摘要
Microscopictomesoscopicstructuralinvestigationsandfoliationintersectionaxes（FIAs）preservedinporphyroblastsrevealaverycomplexhistoryofdeformationandtectonismwithinthesouthwesternpartofthewesternhinterlandzonealongthenorthernmarginoftheIndianplate,NWPakistan.D1,D2,andD3relatedstructuresinthesouthwesternpartresembletheF1/F2,F3,andF4relatedstructuresinthenortheasternpartofthewesternhinterlandzone.Thesestructuresdevelopedatthesametimethroughthesamechangesinthedirectionofbulkshorteninginsouthwesternandnortheasternpartsofthewesternhinterlandzone.FIAset1indicatesNW-SEshortening.TheD2fabrics,minerallineationsandfoldaxesindicateE-Wshortening.FIAset2,D3foldaxesandminerallineationsindicateNNE-SSWshortening.D3deformationeventisequivalenttotheF4deformationeventinthenortheasternpartofthewesternhinterlandzone.D4foldaxes,mineralstretchinglineationsandaxialplanefoliationsuggestENE-WSWshortening.TheD4NNW-SSEfabrics,whichformedintheregionaftertheformationoftheMMT（mainmantlethrust）,Khairabad-Panjalthrustfault,HissartangthrustfaultandMBT（mainboundarythrust）,likelyresultedfromENE-WSWbulkshorteningrelatedtodevelopmentoftheHazara-Kashmirsyntaxis.
出版日期
2016年04月14日（中国期刊网平台首次上网日期，不代表论文的发表时间）
