德南洼陷下第三系成藏动力学系统研究

2004年 11卷 第05期
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Dynamic System for Pool-Forming of Eogene in Denan Depression

付建元1  孙义梅2  王瑞华3
Fu Jianyuan , Sun Yimei,Wang Ruihua.


1. 四川石油管理局成都物探研究中心 2. 中国地质大学,北京 3. 成都地质矿产研究所
运用成藏动力学系统理论和方法, 根据德南洼陷下第三系沉积、构造及异常压力等特征, 重点剖析了泥岩层的欠压实特点, 将其划分为3 个成藏动力学系统即下部高压它源封闭成藏动力学系统、中部高压自源封闭成藏动力学系统和上部常压它源半封闭成藏动力学系统。同时分析了本区以泥灰岩裂缝、砂岩、不整合面以及断层等组成的流体输导体系,并初步探讨了该区有利的油气成藏模式, 即陡坡带成藏模式、洼中垒成藏模式和缓坡带成藏模式。
With the theory and method of the dynamic systemfor pool-forming , 
Denan depression has been classified into three kinds of
dynamic systems and four kinds of link systems , based on the
analysis of the sediment , structure , uncompaction and abnormal
pressure. The dynamic system for pool-forming of Eogene is
divided into lower part high pressure else-sourced closed dynamic
system, middle part high pressure self-sourced closed dynamic
system, upper part normal pressure else2sourced semi-closed
dynamic system. And the liquid link systems consist of marl
fissure , sandstone , unconformity surface and fault. Finally , the
favorable pool2forming models including actic region model , horst
model and ramp region model are discussed and the former two
kinds are principal.


德南洼陷 成藏动力学系统 欠压实 输导体系 成藏模式;
Denan depression ,Dynamic system for pool-forming ,Uncompaction ,Link system ,Pool-forming model.


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