海东京都东莞保定兰州北京十堰南京南昌合肥嘉兴天津安顺宣城巴音郭楞常州平顶山延安张家口徐州成都扬州无锡昆明武汉汕头沈阳济南海口淄博温州漯河玉林盐城石家庄芒廷维尤芝加哥莫斯科西宁西安贵阳运城遵义郑州银川锦州镇江长春长沙青岛鞍山马鞍山

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (2831) PDF downloads(1089) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return