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《Global Geology》 2017-02
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Mineralization age and ore genesis of Guzhonggonglu molybdenum deposit in central-northern Great Xing'an Range

LIU Da-zhong;HAO Yu-jie;YANG Qun;ZHAO Shu-yue;REN Yun-sheng;College of Earth Sciences,Jilin University;Qiqihaer Branch of Heilongjiang Institute of Geological Survey;  
The ore-hosting intrusion of Guzhonggonglu molybdenum deposit is the fragmented silication gneissic monzogranite,and the alterations are distributed in belt.The metallogenic process can be divided into K-feldspar + quartz,quartz + molybdenite and quartz + pyrite stages.The Re-Os isotope model age of two molybdenite samples are(142.4 ± 2.9) Ma and(142.3 ± 2.0) Ma,respectively,indicating that the deposit was caused by the Early Cretaceous tectonic-magmatic activities.The content of Re in the molybdenite are 11.894 × 10~(-6)and11.584 × 10~(-6),respectively,suggesting that the ore-forming materials are mainly derived from the crust,and probably affected by the mantle.The preliminary study of fluid inclusions demonstrates that the fluid inclusions in the quartz are mainly gas-liquid two phase inclusions,secondly gas-liquid-solid three phase inclusions,minor CO2-bearing three phase inclusions.The homogenization temperature of all type of inclusions are of 196.3 ~ 450℃,while the salinities can be divided into two groups:0.18% ~ 12.62% and 45.33% ~ 53.26%.Thus,the oreforming fluid belongs to the medium-high temperature,and high salinity Na Cl-H2O-CO2 fluid system,and thefluid boiling might occur during the ore-forming stage and be the major metallogenic mechanism.Combined with the characteristics of ore-forming conditions,ore deposit geology and fluid inclusions,the study indicate that the Guzhonggonglu molybdenum deposit is of porphyry type,and formed under a regional extension tectonic settings.
【Fund】: 基金项目:古亚洲构造域成矿背景与成矿机制(2013CB429802)
【CateGory Index】: P618.65;;P597
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