石油与天然气地质 ›› 2017, Vol. 38 ›› Issue (6): 1135-1146.doi: 10.11743/ogg20170614
吴海生, 郑孟林, 何文军, 杨彤远, 陈磊, 郭建辰, 杨翼波
收稿日期:
2016-05-06
修回日期:
2017-11-07
出版日期:
2017-12-28
发布日期:
2018-01-08
通讯作者:
郑孟林(1968-),男,教授级高级工程师,盆地构造。E-mail:zhengml@petrochina.com.cn。
E-mail:zhengml@petrochina.com.cn
作者简介:
吴海生(1968-),男,高级工程师,地震资料解释、储层预测、压力预测。E-mail:wuhaisheng@petrochina.com.cn。
基金资助:
Wu Haishen, Zheng Menglin, He Wenjun, Yang Tongyuan, Chen Lei, Guo Jianchen, Yang Yibo
Received:
2016-05-06
Revised:
2017-11-07
Online:
2017-12-28
Published:
2018-01-08
摘要: 应用钻井地层压力实测资料、测录井资料和地震速度资料等,结合盆地地层沉积结构分析,对准噶尔盆地腹部地区地层超压异常的横、纵向空间分布特征及其成因控制因素进行综合研究。研究表明:1)超压异常在盆地腹部地区普遍存在,其出现的顶界面具有穿层性,整体具有向西北方向超压顶面埋深变浅、向凹陷内埋藏变深的特点;超压顶面在莫索湾地区为侏罗系三工河组,顶面埋深在4 400 m左右,向西到夏盐-达巴松和玛湖地区超压顶面为三叠系,埋深在3 500 m左右,在莫南凸起的永进油田超压顶面在白垩系底部,埋深在5 800 m左右。2)莫索湾地区的侏罗系以下地层都存在超压异常,侏罗系的异常压力值最高,在二叠系-石炭系有所降低;同时,根据压力系数结构剖面特征分析,将超压异常划分为两种类型。3)分析盆地腹部超压异常的空间特征,认为不同层系、不同构造位置的超压异常形成具有不同的控制因素。
中图分类号:
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