Advanced Search
Volume 40 Issue 5
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2018  >  40(5): 605-612
PENG Jinning, LUO Kaiping, LIU Guangxiang, YANG Fan, YANG Jun, PAN Wenlei. Causes of abnormal thermal evolution and characteristics of thermal evolution in Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(5): 605-612. doi: 10.11781/sysydz201805605
Citation: PENG Jinning, LUO Kaiping, LIU Guangxiang, YANG Fan, YANG Jun, PAN Wenlei. Causes of abnormal thermal evolution and characteristics of thermal evolution in Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(5): 605-612. doi: 10.11781/sysydz201805605
shu

Causes of abnormal thermal evolution and characteristics of thermal evolution in Sichuan Basin

doi: 10.11781/sysydz201805605

  • Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • Received Date: 2017-09-30
  • Rev Recd Date: 2018-08-10
  • Publish Date: 2018-09-28
    Abstract
  • The causes of thermal evolution anomalies in the Sichuan Basin, and the distribution of thermal fields and their main controlling factors during different geohistory periods were analyzed. The Ro-H thermal evolution profiles of typical wells and outcrops in various tectonic units in the Sichuan Basin were established to discuss the causes of vertical thermal evolution anomalies. The thermal field distributions in the Sichuan Basin from the Late Paleozoic to the Middle Triassic, the Late Triassic to the Jurassic, and at present, respectively, were obtained by a Ro gradient method, and a thermal history analysis was carried out. Some conclusions were made as follows. (1) Hydrogen generation from source rocks produced overpressure, leading to the differential inhibition of Ro and hydrocarbon cracking, which was the main cause of the "negative" anomaly of longitudinal organic matter thermal evolution in the Sichuan Basin. (2) The tectonic movements and basin properties in different periods controlled the vertical thermal evolution in the basin. At the end of middle Permian, regional extension changed the former unified low-heat field, resulting in increasing heat flow value in the fault depression, with an average geothermal gradient above 3.5℃/hm. From the Late Yanshanian to the Early Himalayan periods, the east part of the basin began to uplift, and the basin gradually shrank to the west. The peripheral thrusting action tended to decrease, and the high thermal field began to cool. The rapid uplifting and cooling effects at the end of Himalayan period formed the current low-heat field, with a geothermal gradient less than 2.5℃/hm.

     

    • FullText(HTML)
  • loading
    • References(44)
  • [1]
    胡圣标,汪集旸.沉积盆地热体制研究的基本原理和进展[J].地学前缘,1995,2(3/4):171-180.

    HU Shengbiao,WANG Jiyang.Principles and progresses on thermal regime of sedimentary basins:an overview[J].Earth Science Frontiers,1995,2(3/4):171-180.
    [2]
    袁魏,方石,孙求实,等.沉积盆地热史研究综述[J].当代化工,2014,43(5):728-731.

    YUAN Wei,FANG Shi,SUN Qiushi,et al.Research on thermal history of sedimentary basins[J].Contemporary Chemical Industry,2014,43(5):728-731.
    [3]
    何丽娟.沉积盆地构造热演化模拟的研究进展[J].地球科学进展,2000,15(6):661-665.

    HE Lijuan.Advance in tectono-thermal modeling of sedimentary basins[J].Advance in Earth Sciences,2000,15(6):661-665.
    [4]
    邱楠生,胡圣标,何丽娟.沉积盆地热体制研究的理论与应用[M].北京:石油工业出版社,2004:38-56. QIU Nansheng,HU Shengbiao,HE Lijuan.Theory and application of geothermal system in sedimentary basins[M].Beijing:Petroleum Industry Press,2004:38-56.
    [5]
    任战利.沉积盆地热演化史研究新进展[J].地球科学进展,1992,7(3):43-49.

    REN Zhanli.Advances on thermal histories of sedimentary basins[J].Advance in Earth Sciences,1992,7(3):43-49.
    [6]
    王璞珺,刘万洙,王东坡.沉积盆地热史研究方法[J].世界地质,1994,13(3):114-119.

    WANG Pujun,LIU Wanzhu,WANG Dongpo.Research method of thermal history of sedimentary basin[J].World Geology,1994,13(3):114-119.
    [7]
    陈刚,赵重远,李丕龙,等.Ro反演的盆地热史恢复方法与相关问题[J].石油与天然气地质,2002,23(4):343-347.

