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渤中凹陷石南地区古近系断层活动特征及其对沉积相的控制
引用本文:庞小军,李建平,王冠民,汪跃,周学锋.渤中凹陷石南地区古近系断层活动特征及其对沉积相的控制[J].西安石油大学学报(自然科学版),2012,27(1):11-16,22,117,118.
作者姓名:庞小军  李建平  王冠民  汪跃  周学锋
作者单位:1. 中海石油(中国)有限公司天津分公司,天津,300452
2. 中国石油大学(华东)地球科学与技术学院,山东青岛,266555
基金项目:国家"十一五"科技重大专项,中央高校基本科研业务费专项资金项目,国家"十二五"科技重大专项
摘    要:利用三维地震、钻/测井等资料,对渤中凹陷古近系石南地区的构造、地层及沉积进行详细解释,运用断层活动速率法,系统分析了古近系石南断层活动特征及其对沉积相的控制.结果表明:石南地区由西向东依次发育近EW、NNE、EW走向的分支断层.古近系沉积演化过程中,石南断层活动强度呈"弱—增强—减弱—最强—减弱—最弱"的变化趋势;随着断层活动速率的降低,沉积相依次为扇三角洲、冲积扇、曲流河三角洲、辫状河三角洲、滩坝等相类型.

关 键 词:断层活动速率  沉积相  渤中凹陷  古近系  石南断层

Characteristics and controlling effect of fault activity of Paleogene in Shinan area of Bozhong Depression on sedimentary facies
PANG Xiao-jun,LI Jian-ping,WANG Guan-min,WANG Yue,ZHOU Xue-feng.Characteristics and controlling effect of fault activity of Paleogene in Shinan area of Bozhong Depression on sedimentary facies[J].Journal of Xian Shiyou University,2012,27(1):11-16,22,117,118.
Authors:PANG Xiao-jun  LI Jian-ping  WANG Guan-min  WANG Yue  ZHOU Xue-feng
Institution:1(1.Tianjin Branch,CNOOC Ltd.,Tianjin 300452,China;2.Faculty of Geology Science and Technology,China University of Petroleum(East China),Qingdao 266555,Shandong,China)
Abstract:The detailed structural,stratigraphic and sedimentary interpretation of Paleogene in the studied area are carried out using three-dimensional seismic,drilling / logging data,etc.The characteristics and controlling effect of fault activity of Paleogene on sedimentary facies are analyzed.The results show that in Shinan area are developed the branch faults in the directions of close EW,NNE,EW from west to east.In the evolution of Paleogene sediments,the activity intensity of Shinan fault presents the trend of "weak-Enhancing-weakening-the strongest-weakening-the weakest".With the decreasing of fault activity rate,sedimentary facies are fan-delta or nearshore subaqueous fan,alluvial fan,meandering river delta,braided delta,beach bar and other facies.
Keywords:fault activity rate  sedimentary facies  Bozhong depression  Paleogene system  Shinan fault
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