葛治勋,陈碧华.内蒙古温格哈尔金矿床物化探异常及地质成矿浅析[J].地质找矿论丛,2018,33(1):134-141 |
内蒙古温格哈尔金矿床物化探异常及地质成矿浅析 |
Geophysical and geochemical anomlies at Inner Mongolian Wengerhar gold mine and discussion on geological mineralization |
投稿时间:2017-10-17 修订日期:2017-11-27 |
DOI:10.6053/j.issn.1001-1412.2018.01.017 |
中文关键词: 温格哈尔金矿床 温都尔庙群 绿片岩 地球化学Au异常 内蒙古 |
英文关键词:Wengerhar gold mine Wenduewrmiao group green schist geochemical Au anomaly Inner Mongolia |
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中文摘要: |
温格哈尔金矿床位于内蒙古乌拉特中旗巴音杭盖苏木境内。区内出露地层为古元古界宝音图群(Pt1BY)上部石英岩、大理岩,中上元古界温都尔庙群绿片岩(Jxhr),志留系哈达呼舒群(S1-2HD)含石榴角岩、千枚岩和变质砂岩,侵入岩以海西期二长花岗岩、石英闪长岩、斜长花岗岩为主。通过对温格哈尔金矿勘查区1:1万物化探工作、异常查证和地质综合评价,在勘查Ⅰ区内圈定金矿化体20余条,并认为该金矿是与都尔庙群绿片岩有关的热液型金矿。 |
英文摘要: |
At The Inner Mongolian Wengerhar gold mine are mainly exposed the quartzite and marble in the upper Palaeo-proterozoic Baoyintu Group (Pt1BY), green schist of the Middle-Upper Proterozoic Wenduermiao Group (Jxhr), the garnet hornstone, phyllite and metamorphosed sandstone of Silurian Hadahushu Greoup(S1-2hd) and the intrusive rocks dominated by the Hercynian monzonitic granite, quartz diorite and plagioclase granite. Based on geophysical and geochemical survey at scale 1:10000, check of anomlies and geological synthetic assessment 20 mineralized bodies are located in prospecting area I and the Wengerhar gold deposit is considered a hydrothermal one related to green schist of Wenduermiao Group (Jxhr). |
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