| 吉林省白山市狼洞沟金银矿床地质特征及成因探讨 |
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| 引用本文： | 王兴昌,冷青林,苗迪,潘彦平.吉林省白山市狼洞沟金银矿床地质特征及成因探讨[J].吉林地质,2010,29(3):20-23,28. |
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| 作者姓名： | 王兴昌 冷青林 苗迪 潘彦平 |
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| 作者单位： | 吉林省有色金属地质勘查局六0二队,吉林白山134300 |
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| 摘 要： | 狼洞沟金银矿床是浑江古生界凹陷中发现的第二个小型矿床,通过对矿床的矿体形态﹑矿石组成﹑结构构造﹑围岩蚀变﹑硫同位素测定及矿石爆裂温度测定分析,成矿物质来源于含矿岩体和地层,在成岩成矿作用中,岩浆同熔和交代作用较强烈,其成矿期可分二期,成矿温度可划分三阶段.认为狼洞沟金银矿床是与中温浅成岩浆热液有关的裂隙充填脉状金银矿床.
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| 关 键 词： | 金银矿床 地质特征 矿床成因 狼洞沟 |
Geologic features and genesis of Langdonggou Au-Ag deposit, Baishan City of Jilin Province |
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| WANG Xing-chang,LENG Qing-lin,MIAO Di,PAN Yan-ping.Geologic features and genesis of Langdonggou Au-Ag deposit, Baishan City of Jilin Province[J].Jilin Geology,2010,29(3):20-23,28. |
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| Authors: | WANG Xing-chang LENG Qing-lin MIAO Di PAN Yan-ping |
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| Institution: | Team 602,Nonferrous Exploration Bureau of Jilin Province,Baishan 134300,Jilin,China |
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| Abstract: | Langdonggou Au-Ag deposit is the second small ore deposit in Paleozoic depression.Through the analysis of the ore body shape,ore composition,structure,wall rock alteration,S isotopic determination and ore decrepitating method,it is considered that metallogenitic material derived from the ore-bearing rock body and the stratum;in lithogenesis and mineralization,magmatic syntexis and metasomatism are relative intense,The metallogenenic epochs can be divided into two one,and the metallogenic temperature can be divided into three stages.The study shows that Langdonggou Au-Ag deposit related to mesothermal shallow-seated magmatic hydrothermalism,which belongs to fissure filling vein Au-Ag deposit. |
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| Keywords: | Au-Ag deposit geologic features genesis of deposit Langdonggou |
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