陕西汉阴北部梅子垭组变质作用研究

刘欢, 高栋, 鲁浩, 罗德智, 张国鹏, 焦建刚. 陕西汉阴北部梅子垭组变质作用研究[J]. 西北地质, 2016, 49(2): 237-247.
引用本文: 刘欢, 高栋, 鲁浩, 罗德智, 张国鹏, 焦建刚. 陕西汉阴北部梅子垭组变质作用研究[J]. 西北地质, 2016, 49(2): 237-247.
LIU Huan, GAO Dong, LU Hao, LUO Dezhi, ZHANG Guopeng, JIAO Jiangang. Metamorphism of the Meiziya Formation in Northern Hanyin, Shaanxi Province[J]. Northwestern Geology, 2016, 49(2): 237-247.
Citation: LIU Huan, GAO Dong, LU Hao, LUO Dezhi, ZHANG Guopeng, JIAO Jiangang. Metamorphism of the Meiziya Formation in Northern Hanyin, Shaanxi Province[J]. Northwestern Geology, 2016, 49(2): 237-247.

陕西汉阴北部梅子垭组变质作用研究

  • 基金项目: 中国地质调查局项目"陕西石泉-旬阳金矿整装勘查区关键基础地质研究"(12120114014201)资助

Metamorphism of the Meiziya Formation in Northern Hanyin, Shaanxi Province

  • 梅子垭组是汉阴北部地区出露面积最大的地层,岩性主要为白云母石英片岩、含碳白云母石英片岩、含石榴子石黑云母变斑晶白云母石英片岩等,石榴子石和黑云母变斑晶在该岩层中普遍发育。该岩组构造变形复杂,经历了多期构造活动和变质变形过程。笔者在野外调查的基础上,通过分析研究区石榴子石、黑云母变斑晶的关系,采用石榴子石-黑云母地质温度计,对该区广泛出露的含石榴子石黑云母变斑晶白云母石英片岩进行研究,得到如下结论:研究区存在3期黑云母和石榴子石,石榴子石变斑晶具有明显的生长环带,而黑云母变斑晶没有环带;研究区变质作用的变质温度范围为介于511~572℃,主要为530~560℃;变质压力范围为0.16~0.84GPa,变质相属高绿片岩相。
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出版历程
收稿日期:  2015-06-15
修回日期:  2016-03-09
刊出日期:  2016-06-15

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