摘要
经从岩石学、矿物学、地球化学等方面对燕山期太山庙花岗岩体详细研究,认为该岩体侵入为一重要构造热事件,控制着区内多个多金属矿床的形成与规模。本文着重探讨和阐述太山庙花岗岩体特征及其对周边矿床的控矿关系。
Based on the study of the petrology, mineralogy and geochemistry, the author thought that the late Yanshanian granitoids intrusion is a important tectonism. This intrusion controlled many ore deposits size and ore deposit type. This article carries on the discussion from the above factor; elaborated Taishanmiao granite body controls the ore to its peripheral ore deposit.
出处
《华南地质与矿产》
CAS
2008年第1期12-16,共5页
Geology and Mineral Resources of South China
基金
国土资发[2003]20号文<汝阳县裂子山铅锌矿勘查资源补偿费项目>
关键词
岩体特征
多金属矿产
花岗岩体
太山庙
河南省
rock characteristic
polymetallic
granitoids
Taishanmiao
Henan Province
