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Mineralization age and ore genesis of Guzhonggonglu molybdenum deposit in central-northern Great Xing'an Range
LIU Da-zhong1, HAO Yu-jie1, YANG Qun1, ZHAO Shu-yue2, REN Yun-sheng1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Qiqihaer Branch of Heilongjiang Institute of Geological Survey, Harbin 150036, China
Abstract:

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 and 11.584×10-6, 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 ore-forming fluid belongs to the medium-high temperature, and high salinity NaCl-H2O-CO2 fluid system, and the fluid 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.

Keywords: fluid inclusion   molybdenum deposit   molybdenite Re-Os dating   Guzhonggonglu   porphyry deposit  
�ո����� 2017-01-22 �޻����� 2017-04-27 ����淢������  
DOI: 10.3969/j.issn.1004-5589.2017.02.017
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