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锡霍特-阿林成矿带金属矿床成矿作用的演化
引用本文:冯坚,梁一鸿,刘雪松,李敏,秦亚.锡霍特-阿林成矿带金属矿床成矿作用的演化[J].地质与资源,2012,21(3):266-270.
作者姓名:冯坚  梁一鸿  刘雪松  李敏  秦亚
作者单位:1. 吉林大学 地球科学学院, 吉林 长春 130061;2. 吉林大学 地质博物馆, 吉林 长春 130026
摘    要:锡霍特-阿林构造带由兴凯地块、老爷岭-格罗杰科岛弧和东锡霍特-阿林造山带3个构造单元组成.其金属矿床成矿作用可分为3期:里菲纪末期至志留纪末,在兴凯区形成了喷流-沉积为主的铁(锰)矿、铅锌矿及岩浆热液型锡矿;二叠纪中期,在老爷岭-格罗杰科岛弧地区形成了浅成低温热液型金(银)矿和变质热液型金矿;侏罗纪至古近纪末,在东锡霍特-阿林构造带中形成了夕卡岩型钨床、浅成低温热液型金(银)矿、夕卡岩型及脉状硼矿和铅锌矿、脉状金矿等矿床.

关 键 词:锡霍特-阿林成矿带  金属矿床类型  构造演化  成矿作用演化  
收稿时间:2011-12-15

EVOLVEMENT OF THE METALLIC MINERALIZION IN THE SIKHOTE-ALIN METALLOGENIC PROVINCE
FENG Jian , LIANG Yi-hong , LIU Xue-song , LI Min , QIN Ya.EVOLVEMENT OF THE METALLIC MINERALIZION IN THE SIKHOTE-ALIN METALLOGENIC PROVINCE[J].Geology and Resources,2012,21(3):266-270.
Authors:FENG Jian  LIANG Yi-hong  LIU Xue-song  LI Min  QIN Ya
Institution:1. College of Earth Sciences, Jilin University, Changchun 130061, China;2. The Museum of Geology, Jilin University, Changchun 130026, China
Abstract:There Sikhote-Alin tectonic belt is composed of three tectonic units, i.e. Khanka massif, Laoyeling-Grodekovo island arc and East Sichote-Alin orogenic belt. The evolvement of metallic mineralization in the region can be divided into three periods. From the end of Riphean to the end of Silurian, iron (manganese) deposits and lead-zinc deposits were formed by exhalative-sedimentary mineralization in Khanka area, with also some magmatic hydrothermal tin deposits. During Middle Permian, epithermal gold (sliver) deposits, as well as metamorphic-hydrothermal gold deposits, were formed in Laoyeling-Grodekovo island are region. Through Jurassic to the end of Paleogene, skarn type tungsten deposits, epithermal gold (sliver) deposits, skarn and vein types of boron and lead-zinc deposits, and vein gold deposits were formed in the East Sikhote-Alin tectonic belt.
Keywords:Sikhote-Alin metallogenic province  types of metallic deposits  tectonic evolution  evolvement of mineralization
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