    CHENG Gang,ZHAO Zhongyuan,LI Pilong,et al.Ro inversion of thermal history reconstruction in sedimentary basin and its related problems[J].Oil & Gas Geology,2002,23(4):343-347.
    [8]
    郭随平,王良书,施央申,等.应用磷灰石裂变径迹研究沉积盆地的热史[J].南京大学学报,1995,31(3):469-475.

    GUO Suiping,WANG Liangshu,SHI Yangshen,et al.Application of apatite fission track to study the thermal history of sedimentary basin[J].Journal of Nanjing University,1995,31(3):469-475.
    [9]
    刘进.流体包裹体在盆地热史研究中的应用与问题讨论[J].河南石油,2006,20(4):13-14.

    LIU Jin.Application and discussion on problems of fluid inclusion study in thermal history of the basin[J].Henan Petroleum,2006,20(4):13-14.
    [10]
    胡圣标,何丽娟,朱传庆,等.海相盆地热史恢复方法体系[J].石油与天然气地质,2008,29(5):607-613.

    HU Shengbiao,HE Lijuan,ZHU Chuanqing,et al.Method system of thermal reconstruction for marine basins[J].Oil & Gas Geology,2008,29(5):607-613.
    [11]
    KETCHAM R A,DONELICK R A,CARLSON W D.Variability of apatite fission-track annealing kinetics:Ⅲ.extrapolation to geological time scales[J].American Mineralogist,1999,84:l235-1255.
    [12]
    BUCHARDT B,LEWAN M D.Reflectance of vitrinite-like mace-rals as a thermal maturity index for Cambrian-Ordovician Alum shale,southern Scandinavia[J].AAPG Bulletin,1990,74(4):394-406.
    [13]
    JARVIS G T,MCKENZIE D P.Sedimentary basin formation with finite extension rates[J].Earth and Planetary Science Letters,1980,48(1):42-52.
    [14]
    王钧,黄尚瑶,黄歌山,等.中国地温分布的基本特征[M].北京:地震出版社,1990:130-142. WANG Jun,HUANG Shangyao,HUANG Geshan,et al.The basic characteristics of geothermal field in China[M].Beijing:Seismological Press,1990:130-142.
    [15]
    李皎,何登发,梅庆华.四川盆地及邻区奥陶纪构造-沉积环境与原型盆地演化[J].石油学报,2015,36(4):427-445.

    LI Jiao,HE Dengfa,MEI Qinghua.Tectonic-depositional environment and proto-type basins evolution of the Ordovician in Sichuan Basin and adjacent areas[J].Acta Petrolei Sinica,2015,36(4):427-445.
    [16]
    何登发,李德生,张国伟,等.四川多旋回叠合盆地的形成与演化[J].地质科学,2011,46(3):589-606.

    HE Dengfa,LI Desheng,ZHANG Guowei,et al.Formation and evolution of multi-cycle superposed Sichuan Basin,China[J].Chinese Journal of Geology,2011,46(3):589-606.
    [17]
    汪泽成,赵文智,张林.四川盆地构造层序与天然气勘探[M].北京:地质出版社,2002:59-68. WANG Zecheng,ZHAO Wenzhi,ZHANG Lin.Tectonic sequence and gas exploration in Sichuan Basin[M].Beijing:Geological Publishing House,2002:59-68.
    [18]
    郭正吾,邓康龄,韩永辉.四川盆地形成与演化[M].北京:地质出版社,1996:48-138. GUO Zhengwu,DENG Kangling,HAN Yonghui.The formation and development of Sichuan Basin[M].Beijing:Geological Publishing House,1996:48-138.
    [19]
    吴群,彭金宁.川东北地区埋藏史及热史分析:以普光2井为例[J].石油实验地质,2013,35(2):133-138.

    WU Qun,PENG Jinning.Burial and thermal histories of northeastern Sichuan Basin:a case study of well Puguang 2[J].Petroleum Geology & Experiment,2013,35(2):133-138.
    [20]
    王杰,秦建中,刘文汇,等.川东北元坝地区中生代构造与动态热演化史:磷灰石、锆石(U-Th)/He定年分析[J].石油实验地质,2012,34(1):19-24.

