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Volume 23 Issue 1

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Article Navigation > PETROLEUM GEOLOGY & EXPERIMENT > 2001 > 23(1): 52-55

Xie Zhiqing, Yan Xiaoxiong, Zhou Lifa. RESTORATION OF THE LOWER CRETACEOUS DENUDED THICKNESS IN THE SANTANGHU BASIN AND ITS EFFECT ON HYDROCARBON GENERATION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(1): 52-55. doi: 10.11781/sysydz200101052

Citation:

Xie Zhiqing, Yan Xiaoxiong, Zhou Lifa. RESTORATION OF THE LOWER CRETACEOUS DENUDED THICKNESS IN THE SANTANGHU BASIN AND ITS EFFECT ON HYDROCARBON GENERATION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(1): 52-55. doi: 10.11781/sysydz200101052

Xie Zhiqing, Yan Xiaoxiong, Zhou Lifa. RESTORATION OF THE LOWER CRETACEOUS DENUDED THICKNESS IN THE SANTANGHU BASIN AND ITS EFFECT ON HYDROCARBON GENERATION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(1): 52-55. doi: 10.11781/sysydz200101052

Citation:

Xie Zhiqing, Yan Xiaoxiong, Zhou Lifa. RESTORATION OF THE LOWER CRETACEOUS DENUDED THICKNESS IN THE SANTANGHU BASIN AND ITS EFFECT ON HYDROCARBON GENERATION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(1): 52-55. doi: 10.11781/sysydz200101052

RESTORATION OF THE LOWER CRETACEOUS DENUDED THICKNESS IN THE SANTANGHU BASIN AND ITS EFFECT ON HYDROCARBON GENERATION

doi: 10.11781/sysydz200101052

Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China

Received Date: 2000-05-08
Publish Date: 2001-01-25

Abstract

In this paper,the mudstone acoustic time difference method and the vitrinite reflectance method are used to calculate the Lower Cretaceous denuded thickness in the Santanghu basin.The results from the two methods fit well.It is revealed that the Lower Cretaceous denuded thickness is between 300m to 700m,and the denuded thickness increases from west to east.The Cenozoic sedimentary thickness,which is smaller than the Lower Cretaceous denuded thickness,cannot make up heat losses caused by denudation.Therefore,the Late Yanshanian movement played a destroying role in the generation of hydrocarbon.
- acoustic time difference,
- vitrinite reflectance,
- denuded thickness,
- the Lower Cretaceous,
- destroying effect,
- the Santanghu basin

References

[1]	张枝强,关强.新疆三塘湖盆地二叠系油源分析[J].石油实验地质,1998,20(2):174-181.
[2]	真柄钦次著,陈荷立译.压实与流体运移[M].北京:石油工业出版社,1981.
[3]	罗晓容,陈荷立.江汉盆地地层埋藏史研究[J].石油实验地质,1989,11(4):369-378.
[4]	Aoyagi K.Palaeotemperature analysis by authigenic minerals and its application to petroleum exploration[J].AAPG,1984,68:903-913.
[5]	Katz B J,Pheifer R N,Schunk D J.Interpretation of discontinuous vitrinite reflectance profiles[J].AAPG,1988,72(8):926-931.
[6]	Liu Yi-Qun,Zhou Ding-wu,Li Tao-hong.A discussion on the boundary between diagensis and metamorphism with reference to zeolite facies[J].The Island Arc,1993,1(4):262-272.

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