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准噶尔盆地乌夏断裂带构造分区
引用本文:冯建伟,戴俊生,刘巍,王军,李明.准噶尔盆地乌夏断裂带构造分区[J].新疆石油地质,2007,28(4):406-409.
作者姓名:冯建伟  戴俊生  刘巍  王军  李明
作者单位:1.中国石油大学 地球资源与信息学院, 山东 东营 257061; 2.新疆油田分公司 勘探开发研究院, 新疆 克拉玛依 834000
摘    要:基于对准噶尔盆地乌夏断裂带构造特征和构造演化的研究,依据断裂的分割性、构造变形强度、地层展布、基底起伏形态等,将乌夏地区(盆地亚一级构造单元)划分为乌尔禾冲断带、乌尔禾断褶带、乌尔禾单斜带、乌尔禾-夏子街冲断带、乌尔禾-夏子街单斜带、夏子街-红旗坝冲断带、夏子街-红旗坝断褶带和夏子街-红旗坝单斜带等8个次级单元,显示了东西分区、南北分带的特征。依据构造圈闭发育程度、油气运聚条件等,对各次级构造单元的油气成藏类型及分布进行了研究,认为断褶带油气藏类型最发育,是主力产油区,单斜带勘探潜力大,是油气的远景区。

关 键 词:准噶尔盆地  乌夏断裂带  构造单元  油气藏  
文章编号:1001-3873(2007)04-0406-04
收稿时间:2007-01-15
修稿时间:2007-01-15

Tectonic Units in Wu-Xia Fault Belt, Junggar Basin
FENG Jian-wei,DAI Jun-sheng,LIU Wei,WANG Jun,LI Ming.Tectonic Units in Wu-Xia Fault Belt, Junggar Basin[J].Xinjiang Petroleum Geology,2007,28(4):406-409.
Authors:FENG Jian-wei  DAI Jun-sheng  LIU Wei  WANG Jun  LI Ming
Affiliation:1. Faculty of Geo-Resources and Information, China University of Petroleum, Dongying, Shandong 257061, China; 2. Research Institute of Exploration and Development, PetroChina, Karamay, Xinjiang 834000, China
Abstract:The Wu-Xia fault belt of Junggar basin is divided into eight second-order tectonic units based on the study on tectonic features and tectonic evolution, such as Wuerhe thrust belt, Wuerhe fault-fold belt, Wuerhe monocline belt, Wuerhe-Xiazijie thrust belt, Wuerhe- Xiazijie monocline belt, Xiazijie-Hongqiba thrust belt, Xiazijie-Hongqiba fault-fold belt and Xiazijie-Hongqiba monocline belt, which reflect the characteristics of structural segmentation in east-west direction and structural zonation in south-north direction. According to the development of structural traps and the conditions of hydrocarbon accumulation, these second-order tectonic units are studied in hydrocarbon accumulation type and distribution. It is concluded that the fault-fold types in this area are most developed and serve as major oil production areas; the monocline belts are of the greatest explorative potentials, being the favorable prospecting areas.
Keywords:Wuerhe-Xiazijie fault belt  tectonic unit  petroleum reservoir
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