摘要
油气输导体系和油气运移的特征决定油气藏形成与分布。惠民凹陷商河地区地质条件分析结果表明,其输导体系空间配置构成4种模式:砂体—断层—砂体、砂体—断层—不整合、砂体—火山锥以及砂体—断层—火山锥;该区主要发育的是阶梯型输导体系分布组合,以断裂、骨架砂体共同构成的运聚体系呈阶梯型输导,导致油气爬坡运移、单层系成藏。
The distribution and forming of the reservoir depend on the types of the hydrocarbon transport system and the features of the hydrocarbon migration. The geologic conditions of the Shanghe area in Huimin Sag is analyzed, the result show that the types of its hydrocarbon transport system spatially have four modes, they are＂sand body-fault-sand body＂,＂sand body-fault-unconformity＂,＂sand body-volcanic cone＂and＂sand body-faultvolcanic cone＂, It was mainly developed step- transport system distribution combination, the migrationconcentration system which was consisted of fault and frame sand body jointly showed step transport, it resulted in reservoir forming by migrating upwards and single-layer.
出处
《油气地球物理》
2016年第2期14-18,共5页
Petroleum Geophysics
关键词
油气输导体系
断层
油气运移特征
商河地区
惠民凹陷
hydrocarbon transport system
fault
feature of hydrocarbon migration
Shanghe area and Huimin Sag
作者简介
马玉歌,女,高级工程师,硕士,石油地质专业,现主要从事物探综合研究工作.
