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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(1): 52-57
Liu Guangxiang, Luo Kaiping, Peng Jinning, Deng Mo, Guan Honglin. CAUSES AND SIGNIFICANCE OF ABNORMAL THERMAL EVOLUTION OF ORGANIC MATTERS IN CHANGYANG AREA, HUBEI PROVINCE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(1): 52-57. doi: 10.11781/sysydz201001052
Citation: Liu Guangxiang, Luo Kaiping, Peng Jinning, Deng Mo, Guan Honglin. CAUSES AND SIGNIFICANCE OF ABNORMAL THERMAL EVOLUTION OF ORGANIC MATTERS IN CHANGYANG AREA, HUBEI PROVINCE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(1): 52-57. doi: 10.11781/sysydz201001052
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CAUSES AND SIGNIFICANCE OF ABNORMAL THERMAL EVOLUTION OF ORGANIC MATTERS IN CHANGYANG AREA, HUBEI PROVINCE

doi: 10.11781/sysydz201001052
  • 1.

    School of Energy Resources, China University of Geosciences, Beijing 100083, China

  • 2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

  • Received Date: 2009-08-26
  • Rev Recd Date: 2009-12-08
  • Publish Date: 2010-02-28
    Abstract
  • Studies of vitrinite reflectance and illite crystallinity from Upper Sinian to Lower Triassic in Chang-yang area of Hubei Province have indicated that,there are 2 abnormal zones of equivalent vitrinite reflectance and illite crystallinity between Permian-top of Silurian and bottom of Silurian-top of Lower Cambrian.The upper abnormal zone is formed by thermal effects of advection hot liquid flowing along D2y,S3sh sandstone reservoir as well as D2y/S3sh,C1y/D unconformity surface.The lower abnormal zone is formed by thermal convection of hot liquid in-C1s-O reservoir.Hydrocarbon generation in P and O3w-S1ln should stop at the end of Middle Triassic;however,due to thermal effect of hot liquid during the Yanshanian stage,it continues to the end of Jurassic,hence favorable for petroleum accumulation.

     

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    • References(23)
  • [1]
    张厚福,方朝亮,张枝焕,等.石油地质学[M].北京:石油工业出版社,1999:193-199.
    [2]
    陆克政.含油气盆地分析[M].东营:中国石油大学出版社,2006:320-348.
    [3]
    秦建中,饶丹,蒋宏.高演化海相碳酸盐岩层系古温标的直接指标:包裹体均一温度[J].石油实验地质,2008,30(5):494-498.
    [4]
    周成礼,冯石,王世成,等.磷灰石裂变径迹长度分布数值模拟及地质应用[J].石油实验地质,1994,16(4):409-416.
    [5]
    秦建中,腾格尔,杨琦,等.川东地区海相高演化层系的成熟度指标研究[J].石油学报,2009,30(2):208-213.
    [6]
    王宝清.川西-川西北地区上三叠统碎屑储集岩成岩作用[J].石油实验地质,2008,30(1):69-74.
    [7]
    王玮,周祖翼.镜质体反射率剖面反演中的不确定性分析:以鄂西渝东茶园1井为例[J].石油实验地质,2008,30(3):292-296.
    [8]
    程克明,王兆云,钟宁宁,等.碳酸盐岩油气生成理论与实践[M].北京:石油工业出版社,1996:176-197.
    [9]
    程克明,王兆云,熊英.中国海相碳酸盐岩的生烃研究[J].海相油气地质,1999,4(4):1-11.
    [10]
    郝石生,高岗,王飞宇,等.高过成熟海相烃源岩[M].北京:石油工业出版社,1996:72-84.
    [11]
    戴鸿鸣,王顺玉,陈义才.油气地球化学勘探[M].北京:石油工业出版社,2000:198-208.
    [12]
    KISCH H J.Dlite crystallinity:Recommenadtions on sample preprartion,X-ray diffraction setting,and interlaboratory samples[J].Journal of Metamorphic Geology,1991,9(6):665-670.
    [13]
    丰国秀,陈盛吉.岩石中沥青反射率与镜质体反射率之间的关系[J].天然气工业,1988,8(2):20-25.
    [14]
    毕先梅,莫宣学.成岩-极低级变质-低级变质作用及有关矿产[J].地学前缘,2004,11(1):287-294.
    [15]
    曹学伟,胡文瑄,金之钧,等.临盘油田夏38井区辉绿岩热效应对成烃作用的影响[J].石油与天然气地质,2005,26(3):317-322.
    [16]
    孙永革,傅家谟,刘德汉,等.火山活动对沉积有机质演化的影响及其油气地质意义[J].科学通报,1995,40(11):1019-1022.
    [17]
    钟建华.剪切作用对有机质光学各向异性体发育的控制[J].地质力学学报,1997,3(3):39-40.
    [18]
    董亨茂,张生根,胡远清.断层作用热模型及其对烃源岩热演化的影响[J].地质力学学报,2006,12(4):445-453.
    [19]
    胡善亭,杨起,潘治贵,等.鸡西煤田煤的热液变质作用[J].煤炭学报,1996,21(4):343-347.
    [20]
    郝芳,孙永传,李思田,等.活动热流体对有机质热演化和油气生成作用的强化[J].地球科学:中国地质大学学报,1996,21(1):68-72.
    [21]
    袁玉松,朱传庆,胡圣标.江汉盆地热流史、沉积构造演化与热事件[J].地球物理学进展,2007,22(3):934-939.
    [22]
    薄冬梅,姜林,唐艳军,等.热流体活动与油气成藏[J].西南石油大学学报,2007,29(5):38-41.
    [23]
    叶加仁,杨香华.沉积盆地热流体活动及其成藏动力学意义[J].沉积学报,2001,19(2):214-218.
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