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新疆东部马庄山金矿成矿作用同位素年代学研究
引用本文:李华芹,陈富文.新疆东部马庄山金矿成矿作用同位素年代学研究[J].地质科学,1999,34(2):251-256.
作者姓名:李华芹  陈富文
作者单位:中国地质科学院同位素研究与测试中心 宜昌 443003
基金项目:国家305项目,国家自然科学基金
摘    要:马庄山金矿位于新(疆)甘(肃)边境。地质、地球化学研究表明,马庄山金矿床受马庄山古火山机构控制,与矿区内同期火山-次火山作用有直接的成因联系,成因类型为浅成中-低温热液型。次火山岩及含金石英脉年代学研究表明,马庄山火山机构形成时代与金矿成矿时代均为中-晚石炭世:次流纹斑岩和次英安斑岩全岩及含金石英细(网)脉石英流体包裹体Rb-Sr等时线年龄分别为301±21Ma、303Ma±26Ma和298Ma±28Ma(95%置信度)。

关 键 词:金成矿作用  同位素年代学  马庄山  新疆东部
收稿时间:1998-06-25
修稿时间:1998-06-25;

STUDY ON ISOTOPIC CHRONOLOGY OF THE MAZHUANGSHAN GOLD MINERALIZATION,EASTERN XINJIANG
Li Huaqin,Chen Fuwen,Cai Hong,Liu,Houqun.STUDY ON ISOTOPIC CHRONOLOGY OF THE MAZHUANGSHAN GOLD MINERALIZATION,EASTERN XINJIANG[J].Chinese Journal of Geology,1999,34(2):251-256.
Authors:Li Huaqin  Chen Fuwen  Cai Hong  Liu  Houqun
Institution:Center of Isotopic Research and Dating; Yichang Institute of Geology and Miner al Resources, Chinese Academy of Geological Sciences(CAGS), Yichang, Hubei Province, 443003
Abstract:Located geographically in the border of Xinjiang Uygur Autonomous Region and Gansu Province and geologically in the juncture of the Siberian, T arim, Kazakhstan and Sino Korean palaeoplate, the Mazhuangshan paleovolcanic apparatus is a typical ore-control one in eastern Xinjiang. Geological and geoche mical evidence indicates that the Manzhuangshan gold deposit, a volcanogenic one, shows direct genetic relationship with contemporary volcanic-subvolcanic activities and is controlled by the Manzhuangshan paleovolcanic apparatus. chronological study on subvolcanic rocks and gold bearing gold veins show that both the paleovolcanic apparatus and the gold deposit were formed during the Middle Carbo niferous with the Rb-Sr isochron ages of rhyolite porphyry, dacite porphyry and fluid inclusions of quartz from the gold-bearing quartz veins to be 301?21Ma, 303?26 Ma and 298?28 Ma (95% confidence), respectively.
Keywords:Gold Mineralization  Isotope Chronology  Mazhuangshan  Eastern Xinjiang  
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