Zhao Yongqiang, Zhang Genfa, Wang Bin, Luo Yu, Zhou Yushuang, Lin Xueqing, Chen Xuyun. MaincontrollingfactorsforpetroleumaccumulationinKongqueheslope, TarimBasin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(5): 487-494. doi: 10.11781/sysydz201305487
Citation: Zhao Yongqiang, Zhang Genfa, Wang Bin, Luo Yu, Zhou Yushuang, Lin Xueqing, Chen Xuyun. MaincontrollingfactorsforpetroleumaccumulationinKongqueheslope, TarimBasin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(5): 487-494. doi: 10.11781/sysydz201305487

MaincontrollingfactorsforpetroleumaccumulationinKongqueheslope, TarimBasin

doi: 10.11781/sysydz201305487
  • Publish Date: 2013-09-28
  • Petroleum generation in the Kongquehe slope is closely related with paleostructure during the late Caledonian Movement. Paleostructural background is the key for accumulation. The space -time matching relationship between the peak of hydrocarbon expulsion of source rock and the trap formation works as the main controlling factor. The traps with paleostructural background are favorable exploration targets. The main source rocks from Cambrian and Middle-Lower Ordovician become mature and over-mature during the middle and late Caledonian stage, and do not generate hydrocarbon during the late period. Traps are formed during the late Caledonian and the middle Yanshanian stages. The studies of accumulation stage, exploration practice and conditions of crude oil cracked gas prove that the discovered oil and gas in the Kongquehe slope may be early primary petroleum accumulations.

     

  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-042025-05051015202530
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 18.5 %FULLTEXT: 18.5 %META: 78.0 %META: 78.0 %PDF: 3.4 %PDF: 3.4 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 2.3 %其他: 2.3 %China: 0.7 %China: 0.7 %[]: 0.2 %[]: 0.2 %上海: 1.1 %上海: 1.1 %中卫: 0.5 %中卫: 0.5 %北京: 6.2 %北京: 6.2 %南阳: 0.5 %南阳: 0.5 %哥伦布: 0.2 %哥伦布: 0.2 %天津: 0.5 %天津: 0.5 %平顶山: 0.2 %平顶山: 0.2 %张家口: 5.0 %张家口: 5.0 %扬州: 0.2 %扬州: 0.2 %武汉: 0.5 %武汉: 0.5 %沃思堡: 0.7 %沃思堡: 0.7 %济宁: 0.5 %济宁: 0.5 %温州: 0.2 %温州: 0.2 %盘锦: 0.7 %盘锦: 0.7 %芒廷维尤: 62.5 %芒廷维尤: 62.5 %莫斯科: 0.5 %莫斯科: 0.5 %西宁: 14.6 %西宁: 14.6 %贵阳: 0.2 %贵阳: 0.2 %郑州: 0.5 %郑州: 0.5 %金华: 0.2 %金华: 0.2 %长沙: 0.2 %长沙: 0.2 %阿什本: 0.7 %阿什本: 0.7 %青岛: 0.2 %青岛: 0.2 %黄石: 0.2 %黄石: 0.2 %其他China[]上海中卫北京南阳哥伦布天津平顶山张家口扬州武汉沃思堡济宁温州盘锦芒廷维尤莫斯科西宁贵阳郑州金华长沙阿什本青岛黄石

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

    Article Metrics

    Article views (1304) PDF downloads(872) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return