珠江口盆地番禺隆起东南缘断裂坡折带及其对低位域构造—岩性油气藏的控制作用
    点此下载全文
引用本文:董伟,林畅松,谢利华,张忠涛,阳孝法,张燕梅,张博,崔立叶.2009.珠江口盆地番禺隆起东南缘断裂坡折带及其对低位域构造—岩性油气藏的控制作用[J].地球学报,30(2):256-262.
DOI:10.3975/cagsb.2009.02.15
摘要点击次数: 3222
全文下载次数: 4921
作者单位E-mail
董伟 中国地质大学(北京)能源学院, 北京 100083 dongwei_21@163.com 
林畅松 中国地质大学(北京)能源学院, 北京 100083  
谢利华 中国地质大学(北京)能源学院, 北京 100083  
张忠涛 中国海洋石油深圳分公司研究院, 广东广州 510240  
阳孝法 中国地质大学(北京)能源学院, 北京 100083  
张燕梅 中国地质大学(北京)地球物理与信息技术学院, 北京 10083  
张博 中国地质大学(北京)能源学院, 北京 100083  
崔立叶 中国地质大学(北京)能源学院, 北京 100083  
基金项目:国家重大基础规划发展项目(编号: 2006CB202302)资助
中文摘要:番禺隆起是珠江口盆地中南部的一个重要含油气区。区内新近系沉积期主要发育NW向和近EW向的同沉积断裂, 它们的发育和分布控制着沉积充填和总体的古构造地貌特征。古隆起的东南和东北缘发育的主要同沉积断裂形成明显的古地貌突变带或断裂坡折带。东南缘的主控断裂是由裂陷期发育的缓坡反向断裂所形成的, 构成了番禺隆起与白云深凹带的分界。地震相、地震属性等分析和追踪其分布范围揭示出, 珠海组、珠江组中下部层序的低位域三角洲砂体沿断裂坡折带下斜坡呈裙带状分布。研究指出断裂坡折带下斜坡低位域具有形成构造—岩性油气藏的良好条件, 并为该区近期的勘探突破提供了重要依据
中文关键词:断裂坡折带  古构造地貌  岩性油气藏  珠江口盆地
 
Fault Slope-Break Zone and Its Control over Structural Lithostratigraphic Traps of Lowstand System Tracts in Southeast Panyu Uplift of the Pearl River Mouth Basin
Abstract:The Panyu Uplift is an important oil and gas-bearing district in central south Pearl River Mouth Basin. A series of northwest and east-west striking syndepositional faults were developed during Neogene, and their development and distribution controlled the paleo-structural framework and the sedimentary filling pattern. The main syndepositional faults along the southeastern and northeastern margins of the ancient uplift formed obvious geo-morphologic abrupt zones or fault slope-break zones. The main controlling faults in the southeastern part were formed by the antithetic faults in the hinge gentle slope which were developed during syn-rifting and formed the boundary between Panyu Uplift and Baiyun deep sag. An analysis of seismic facies and seismic attributes has shown that the lowstand system tract deltaic sandstones in the middle-lower part of Zhuhai and Zhujiang Forma-tions were developed and distributed along the low slope of the fault slope-break zone. Researches indicate that the low slope lowstand system tracts along the fault slope-break zone constitute a favorable condition for the forma-tion of lithostratigraphic or structural-stratigraphic traps. This study hence has offered an important basis for the recent exploration breakthrough in this area.
keywords:fault slope-break zone  paleo-structrual geomorphic feature  lithostratigraphic reservoirs  Pearl River Mouth Basin
查看全文  查看/发表评论  下载PDF阅读器
版权所有 《地球学报》编辑部 Copyright©2008 All Rights Reserved
主管单位:中华人民共和国自然资源部 主办单位:中国地质科学院
地址: 北京市西城区百万庄大街26号,中国地质科学院东楼317室 邮编:100037 电话:010-68327396 E-mail: diqiuxb@126.com
技术支持:北京勤云科技发展有限公司
京ICP备05029128号-6

京公网安备 11010202007616号