    WANG Jie,QIN Jianzhong,LIU Wenhui,et al.Mesozoic tectonics and dynamic thermal history in Yuanba area of northeastern Sichuan Basin:application of(U-Th)/He dating of apatite and zircon[J].Petroleum Geology & Experiment,2012,34(1):19-24.
    [21]
    马德文,邱楠生,许威,等.四川盆地原油裂解气的有利地温场分布及其演化特征[J].地球科学与环境学报,2012,34(2):49-56.

    MA Dewen,QIU Nansheng,XU Wei,et al.Distribution and evolution characteristic of favorable geothermal field for oil cracking gas in Sichuan Basin[J].Journal of Earth Sciences and Environment,2012,34(2):49-56.
    [22]
    卢庆治,胡圣标,郭彤楼,等.川东北地区异常高压形成的地温场背景[J].地球物理学报,2005,48(5):1110-1116.

    LU Qingzhi,HU Shengbiao,GUO Tonglou,et al.The background of the geothermal field for formation of abnormal high pressure in the northeastern Sichuan Basin[J].Chinese Journal of Geophysics,2006,48(5):1110-1116.
    [23]
    沈传波,梅廉夫,郭彤楼.川东北地区中、新生代热历史的裂变径迹分析[J].天然气工业,2007,27(7):24-26.

    SHEN Chuanbo,MEI Lianfu,GUO Tonglou.Fission track analysis of Mesozoic-Cenozoic thermal history in northeast Sichuan Basin[J].Natural Gas Industry,2007,27(7):24-26.
    [24]
    卢庆治,郭彤楼,胡圣标.川东北地区热流史及成烃史研究[J].新疆石油地质,2006,27(5):549-551.

    LU Qingzhi,GUO Tonglou,HU Shengbiao.Hydrothermal history and hydrocarbon generation history in northeastern Sichuan Basin[J].Xinjiang Petroleum Geology,2006,27(5):549-551.
    [25]
    韩永辉,吴春生.四川盆地地温梯度及几个深井的热流值[J].石油与天然气地质,1993,14(1):80-84.

    HAN Yonghui,WU Chunsheng.Geothermal gradient and heat flow values of some deep wells in Sichuan Basin[J].Oil & Gas Geology,1993,14(1):80-84.
    [26]
    曾道富,曾学思.四川盆地古地温及古地温梯度的研究[J].天然气工业,1987,7(4):12-16.

    ZENG Daofu,ZENG Xuesi.A research on paleo-geotherm and paleo-geothermal gradient of Sichuan Basin[J].Natural Gas Industry,1987,7(4):12-16.
    [27]
    伍大茂,吴乃苓,郜建军.四川盆地古地温研究及其地质意义[J].石油学报,1998,19(1):18-23.

    WU Damao,WU Nailing,GAO Jianjun.Paleogeo-temperature in Sichuan Basin and its geological significance[J].Acta Petrolei Sinica,1998,19(1):18-23.
    [28]
    谢晓黎,于汇津.四川盆地区域地温场的特征[J].成都地质学院学报,1988,15(4):107-114.

    XIE Xiaoli,YU Huijin.The characteristics of the regional geothermal field in Sichuan Basin[J].Journal of Chengdu College of Geology,1988,15(4):107-114.
    [29]
    汪集旸,黄少鹏.中国大陆地区大地热流数据汇编(第二版)[J].地震地质,1990,12(4):351-360.

    WANG Jiyang,HUANG Shaopeng.Compilation of heat flow data in the China continental area:2nd edition[J].Seismology and Geology,1990,12(4):351-360.
    [30]
    黄少鹏,汪集旸.四川盆地川西北拗陷几个深孔热流测试[J].科学通报,1990(10):773-776. HUANG Shaopeng,WANG Jiyang.Several heat flow values from deep drill holes in the Northwest Depression of the Sichuan Basin, SW China[J].Chinese Science Bulletin,1990(1):47-51.
    [31]
    徐明,朱传庆,田云涛,等.四川盆地钻孔温度测量及现今地热特征[J].地球物理学报,2011,54(4):1052-1060.

    XU Ming,ZHU Chuanqing,TIAN Yuntao,et al.Borehole temperature logging and characteristics of subsurface temperature in the Sichuan Basin[J].Chinese Journal of Geophysics,2011,54(4):1052-1060.
    [32]
    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):292-299.

