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塔北隆起中西部新近纪末构造应力场数值模拟
引用本文:王延欣,侯贵廷,李江海,潘懋.塔北隆起中西部新近纪末构造应力场数值模拟[J].北京大学学报(自然科学版),2008,44(6).
作者姓名:王延欣  侯贵廷  李江海  潘懋
作者单位:北京大学地球与空间科学学院,造山带与地壳演化教育部重点实验室,北京,100871
基金项目:国家自然科学基金 , 国家"863"计划  
摘    要:塔北隆起是塔里木盆地油气勘探开发最成功的地区之一,前人在构造变形特征、发育演化和形成的地球动力学机制等方面已经取得了较为明确的认识,并对中新生代负反转构造的形成机制做了深入研究1-6],但对本区各个时期的构造应力场研究却只限于简要描述,缺乏直接的证据和定量的分析

关 键 词:数值模拟  构造应力场  断裂构造  塔北隆起中西部

Numercial Simulation of Tenconic Stress Field at the end of Neocene in the Midwest of Tabei Uplift
WANG Yanxin,HOU Guiting,LI Jianghai,PAN Mao.Numercial Simulation of Tenconic Stress Field at the end of Neocene in the Midwest of Tabei Uplift[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2008,44(6).
Authors:WANG Yanxin  HOU Guiting  LI Jianghai  PAN Mao
Institution:WANG Yanxin,HOU Guiting,LI Jianghai,PAN Mao The Key Laboratory of Orogenic Belts and Crustal Evolution,School of Earth and Space Sciences,Peking University,Beijing 100871
Abstract:The plane and profile geological models at the end of Neocene in the midwest of Tabei uplift are established on the basis of seismic data of oil field and tectonic analysis,and the numerical simulation results of tectonic stress field in the area are obtained using linear elastic finite element method.Modeling results indicate that N-S regional compressive stress dominates the stress field of the whole area at that time,as well as that all faults of Yaha,Luntai,Hongqi,Yingmai 7 are compresso-shear structures with sinistral strike slip,while Kalayuergun fault is right lateral,and Yangtake fault is pure compressive thrust.In the condition of regional compressive stress,local stress field is formed,and affected by the main faults,which controlles the generation of secondary structures.In the modeling results of profile stress field,the orientation of the major principal stress change from horizon to incline in the middle of the uplifting area and the vertical stress component becomes bigger,which is the main factor to control the development of the compressional and subtuberant structures.
Keywords:numerical simulation  tectonic stress field  fault structure  the midwest of Tabei uplift
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