八面河地区郭井子潜山结构构造及演化  

On Guojingzi Buried Hill Structural Evolution in Bamianhe Area

作　　者：许叶妹[1] 张磊[1] 胡秀蓉 

机构地区：[1]中国石化江汉油田分公司勘探开发研究院,湖北武汉430223 [2]中国石油西南油气田川东北气矿,四川达州635006

出　　处：《江汉石油职工大学学报》2015年第2期4-5,11,共3页Journal of Jianghan Petroleum University of Staff and Workers

摘　　要：郭井子潜山为北西向古生界残丘山与中生界断块山复合型潜山,主要受印支、燕山和喜山三期构造运动的控制与改造,形成现今北西成带、南北分块的构造格局,其对本区含油气系统的发育与油气分布起制约作用。区内古生界奥陶系及中生界侏罗系均发现工业油流,是八面河地区油气勘探的接替层系之一。NW -trending Paleozoic residual hillock and Mesozoic block mountain constitute compound Guo‐jingzi buried hill .Mainly controlled and transformed by tectonic movement at three stages of Indosinian , Yanshan and Himalayan ,it is in the structural frameworks of NW -trending banded structure and SN -trending block structure ,w hich restricts the development of its hydrocarbon -bearing system and its hydro‐carbon distribution .Industrial oil flow of Paleozoic Ordovician and Mesozoic Jurassic in this region shows that it is one of ready bed series for oil -gas exploration in Bamianhe Oilfield .

关 键 词：郭井子潜山 中古生界 结构 构造演化 

分 类 号：TE111.2[石油与天然气工程—油气勘探]