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江苏六合方山新生代碱性玄武岩中幔源橄榄岩的显微构造研究
引用本文:杨美娥,王文瑚.江苏六合方山新生代碱性玄武岩中幔源橄榄岩的显微构造研究[J].地震地质,1985,7(4):71.
作者姓名:杨美娥  王文瑚
作者单位:国家地震局地质研究所 (杨美娥),国家地震局地质研究所(王文瑚)
摘    要:本文对江苏六合方山玄武岩火山锥中的幔源捕虏体进行了显微构造、结构、组构以及橄榄石的扭折构造和滑移系作了测定和初步研究,并估算了本区上地幔古温压状态和应变速率等物理参数,对上地幔的运动特性进行了探讨

关 键 词:橄榄石  捕虏体  江苏六合  幔源橄榄岩  方山  碱性玄武岩  显微构造  顽火辉石  新生代  扭折

MICROSTRUCTURE STUDIES OF SOME MANTLE PERIDOT1TES IN CENOZOIC ALKALI-BASALTS FROM FANGSHAN,LIUHE COUNTY,JIANGSU PROVINCE
Abstract:In this paper microstructure,texture,and preferred orientations in peridotites from Fangshan have been studied and kink structure,glide systems in olivins have been measured primarily.Fangshan is a volcanoc cone which consisted of Cenozoic alkali-basalts as the substances were carried out from upper mantle by volcanic eruptions.The results indicate that crystalline plasticity and solid state flow are characteristic of upper mantle.The upper mantle physical parameters for this region have been calculated as:Temperature T=1278-1487°KConfining pressure P= 17.3-30.1kbApplied stress =214-362bDepth Z = 57-95kmstrain rate = 10-13...10-16 strain/sec.Viscosity =1.3×1020p-1.3×1023p
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