摘要
陕西小秦岭华阳川韧性剪切带发育在新太古界太华群之中,野外调研和显微构造观察结果表明,该韧性剪切带是由构造片岩、眼球状片麻岩组成的深层次韧性剪切带,具有逆冲兼左行走滑的斜冲特征。对韧性剪切带构造片岩黑云母进行40Ar/39Ar同位素定年,获得坪年龄为419M±0.6Ma,反等时线年龄为417Ma±0.8Ma。认为华阳川韧性剪切带及其相应的小秦岭区域主导构造变形是发生于419Ma左右的秦岭加里东事件的结果。
The Huayangchuan ductile shear zone in the Xiaoqinling Mountains, Shaanxi, formed in the Neoarchean Taihua Group complex. Field survey and microscopic observation have revealed this ductile shear zone is a deep-level zone, consisting of tectonic schist and augen gneiss, which have features of thrust and sinistral strike-slip oblique subduction. ^40Ar/^39Ar dating of biotite from tectonic schist in the ductile shear zone yielded a plateau age of 419±0.6 Ma and an inverse isochron age of 417±0.8 Ma. Therefore the authors think that the Huayangchuan ductile shear zone and its related regional principal tectonic deformation of the Xiaoqinling Mountains formed in the Caledonian event at 419±Ma.
出处
《地质通报》
CAS
CSCD
北大核心
2008年第6期823-828,共6页
Geological Bulletin of China
基金
国家精品课程《鄂尔多斯盆地-秦岭造山带野外地质教学》项目资助