    WANG Wei,ZHOU Zuyi.Uncertainties in the inversion of vitrinite reflectance profile:a case study of well Chayuan 1,West Hubei and East Chongqing[J].Petroleum Geology and Experiment,2008,30(3):292-299.
    [33]
    王玮,周祖翼,于鹏.镜质体反射率与最高温度及其附近温度变化率的关系:几种镜质体反射率计算模型的比较[J].地球物理学报,2005,48(6):1375-1383.

    WANG Wei,ZHOU Zuyi,YU Peng.Relations between vitrinite reflectance,peak temperature and its neighboring temperature variation rate:a comparison of methods[J].Chinese Journal of Geophysics,2005,48(6):1375-1383.
    [34]
    WOOD D A.Relationships between thermal maturity indices calculated using Arrhenius equation and Lopatin method:implications for petroleum exploration[J].AAPG Bulletin,1988,72(2):115-134.
    [35]
    HAO Fang,SUN Yongchuan,LI Sitian,et al.Overpressure retardation of organic-matter maturation and petroleum generation:a case study from the Yinggehai and Qiongdongnan basins,South China Sea[J].AAPG Bulletin,1995,79(4):551-562.
    [36]
    孙嘉陵.南海崖13-1气田特征及富集成藏条件[J].天然气工业,1994,14(2):1-7.

    SUN Jialing.The characteristics of Nanhaiya 13-1 gas field and its enrichment pool-formed conditions[J].Natural Gas Industry,1994,14(2):1-7.
    [37]
    CARR A D.A vitrinite reflectance kinetic model incorporating overpressure retardation[J].Marine and Petroleum Geology,1999,16(4):355-377.
    [38]
    郝芳,姜建群,邹华耀,等.超压对有机质热演化的差异抑制作用及层次[J].中国科学(D辑地球科学),2004,34(5):443-451. HAO Fang,JIANG Jianqun,ZOU Huayao,et al.Differential retardation of organic matter maturation by overpressure[J].Science in China (Ser. D Earth Sciences),2004,47(9):783-793.
    [39]
    马启富,陈斯忠,张启明,等.超压盆地与油气分布[M].北京:地质出版社,2000:5-17. MA Qifu,CHEN Sizhong,ZHANG Qiming,et al.Overpressure basin and oil and gas distribution[M].Beijing:Geological Publishing Hous,2000:5-17.
    [40]
    高喜龙,肖贤明,刘中云,等.用开放体系的热解方法对烃源岩生烃动力学的研究:以东营凹陷某生油岩为例[J].地球化学,2003,32(5):485-490.

    GAO Xilong,XIAO Xianming,LIU Zhongyun,et al.Hydrocarbon generation kinetics of source rocks in open system based on pyrolysis simulation experiment:a case study of the Dongying Depression[J].Geochimica,2003,32(5):485-490.
    [41]
    BARKER C E.Implications for organic maturation studies of evidence for a geologically rapid increase and stabilization of vitrinite reflectance at peak temperature:Cerro Prieto geothermal system,Mexico[J].AAPG Bulletin,1991,75(12):1852-1863.
    [42]
    袁玉松,马永生,胡圣标,等.中国南方现今地热特征[J].地球物理学报,2006,49(4):1118-1126.

    YUAN Yusong,MA Yongsheng,HU Shengbiao,et al.Present-day geothermal characteristics in South China[J].Chinese Journal of Geophysics,2006,49(4):1118-1126.
    [43]
    冯昌格,刘绍文,王良书,等.塔里木盆地现今地热特征[J].地球物理学报,2009,52(11):2752-2762.

    FENG Changge,LIU Shaowen,WANG Liangshu,et al.Present-day geothermal regime in Tarim Basin,Northwest China[J].Chinese Journal of Geophysics,2009,52(11):2752-2762.
    [44]
    王良书,李成,施央申.塔里木盆地大地热流密度分布特征[J].地球物理学报,1995,38(6):855-856.

    WANG Liangshu,LI Cheng,SHI Yangshen.Distribution of terrestrial heat flow density in Tarim Basin,Western China[J].Acta Geophysica Sinica,1995,38(6):855-856.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

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 (1148) PDF downloads(407) 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