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甘肃佐家锑矿床地质特征及找矿标志

The Geological Features of Zuojia Antimony Deposit in Gansu and the Corresponding Ore Prospecting Sign

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【作者】 李有武李军

【Author】 LI You-wu;LI Jun;Tianshui Mineral Prospecting Institute of Gansu Province Bureau of Non-Ferrous Metal Geology and Exploration;

【机构】 甘肃省有色金属地质勘查局天水矿产勘查院

【摘要】 甘肃礼县佐家锑矿大地构造位置为秦岭印支褶皱带。其北以毛羽沟-寺顶山-江洛镇大断裂与华力西褶皱带相邻,南以银洞湾-铁家山-沈家院-秦家坝大断裂与加里东褶皱带接壤。矿体赋存于上三叠系三渡水组第二层(Ts3-2b)粉砂岩、细砂岩、角砾岩、硅质白云质灰岩夹板岩中。受近东西向断裂破碎带控制。文章在总结了成矿地质背景及地质特征的基础上,提出了找矿标志。

【Abstract】 The Zuojia antimony in Lixian county, Gansu province, is located in the geotectonic location is the Qinling indosin fold beltlead.The north is bordered by the Maoyugou-Teodingshan-Jiangluo town fault and the Hualixi fold belt. The south is bordered by the Yindongwan-Tiejiashan-Shenjiayuan-Qinjiaba fault and the Caledonian fold belt.The ore body is located in the second layer(Ts3-2 b) siltstone, fine sandstone, breccia and siliceous dolomitic limestone plywood of the Upper Triassic Sandu Formation. Controlled by the near-east-west fault fracture zone. Based on the summarization of ore-formation geological settings and geological features, some ore prospecting indicators are given in the essay.

  • 【分类号】P618.66
  • 【被引频次】1
  • 【下载频次】18
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