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南美洲铁矿重要成矿区带与成矿规律研究
引用本文:赵宏军,卢民杰,周尚国,叶锦华,陈秀法,张潮,郭维民,黄费新,姚春彦.南美洲铁矿重要成矿区带与成矿规律研究[J].中国地质,2017,44(4):690-706.
作者姓名:赵宏军  卢民杰  周尚国  叶锦华  陈秀法  张潮  郭维民  黄费新  姚春彦
作者单位:中国地质调查局发展研究中心, 北京 100037,中国地质科学院地质研究所, 北京 100037,中国冶金地质总局矿产资源研究院, 北京 101300,中国地质调查局发展研究中心, 北京 100037,中国地质调查局发展研究中心, 北京 100037,中国地质调查局发展研究中心, 北京 100037,中国地质调查局南京地质调查中心, 江苏 南京 210016,中国冶金地质总局矿产资源研究院, 北京 101300,中国地质调查局南京地质调查中心, 江苏 南京 210016
基金项目:中国地质调查局地质调查项目(121201004000150010、:121201004000150009、1212011220912)及国家国际科技合作专项(2011DFA22460)联合资助。
摘    要:南美洲铁矿资源丰富、分布广泛、矿床规模大、矿石品位高、类型较齐全。从南美洲大地构造格架分析,分布在克拉通地盾区或其边缘的沉积-变质型铁矿和分布在安第斯海岸造山带的火山成因型铁矿最为重要,沉积-变质型铁矿主要形成于太古宙—元古宙,火山成因型铁矿主要形成于中新生代。综合研究分析,圈出10个铁矿重要成矿区带,主要分布在委内瑞拉的玻利瓦尔州,巴西的阿马帕州、帕拉州、米纳斯吉拉斯州、北里奥格兰德州、巴拉伊巴州、巴伊亚州、南马托格罗索州,玻利维亚的圣克鲁斯州,秘鲁的伊卡—阿雷基帕海岸带和智利的卡拉马—圣地亚哥海岸带等。通过对重要成矿区带内典型矿床的剖析,并采用统计分析方法总结南美洲铁矿成矿时空分布规律,为未来在该区寻找更多的铁矿资源提供参考。

关 键 词:南美洲  铁矿  资源特征  成矿区带  成矿规律
收稿时间:2017/7/20 0:00:00
修稿时间:2017/8/20 0:00:00

A study of key metallogenetic zones and principal metallogeic regularities of iron ore resources in South American countries
ZHAO Hongjun,LU Minjie,ZHOU Shangguo,YE Jinhu,CHEN Xiuf,ZHANG Chao,GUO Weimin,HUANG Feixin and YAO Chunyan.A study of key metallogenetic zones and principal metallogeic regularities of iron ore resources in South American countries[J].Chinese Geology,2017,44(4):690-706.
Authors:ZHAO Hongjun  LU Minjie  ZHOU Shangguo  YE Jinhu  CHEN Xiuf  ZHANG Chao  GUO Weimin  HUANG Feixin and YAO Chunyan
Institution:Development and Research Center of China Geological Survey, 100037, Beijing, China,Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China,Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 101300, China,Development and Research Center of China Geological Survey, 100037, Beijing, China,Development and Research Center of China Geological Survey, 100037, Beijing, China,Development and Research Center of China Geological Survey, 100037, Beijing, China,Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China,Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 101300, China and Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China
Abstract:South America is rich in iron ore resources, which are characterized by widely distributed world-class iron deposits, high grade of orebodies, and a variety of deposit types. An analysis of tectonic framework of South America shows that the most important types of iron deposits include sedimentary metamorphic type which is distributed in cratonic shield area and its edge, and volcanic origin type which is distributed in Andean coastal orogenic belt. The former mainly formed in the Archean Proterozoic, whereas the latter mainly formed in Mesozoic and Cenozoic. The results of comprehensive studies show that 10 important iron metallogenic zones can be delineated:Bolivar iron zone of Venezuela, Amapa iron zone of Brazil, Para iron zone of Brazil, Minas gerais iron zone of Brazil, Rio Grande do Norte iron zone of Brazil, balaiba iron zone of Brazil, Bahia iron zone of Brazil, Mato Grosso do Sul iron zone of Brazil, Santa Cruz iron zone of Bolivia, Ika-Arequipa iron zone of Peru, and Calama-Santiago coastal iron zone of Chile. Based on an analysis of typical deposits in important metallogenic zones and statistical analysis methods, the authors have summarized the temporal and spatial distribution regularities of iron mineralization in South America with the purpose of providing references so as to find more iron ore resources in this area in the future.
Keywords:South America  iron ore  important iron ore forming area  metallogenic regularity
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