地质通报Issue(4)：605-617,13.
俄罗斯远东东北部中生代造山带成矿地质背景--兼论鄂霍茨克-楚科奇火山深成岩带金属成矿作用
摘要
Abstract
Russian Far East area is an important endogenic metal cluster area in the world, where gold, silver, copper, tungsten, tin and some other mineral resources are extremely rich. The study area includes Verkhoyansk craton marginal zone in northeast North Asia craton,Verkhoyansk-Chukchi orogenic belt, Okhotsk-Chukchi orogenic (volcanic rock) belt, and Koryak-Sakhalin orogenic belt. In this paper, the authors briefly described regional tectonic evolution and geological setting for ore-forming processes of north⁃east Russian Far East, and summarized the ore-forming processes of main endogenic metal deposits in Okhotsk-Chukchi volcanic belt and its neighboring areas. It is considered that, in this volcanic belt, the epithermal gold-silver deposits are dominant mineral de⁃posits in the volcanic basin, whereas the porphyry copper deposits and copper-molybdenum deposits are mainly distributed in the granitoid rock area lying within the relatively upwarping place in or on the margin of the volcanic belt.关键词
远东东北部/鄂霍茨克-楚科奇/中生代造山带/成矿地质背景/金属成矿作用Key words
northeast Far East/Okhotsk-Chukchi/Mesozoic orogenic belt/metallogenic geological background/metallogenic pro cess分类
天文与地球科学引用本文复制引用
鲍庆中,周永恒,邵军,柴璐,王宏博,张璟,张哲寰..俄罗斯远东东北部中生代造山带成矿地质背景--兼论鄂霍茨克-楚科奇火山深成岩带金属成矿作用[J].地质通报,2015,(4):605-617,13.基金项目
中国地质调查局项目（编号1212011220906、1212011220912）、国土资源公益性行业科研专项（编号200811010）和国家国际科技合作项目 （）
