南秦岭汉阴北部金斗坡矿区志留系梅子垭组面理以S2面理为主。大比例尺构造-岩相填图和剖面实测所获得的大量S2面理产状数据显示，S2面理倾向305°~355°，倾角为25°~50°，为稳定北倾的平直面理。通过S2面理产状数据连图和综合分析，S2面理与金矿化具有相同的展布特征及变化规律，对成矿具有制约作用。此外，选取梅子垭组含石榴石黑云母变斑晶绢云母石英片岩中的共生矿物石榴石-黑云母进行电子探针测试，运用 Holdaway 石榴石-黑云母地质温度计方法，估算出该区热蚀变温度为590℃~670℃。综合研究表明，印支晚期—燕山早期为金矿的成矿期，在此期间岩浆热液的强烈活动引起热蚀变作用的发生，生成石榴石与黑云母变斑晶；热变质作用促使Au元素发生活化，有利于后期Au元素富集成矿。%The foliation of Silurian Meiziya Group in Jindoupo ore area of the northern Hanyin, South Qinling is mostly S2 foliation.The massive occurrence data from mapping as well as section plane based on large measuring scale indicate that the tendency of S2 foliation are 305°-355°with the dip angle of 25°-50°;the S2 foliation,which inclines towards the north,is stable as well as placid.After comprehensive mapping and analysis,the distribution direction of S2 foliation is mainly the same as that of gold mineralization,and has obvious constraint on mineralization.In addition,after testing the biotite-garnet paragenetic mineral assemblage from garnet-bearing biotite metacrysta sericite-schist of Meiziya Group by electron probe microanalysis,the thermal alteration temperature (590 ℃-670 ℃)was estimated by the means of Holdaway biotite-garnet geothermometer method.Comprehensive study indicates that Late Indosinian-Early Yanshanian is the metallogenic period of Au deposit,and the intense magmatic hydrothermal activities cause hydrothermal alteration and give birth to biotite metacrysta as well as garnet;the thermometamorphism accelerates the activity of Au,which has the advantage of later mineralization.
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