[an error occurred while processing this directive] 世界地质 2020, 39(3) 557-568 DOI:   10.3969/j.issn.1004-5589.2020.03.005  ISSN: 1004-5589 CN: 22-1111/P
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本文关键词相关文章
流体包裹体测温
气相成分
漠河推覆构造
前哨林场锑金矿
本文作者相关文章
陆胜
王可勇
张涵远
赵焕利
相雷
刘阳
张志博
PubMed
Article by Lu S
Article by Wang K
Article by Zhang H
Article by Zhao H
Article by Xiang L
Article by Liu Y
Article by Zhang Z
黑龙江漠河推覆带前哨林场锑金矿床流体包裹体特征及其地质意义
陆胜1, 王可勇2, 张涵远3, 赵焕利4, 相雷1, 刘阳1, 张志博1
1. 黑龙江省第五地质勘查院, 哈尔滨 150090;
2. 吉林大学地球科学学院, 长春 130061;
3. 辽宁省冶金地质四〇四队有限责任公司, 辽宁辽阳 111000;
4. 黑龙江省地质矿产局, 哈尔滨 150300
摘要： 从矿床地质出发，报道了大兴安岭漠河地区前哨林场锑金矿的流体包裹体岩相学、显微测温及气相成分，探讨了前哨林场锑金矿床流体包裹体性质、成岩成矿时间及空间分布特征。研究结果表明：其成矿过程经历灰白色石英-黄铁矿阶段（Ⅰ）、灰黑色石英-辉锑矿-黄铁矿阶段（Ⅱ）及乳白色石英-少硫化物-碳酸盐阶段（Ⅲ）等3个阶段；矿物流体包裹体类型以气液两相型包裹体为主，并含少量CO2三相包裹体，成矿流体应为中低温、低盐度的H2O-CO2-NaCl体系热液，现阶段所卸载的矿（化）体为主成矿晚期的矿体，该期矿体的西北部找矿潜力较大；结合矿区地质特征，初步认为其形成于晚侏罗世晚期—早白垩世。
关键词： 流体包裹体测温   气相成分   漠河推覆构造   前哨林场锑金矿  
Characteristics of fluid inclusions and geological significance of Qianshao forest farm Sb-Au deposit in Mohe nappe structure, Heilongjiang
LU Sheng1, WANG Ke-yong2, ZHANG Han-yuan3, ZHAO Huan-li4, XIANG Lei1, LIU Yang1, ZHANG Zhi-bo1
1. The Fifth Geological Prospecting Institute of Heilongjiang Province, Harbin 150090, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, China;
3. Liaoning Metallurgical Geology Team 404 Co., Ltd, Liaoyang 111000, Liaoning, China;
4. Bureau of Geology and Mineral Resources of Heilongjiang Province, Harbin 150300, China
Abstract: Based on the geology of the deposit, the authors report herein the petrographic, microscopic temperature measurement and vapor phase composition of fluid inclusions of Qianshao forest farm Sb-Au deposit in Mohe area of Great Xing'an Range, and discuss the characteristics of fluid inclusions, time and spatial distribution of diagenesis and mineralization in Qianshao forest farm Sb-Au deposit. Results show that the ore-forming process experienced three stages: gray white quartz-pyrite stage (Ⅰ), gray black quartz-stibnite-pyrite stage (Ⅱ) and milky white quartz-less sulfide-carbonate stage (Ⅲ). The mineral fluid inclusions are mainly gas-liquid two-phase inclusions, and small amount of contain CO2 three-phase inclusions. The ore-forming fluid should be the medium-low temperature and low salinity hydrothermal solution of the H2O-CO2-NaCl system. The ore bodies unloaded at this stage are the late stage of main metallogenic, and the northwest part of the ore bodies in this stage has great prospecting potential. According to the geological characteristics of the mining area, it is preliminarily considered that it was formed in the late Late Jurassic-Early Cretaceous.
Keywords: fluid inclusions temperature measurement   vapor phase composition   Mohe nappe structure   Qianshao forest farm Sb-Au deposit  
收稿日期 2020-06-29 修回日期 2020-08-06 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2020.03.005
基金项目:

中国地质调查局项目（2017YFC0601304）

通讯作者: 张涵远(1987-),女,硕士,工程师,主要从事地质矿产方面的研究。E-mail:742934556@qq.com
作者简介:
作者Email: 742934556@qq.com
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