摘要
川西坳陷不同地区须三-须四段含油气系统主要成藏期各不相同。作者以烃源岩演化过程中各阶段的最大古地温和最大埋深为基础,结合实钻资料,确立了川西坳陷须三-须四段含油气系统不同地区烃源岩的生排烃阶段,并利用不同生排烃阶段生排烃量、砂泥岩孔隙度变化和油气成藏之间的关系,确定了不同地区的主要成藏期,同时进行了对比研究。东西方向上,在中部地区该含油气系统的主要成藏期都为晚侏罗世;而在南北方向上,北部地区明显要早于中部和南部地区。
Based on the maximum paleogeotemperature and buried depth of each stage in the source rock evolution process and combined the real data of drilled wells, the paper establishes the hydrocarbon generating and expulsion- stages of source rocks in the T3x^3- T3x^4 petroleum system of different areas in the west Sichuan depression. Using the relation among quantity of different hydrocarbon-generating and expulsion stage and the porosity variation of sandstone and mudstone and oil/gas accumulation, the paper establishes the main accumulation stages in different areas, and at the same time, makes a comparative study. The main accumulation stages were all in Late Jurassic in this petroleum system in the middle part in latitudinal direction, but that of north area was earlier than that of the middle and south areas in meridional direction.
出处
《成都理工大学学报(自然科学版)》
CAS
CSCD
北大核心
2006年第3期252-255,共4页
Journal of Chengdu University of Technology: Science & Technology Edition
基金
国家"十五"科技攻关项目(2001BA605A-05-01)
关键词
川西坳陷
含油气系统
生排烃
主要成藏期
west Sichuan depression
petroleum system
generation and expulsion of hydrocarbon
main accumulation stage