地球学报2011，Vol.32Issue(3)：313-321,9.DOI:10.3975/cagsb.2011.03.06
印度尼西亚塔里亚布岛锡铁多金属矿床的地质地球化学特征与成因
Geological and Geochemical Characteristics and Genesis of the Sn-Fe Polymetallic Deposit in Taliabu Island, Indonesia
摘要
Abstract
A large-size Sn-Fe polymetallic deposit, with more than one hundred million tons of iron reserves whose average grade (total Fe) is above 50％, has been recently discovered in Taliabu Island, Indonesia. Skarn and ore-magma are the main genetic types of the ore deposit, with the existence of hydrothermal type. These genetic types constitute a complete metallogenic system. The Indo-Chinese monzogranite derived from crustal partial melting magma is the main metallogenic material source and ore-control factor. Through high-degree evolution,the magma produced Fe-rich ore-magma injection and subsequently formed ore bodies, which mainly occurred in drastic variation places along rock mass boundary, soft and hard rock boundary in the contact zone between granite and Carboniferous strata. Skam type iron ore was formed in the contact zone between Carboniferous (dolomitic)marble, calciferous metasandstone and granite. The ore deposit belonged to Eastern Australia metallogenic belt during its formation, and then moved to Southeast Asia metallogenic belt by Himalayan movement.关键词
塔里亚布岛/地质地球化学/锡铁多金属矿床/矽卡岩型/矿浆型Key words
Taliabu Island/ geology and geochemistry/ Sn-Fe polymetallic deposit skarn type/ ore magma type分类
天文与地球科学引用本文复制引用
丁俊,张术根,徐忠发,秦新龙..印度尼西亚塔里亚布岛锡铁多金属矿床的地质地球化学特征与成因[J].地球学报,2011,32(3):313-321,9.基金项目
本文由中南大学与华东有色地勘集团合作项目"印度尼西亚塔里亚布岛铁矿成因、成矿机理及找矿方向研究"资助. （）
