东南亚中南半岛岩浆岩带特征与成矿关系研究  

Magmatic Rock Zones and Mineralization in Indo-China Peninsula

作　　者：徐卫东 张道阔[1] 马腾飞 彭江波 王海侠[1] 杨国强[1] XU Wei-dong;ZHANG Dao-kuo;MA Teng-fei;PENG Jiang-bo;WANG Hai-xia;YANG Guo-qiang(Henan Center for Aerial Geophysical Remote Sensing,Zhengzhou450000;The 7th Geological Team,Henan Bureau of Non-ferrous Metals Geological Mineral Resources,Zhengzhou450000)

机构地区：[1]河南省航空物探遥感中心,郑州450000 [2]河南省有色金属地质矿局第七地质大队,郑州450000

出　　处：《四川地质学报》2021年第4期562-567,共6页Acta Geologica Sichuan

摘　　要：东南亚中南半岛成矿带是特提斯成矿域的重要组成部分,富含丰富的矿产资源(刘书生等,2014)。根据岩浆岩带的空间展布、形成机制、岩石组合类型,按照板块构造、碰撞造山及岩浆事件的火山喷发沉积特征等,将该成矿带中岩浆岩划分为3大类岩浆岩带。通过对东南亚中南半岛地质背景及成矿规律研究,结合前人研究成果,将东南亚中南半岛成矿带划分了12个三级成矿带,6种成矿类型。本文为从整体上认识该区的岩浆岩展布特征,进而总结其成矿作用提供了有益信息,同时为该区开展区域地质调查与矿产勘查工作提供参考依据。The Indo-China Peninsula metallogenic belt is an important part of the Tethyan metallogenic domain which is rich in mineral resources.The magmatic rocks in this metallogenic belt may be divided into 3 major zones.The metallogenic belt is divided into 12 tertiary metallogenic belts and contains 6 mineralization types.Distribution and characteristics of the magmatic rock zones and mineralization types are discussed.

关 键 词：岩浆岩带 成矿作用 东南亚中南半岛 

分 类 号：P588.19[天文地球—岩石学] P612[天文地球—地质学]