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信阳龟山地区变余糜棱岩的矿物学特征与热-构造演化史
引用本文:徐德明,翟淳. 信阳龟山地区变余糜棱岩的矿物学特征与热-构造演化史[J]. 成都理工大学学报(自然科学版), 1997, 0(4)
作者姓名:徐德明  翟淳
作者单位:宜昌地质矿产研究所(徐德明),成都理工学院(翟淳)
摘    要:通过对河南信阳龟山地区变余糜棱岩中不同产状的石榴石、黑云母及白云母等矿物的矿物学特征及其反映的变质作用温压条件研究,建立了区内变余糜棱岩热-构造演化的三阶段模式:(1)原岩的深部加热和抬升;(2)中深部走滑剪切和逆冲推覆;(3)浅表层脆性断裂和火山岩浆活动。

关 键 词:矿物学,变质作用,热-构造演化史,变余糜棱岩,信阳龟山

MINERALOGY AND THERMOTECTONIC EVOLUTION OF BLASTOMYLONITES IN GUISHAN AREA, XINYANG, HENAN PROVINCE
Xu Deming. MINERALOGY AND THERMOTECTONIC EVOLUTION OF BLASTOMYLONITES IN GUISHAN AREA, XINYANG, HENAN PROVINCE[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 1997, 0(4)
Authors:Xu Deming
Abstract:This paper studies mineralogical features of some minerals such as garnet, biotite and muscovite etc. which exist as various occurrences and metamorphic conditions recorded by these minerals in blastomylonites in Guishan area, Xinyang. It is concluded that the thermotectonic evolution of the blastomylonites is divided into three stages as follows: the heating in depth and uplift of the parent rock of blastomylonites, deep ductile shearing and thrust napping, and the brittle fracturing and volcanic magmatism of the upper blanket.
Keywords:mineralogy  metamorphism  thermotectonic evolution  blastomylonite  Guishan in Xinyang
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