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A New Growth Model of Fault Attributes in a Strike-Slip Fault System in the Tarim Basin

A New Growth Model of Fault Attributes in a Strike-Slip Fault System in the Tarim Basin

作     者:ZHANG Yintao WU Guanghui WANG Junfang LI Guohui WAN Xiaoguo YANG Tianyi ZHANG Yintao;WU Guanghui;WANG Junfang;LI Guohui;WAN Xiaoguo;YANG Tianyi

作者机构:School of Geoscience and TechnologySouthwest Petroleum UniversityChengdu 610500China PetroChina Tarim Oilfield CompanyKorlaXinjiang 841000China PetroChina Key Laboratory of Carbonate ReservoirSouthwest Petroleum UniversityChengdu 610500China 

出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))

年 卷 期:2020年第94卷第5期

页      面:1373-1380页

核心收录:

学科分类:0709[理学-地质学] 0819[工学-矿业工程] 081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0816[工学-测绘科学与技术] 

基  金:partly supported by the National Natural Science Foundation of China(Grant No.91955204) Science and Technology Cooperation Project of the CNPC-SWPU Innovation Alliance(Grant No.2020CX010300) 

主  题:fault modeling fault attributes strike-slip fault overlapping zone power-law-scaling fault growth process 

摘      要:Fault attributes generally display a consistent power–law-scaling *** on new 3 D seismic data,however,we found some exceptional fault attribute relationships of lengths(L)–throw(T)(vertical component of displacement),overlap zone length(Lo)–width(Wo)from a strike-slip fault system of the Ordovician carbonates in the Tarim *** L–T relationship shows two linear segments with breakup at^40 km in fault *** presents an exceptional throw increase in the second stage,which is attributed to a localization of vertical displacement and deformation in overlapping zones other than the different fault scales in a mature fault *** Lo–Wo relationship in the overlapping zones shows multiply stepped-shape patterns,suggesting multiple fault differential growth and periodic increase in fault ***,we propose a new alternative growth model of fault attributes in strike-slip fault zones,in which the overlapping zones accumulated localized displacement and deformation in the intracratonic strike-slip fault zone.

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