摘要
青海省卡而却卡铜多金属矿位于秦祁昆晚加里东造山系(Ⅰ级)、东昆仑造山带(Ⅱ级)的伯喀里克—香日德元古宙古陆块体(Ⅲ级),区域内岩浆活动强烈,以中—酸性岩浆侵入为主,其主要受断裂为主的构造作用构成典型的多旋回构造岩浆,地层出露较简单。对青海省卡而却卡铜多金属矿地球化学特征与成矿规律进行了研究分析。
Kaerikaka copper polymetallic deposit in Qinghai Province is located in the Berkrik-Xiangride Proterozoic paleocontinental block of the Qinjiao-Kanga-Galdong-Orogenic System-Grade I and the Eastern Kunlun Orogenic Belt/Level II. The magmatic activity in the area is strong, mainly due to the intrusion of medium-acid magma. The main structural damage is caused by faults that constitutes a typical multi-cycle structural magma. The formation is relatively simple. The geochemical characteristics and deposit in Qinghai Province were studied and analyzed metallogenic regularity of the Kaerika copper polymetallic deposit in Qinghai Province were studied and analyzed.
作者
马璟璟
陈澍豪
代威
莫生娟
MAJingjing;CHEN Shuhao;DAI Wei;MO Shengjuan(The Third of Qinghai Geological and Mineral Exploration Institute,Xining,Qinghai 810001,China)
出处
《中国锰业》
2018年第5期64-66,73,共4页
China Manganese Industry
基金
青海省科技厅重大科技专项(2016-SF-A3)
国土资源部公益性行业科研专项(201411025)
关键词
卡而却卡
铜多金属矿
地球化学特征
成矿规律
Cadillac
Copper polymetallic ore
Geochemical characteristics
Metallogenic regularity
