| 注册
首页|期刊导航|中国石油大学学报(自然科学版)|东辛地区营26断层变换带形成机制模拟

东辛地区营26断层变换带形成机制模拟

杨少春 白青林 路智勇 汪勇

中国石油大学学报(自然科学版)2017,Vol.41Issue(1):25-33,9.
中国石油大学学报(自然科学版)2017,Vol.41Issue(1):25-33,9.DOI:10.3969/j.issn.1673-5005.2017.01.003

东辛地区营26断层变换带形成机制模拟

Forming mechanism simulation of Ying 26 transfer zone in Dongxin area

杨少春 1白青林 2路智勇 1汪勇1

作者信息

  • 1. 中国石油大学地球科学与技术学院,山东青岛266580
  • 2. 海洋国家实验室海洋矿产资源评价与探测技术功能实验室,山东青岛266071
  • 折叠

摘要

Abstract

An tenso-torsional experimental apparatus with diapirism is designed for Ying 26 overlapping transfer zone formed during Shahejie Formation depositional stage in responding to the regional stress field in Dongxin area,Dongying sag.The aim is to simulate the formation mechanism and to reveal the law of distribution and development in the fracture system.Moist arentilla is chosen as the experimental material from the sand,clay and their mixture with different moisture.Experimentation process is filmed in detail and interpreted accurately.The results of the experiment show that:The Ying1 fault and Ying31 fault did not result from an early fault dislocated by lately transfer fault;instead they formed as two parallel faults before the deposition of Shahejie Formation under the effect of the extension in about NE10°.As pre-existing faults,the extensional displacement of the two faults induced the first shearing transform fault in the transfer zone.The fault strike of transform fault is oblique with the stretching direction with 50-degree angle.The higher the overlap ratio of the two faults,the more developed the transfer fault.Then dextral strike slipping formed a series of en-echelon faults and the dominant strike direction is in accord with the direction of shear stress field.At last,the diapirism complicated the fracture system in the late stage.Lowgrade faults grew mostly on the cross,round and the crotch of faults,especially in small blocks closed or semi-closed by secondary faults due to large differences between minimum and maximum principal stress in this area.In addition,shear faults are oblique in the plane and strike-slip in different directions,forming tilted local blocks.As a result,the distribution of lowgrade fault is more complex.

关键词

东辛地区/营26断层变换带/形成机制/应力场数值模拟/构造物理模拟/低级序断层/东营凹陷

Key words

Dongxin area/Ying 26 transfer zone/formation mechanism/stress field numerical simulation/structural physical simulation/low-grade faults/Dongying sag

分类

能源科技

引用本文复制引用

杨少春,白青林,路智勇,汪勇..东辛地区营26断层变换带形成机制模拟[J].中国石油大学学报(自然科学版),2017,41(1):25-33,9.

基金项目

国家科技重大专项课题(2011ZX05011-003) (2011ZX05011-003)

中国石油大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1673-5005

访问量0
|
下载量0
段落导航相关论文