石油实验地质Issue(2)：153-159,7.DOI:10.11781/sysydz201402153
苏北盆地溱潼凹陷新生代侵入岩蚀变带油藏地质特征
Geologic features of reservoirs in Cenozoic intrusive rock metamorphic zone, Qintong Sag, Northern Jiangsu Basin
姚洪生 1张勇 1蒋永平 1赵梓平1
作者信息
- 1. 中国石化 华东分公司 采油厂，江苏 泰州 225300
- 折叠
摘要
Abstract
The time and space relationships between Cenozoic intrusive rock distributions and metamorphic zone reservoirs in the Qintong Sag of the Northern Jiangsu Basin were analyzed, and the corresponding accumulation mechanisms and patterns were discussed. The rock intrusions started during the Sanduo Movement of Eocene. Vertically, there were bedding intrusions and cutting-bedding intrusions. The intrusive rocks distributed like bead strings on plane map. Magma intrusions accelerated the thermal evolution of source rocks, and metamorphisms formed favorable reservoir spaces. Affected by up-arch stress and upper sediments, a series of related hydrocar-bon traps was formed. The evolution of magma intrusion played an important role in the hydrocarbon accumulation in the Qintong Sag.关键词
油气成藏/蚀变带/侵入岩/新生代/溱潼凹陷/苏北盆地Key words
hydrocarbon accumulation/metamorphic zone/intrusive rock/Cenozoic/Qintong Sag/Northern Jiangsu Basin分类
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姚洪生,张勇,蒋永平,赵梓平..苏北盆地溱潼凹陷新生代侵入岩蚀变带油藏地质特征[J].石油实验地质,2014,(2):153-159,7.
