新生代火山岛弧型成矿地质特征——以印度尼西亚吉布吉斯多金属矿床为例  

Geological characteristics of volcanic island arc mineralization in Cenozoic era——A Case Study of Cibugis polymetallic deposit in Indonesia

作　　者：符海明[1] 罗小洪 FU Hai-ming;LUO Xiao-hong(Geological Survey of JiangXi Province,Nanchang 330000,China;Geology and Mineral Bureau of JiangXi Province,Nanchang 330000,China)

机构地区：[1]江西省地质调查研究院,江西南昌330000 [2]江西省地质矿产勘查开发局,江西南昌330000

出　　处：《世界有色金属》2019年第14期135-137,共3页World Nonferrous Metals

摘　　要：新生代火山岛弧型矿床是环太平洋成矿带的一个重要的矿床类型,主要有铜、铅、锌、金、银等多金属成矿。本文论述了印度尼西亚吉布吉斯(Cibugis)多金属矿的矿床地质及矿体特征,以该矿床为例,概略地阐述了新生代火山岛弧成矿的主要特点:即第三纪成矿、火山构造控矿、容矿构造巨大、成矿元素复杂、氧化深度变化大、采选工艺复杂。The deposit of cenozoic volcanic island arc in the circum-pacific metallogenic belt is an important deposit type,gold、silver、copper、lead、zinc is main minerals in this article,such as the Indonesia's miss burgess(Cibugis)polymetallic ore deposit geology and ore body characteristics,the deposit,for example,briefly expounds the Cenozoic volcanic island arc the main characteristics of mineralization:namely tertiary metallogenic volcanic tectonic ore,ore controlling structures,oreforming elements complex oxide depth changes after selecting process.

关 键 词：印度尼西亚 新生代火山岛弧 矿床地质特征 吉布吉斯 

分 类 号：P618.2[天文地球—矿床学]