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地球科学进展  2005, Vol. 20 Issue (4): 459-466    DOI: 10.11867/j.issn.1001-8166.2005.04.0459
综述与评述     
烃源岩排烃作用研究现状及展望
陈中红, 查明
石油大学地球资源与信息学院,山东 东营 257061
CURRENT SITUATION AND PROSPECT OF THE INVESTIGATION ON HYDROCARBON EXPULSION FROM SOURCE ROCKS
CHEN Zhonghong; ZHA Ming
University of Petroleum, Shandong Dongying 257061, China
 全文: PDF(281 KB)  
摘要:

烃源岩排烃作用的研究在20世纪80年代以后取得了很大进展,主要体现在对烃源岩的排烃机理及控制因素的分析、煤成油排驱的理论研究及勘探突破、幕式排液的探讨及压实—压裂双端元排烃模型的建立等方面。在针对研究现状分析的基础上,提出了几点研究方向及展望:加强对烃源岩剖面排烃特征的高分辨率研究,建立压实—欠压实—压裂三端元排烃模型,对存在严重非均质性的烃源岩进行烃源岩排烃分级评价,深入探讨排烃与油气成藏的关系。

关键词: 烃源岩排烃作用幕式排液排烃模型    
Abstract:

The investigation on hydrocarbon-expulsion from source rocks has made big advances in the following aspects: the mechanism and key factors on hydrocarbon expulsion, the research on the oil derived from coals and its exploration break, episodic hydrocarbon-expulsion, and establishment of compaction-fracturing model of hydrocarbon-expulsion. On the basis of current situation on the investigation, the paper brings forward several suggestions and prospects of the research: strengthen the high resolution research on the characteristics of the hydrocarbon-expulsion in the section of source rocks, set up the hydrocarbon-expulsion model including three phases(compaction, uncompaction and cracking), evaluate hydrocarbon-expulsion on classification of the anisotropic source rocks, and discuss the relation between hydrocarbon-expulsion and hydrocarbon accumulation. 

Key words: Source rocks    Hydrocarbon-expulsion action    Episodic hydrocarbon-expulsion    Model of hydrocarbon-expulsion 
收稿日期: 2004-03-11 出版日期: 2005-04-25
:  P618.13  
基金资助:

国家“十五”重点科技攻关项目“济阳坳陷下第三系沉积体系与油气运聚机理”(编号:2001BA605A-09-21)资助

通讯作者: 陈中红   
作者简介: 陈中红(1976-),男,安徽怀宁人,博士研究生,现主要从事油气地质与勘探研究. E-mail:hongczh@163.com
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陈中红;查明. 烃源岩排烃作用研究现状及展望[J]. 地球科学进展, 2005, 20(4): 459-466.

CHEN Zhonghong;ZHA Ming. CURRENT SITUATION AND PROSPECT OF THE INVESTIGATION ON HYDROCARBON EXPULSION FROM SOURCE ROCKS. Advances in Earth Science, 2005, 20(4): 459-466.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2005.04.0459        http://www.adearth.ac.cn/CN/Y2005/V20/I4/459

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