Lin Liangbiao, Wu Xinhe. PETROLEUM GEOLOGY CONDITION ANALYSIS ON THE MESOZOIC OF THE CUOQIN BASIN IN TIBET[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(4): 348-352. doi: 10.11781/sysydz201004348
Citation: Lin Liangbiao, Wu Xinhe. PETROLEUM GEOLOGY CONDITION ANALYSIS ON THE MESOZOIC OF THE CUOQIN BASIN IN TIBET[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(4): 348-352. doi: 10.11781/sysydz201004348

PETROLEUM GEOLOGY CONDITION ANALYSIS ON THE MESOZOIC OF THE CUOQIN BASIN IN TIBET

doi: 10.11781/sysydz201004348
  • Received Date: 2010-03-29
  • Rev Recd Date: 2010-07-13
  • Publish Date: 2010-08-28
  • According to the petroleum geologic research of outcrop,the test analysis of the rock samples,and the datum or results of the predecessors,this paper had researched the petroleum geological conditions of Cuoqin Basin integratively,such as the hydrocarbon rock,reservoir rock and cap rock.The result suggest that the Cuoqin Basin in Mesozoic have three units source rocks(limestone and marlstone of Langshan Formation-Jiega Formation,mudstone of Chuanba section of Duoni Formation,marlstone of Jienu Group),three kinds of reservoir rocks(reef-limestone,dolostone and sandrock of Langshan Formation and Duoni Formation),two units cap rocks(mudstone of Duoni Formation and limestone of Langshan Formation).Furthermore,the discovery of oil exposure and the bituminous of fluid inclusions showed that the Cuoqin Basin had underwent the process of oil and gas generated,migrated,gathered and lost,possesses the material foundation of oil and gas generation and the petroleum geologic conditions of hydrocarbon accumulation.All the evidences indicate that the Cuoqin Basin has good prospect of oil and gas exploration.

     

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  • [1]
    王成善,伊海生,李勇,等.羌塘盆地地质演化与油气远景评价[M].北京:地质出版社,2001:184-215.
    [2]
    赵政璋,李永铁,叶和飞,等.青藏高原海相烃源层的油气生成[M].北京:科学出版社,2000:610-613.
    [3]
    赵政璋,李永铁,叶和飞,等.青藏高原羌塘盆地石油地质[M].北京:科学出版社,2000:356-367.
    [4]
    赵政璋,李永铁,叶和飞,等.青藏高原大地构造特征及盆地演化[M].北京:科学出版社,2000:1-439.
    [5]
    南征兵,李永铁,郭祖军.羌塘盆地油气显示及油源对比[J].石油实验地质,2008,30(5):503-507.
    [6]
    杜佰伟,陈明.羌塘盆地上侏罗统索瓦组烃源岩分布特征及远景分析[J].石油实验地质,2008,30(2):174-178.
    [7]
    王成善,伊海生,刘池洋,等.西藏羌塘盆地古油藏发现及其意义[J].石油与天然气地质,2004,25(2):139-143.
    [8]
    伍新和,张丽,王成善,等.西藏羌塘盆地中生界海相烃源岩特征[J].石油与天然气地质,2008,29(3):348-354.
    [9]
    刘增谦,潘桂棠.西藏特提斯地质[M].北京:地质出版社,1990:94-98.
    [10]
    余光明,王成善,张哨楠.西藏特提斯中生代沉积盆地特征及演化[J].中国科学(B辑),1989(9):982-990.
    [11]
    王成善,张哨楠.青藏高原含油气盆地分析及油气资源预测[J].地球科学——中国地质大学学报,1996,21(2):120-129.
    [12]
    费琪,邓忠凡.西藏特提斯构造域海相油气前景[J].地球科学——中国地质大学学报,1996,21(2):113-119.
    [13]
    王成善,张哨楠.藏北双湖地区三叠系油页岩的发现[J].中国地质,1987(8):29-31.
    [14]
    孔祥儒,王谦身.西藏高原西部综合地球物理与岩石圈结构研究[J].中国科学(D辑),1996,26(4):308-315.
    [15]
    杨华.青藏高原航磁图展示的地球物理特征及其地质构造意义[J].地球物理学报,1985,28(增刊I):185-195.
    [16]
    熊绍柏,刘宏兵.青藏高原西部的地壳结构[J].科学通报,1997,42(12):1309-1312.
    [17]
    熊盛青,周伏洪,姚正煦,等.青藏高原中西部航磁调查[M].北京:地质出版社,2001:1-221.
    [18]
    殷秀华,黎益仕,冯华.青藏高原重力场特征和地壳构造[J].物探与化探,1998,22(6):440-445.
    [19]
    王冠民.西藏措勤盆地构造沉积演化及含油气远景[J].石油学报,2001,22(1):31-35.
    [20]
    丁俊,王剑,王成善,等.青藏油气资源战略选区[M].北京:地质出版社,2008:20-200.
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