| 吉林山门银金矿床地质特征 |
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| 引用本文： | 冯守忠,冯淼.吉林山门银金矿床地质特征[J].地质与资源,2000,9(1):15-19. |
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| 作者姓名： | 冯守忠 冯淼 |
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| 作者单位： | 1. 吉林矿产地质研究所, 吉林 长春 130012;2. 吉林大学, 吉林 长春 130012 |
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| 摘 要： | 山门银金矿床为浅成低温热液型矿床,贫硫化物型矿石.银矿物有自然银、辉银矿、锌银黝铜矿、深红银矿、硫砷铜银矿、硫锑铜银矿、马硫铜银矿、硫铜银矿.矿化分6个阶段.成矿温度为110~160℃.成矿时代燕山晚期.
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| 关 键 词： | 山门银金矿床 矿床成因 矿床特征 吉林省 |
| 文章编号： | 1002-4182(2000)01-0015-05 |
| 收稿时间： | 1999-05-12 |
| 修稿时间： | 1999-05-12 |
GEOLOGICAL FEATURES OF SHANMEN Ag-Au DEPOSIT |
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| FENG Shou-zhong,FENG Miao.GEOLOGICAL FEATURES OF SHANMEN Ag-Au DEPOSIT[J].Geology and Resources,2000,9(1):15-19. |
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| Authors: | FENG Shou-zhong FENG Miao |
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| Institution: | 1. Jilin Research Institute of Geology for Mineral Resources, CNNC, Changchun 130012, China;2. Jilin University, Changchun 130012, China |
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| Abstract: | The ore bodies of Shanmen Ag Au deposit is located in the internal and external contact zones,of which Shifeng formation of Ordovician System is overlapped by granodiorite of Indo China Epoch The ore bodies are controlled by NNE trending faults The metallogenesis of the deposit is related to magmatic hydrothermal fluid with multistage ore forming processes The stratabound deposit can be classified as broken altered rock type ore with mainly mid low temperature hydrothermal fluid filling |
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| Keywords: | Shanmen Ag Au deposit metallogenesis feature of deposit Jilin Province |
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