天然气地质学

试论柴达木盆地第四系盖层的封盖机理

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  • [1]西南石油学院; [2]青海油田; 四川南充; 甘肃敦煌;

网络出版日期: 2004-08-20

THE DISCUSSION UPON SEALING MECHANISM OF QUATERNARY CAP ROCK IN QAIDAM BASIN

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  • 1. Southwest Petroleum Institute, Nanchong, 637001, China;2. Qinghai Oilfield Company, Dunhuang 736202, China

Online published: 2004-08-20

摘要

通过对柴达木盆地第四系高孔隙度、低突破压力和具有一定渗透性的特殊盖层研究后指出:这种特殊盖层封盖天然气的机理在于其中饱和高矿化度的地层水;泥岩盖层中孔隙流体压力同下伏气藏压力值很接近;区域盖层厚度巨大;盖层是源岩层;区内气候寒冷,冰冻期长,冰川广布。

本文引用格式

张祥;纪宗兰;杨银山;曾惠兰;王永强;李宝山; . 试论柴达木盆地第四系盖层的封盖机理[J]. 天然气地球科学, 2004 , 15(4) : 383 -386 . DOI: 10.11764/j.issn.1672-1926.2004.04.383

Abstract

Through the researches onthe special Quaternary cap rock with the characteristics of high porosity, low breakthrough pressure and some permeability in qaidamu Basin, the parper points out that the sealing mechanism of the cap rock lies in the high salty formation water existing inside the cap rock. The fluid pressure in mudstone pores approximately equals to the pressure in gas reservoir below; the thickness of regional cap rock in very high and the cap rock itself belongs to source rock.

参考文献

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