Paleo-temperature Evolution and Water Soluble Gas in Sinian Reservoir, Anpingdian-Gaoshiti Structural Zone, Central Sichuan Basin

被引：4

作者：

袁海锋 ^{[1
]}

徐国盛 ^{[1
]}

刘树根 ^{[1
]}

王国芝 ^{[1
]}

机构：

[1] State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology

来源：

Journal of China University of Geosciences | 2008年 / 06期

关键词：

Central Sichuan (四川) basin; Anpingdian (安平店)-Gaoshiti (高石梯) structural zone; paleo-temperature; apatite fission track; fluid inclusion; water soluble gas;

D O I：

暂无

中图分类号：

P618.13 [石油、天然气];

学科分类号：

0709 ; 081803 ;

摘要：

The paleo-temperature evolution of Sinian reservoir of Anping (安平) 1 well was rebuilt by taking the method of apatite fission track and Easy%Ro model. The result of apatite fission track determines the accurate burial history and overcomes the flaw that the vitrinite reflectance is taken as paleo-temperature indicator simply. The authors used the laser Raman technique to analyze the meth- ane present in the calcite and quartz fluid inclusions of Sinian reservoir, finding that the methane is water soluble gas. The authors also simulated the paleo-pressure of fluid inclusion by using PVTsim software and finally worked out the methane solubility in water.

引用

页码：707 / 714

页数：8

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