| 青海玉树赵卡隆铁铜多金属矿床地质特征及成因探讨 |
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| 引用本文： | 李欢.青海玉树赵卡隆铁铜多金属矿床地质特征及成因探讨[J].地质与勘探,2011,47(3):380-387. |
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| 作者姓名： | 李欢 |
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| 作者单位： | 1. 中南大学地质研究所,湖南长沙,410083
2. 有色金属华东地质勘查局805队,江苏南京,211500 |
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| 基金项目： | 国家自然科学基金资助项目(项目编号:40372099); 高等学校博士学科点专项科研基金(编号:20110162110054)资助 |
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| 摘 要： | 赵卡隆铁铜多金属矿床产于三叠纪末期江达弧后裂谷热水沉积盆地中,具有铁、铜、金、铅锌等多金属矿化.矿体赋存于三叠系巴塘群上部碎屑岩组上岩性段地层中,严格受地层和岩性控制.各矿(体)群根据矿体分布部位不同划分为若干条矿体.火山喷发活动(安山岩)为成矿提供了物质来源和热源,同期火山岩具有富铝钠质低钾质特征,属安山岩类-拉斑玄...
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| 关 键 词： | 铁铜多金属矿床 裂谷 安山岩 赵卡隆 三江成矿带北段 |
| 收稿时间： | 3/3/2010 12:00:00 AM |
| 修稿时间： | 2010/7/16 0:00:00 |
Geology and Metallogenesis of the Zhaokalong Iron-Copper-Polymetallic
Ore Deposit in Yushu,Qinghai Province |
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| LI Huan.Geology and Metallogenesis of the Zhaokalong Iron-Copper-Polymetallic
Ore Deposit in Yushu,Qinghai Province[J].Geology and Prospecting,2011,47(3):380-387. |
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| Authors: | LI Huan |
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| Institution: | LI Huan1,XI Xiao-shuang1,WU Cheng-ming1,Di Chun-xia2 (1. Institute of Geology,Central South University,Changsha,Hunan 410083,2.Team 805 of ECE,Nanjing,Jiangsu 211500) |
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| Abstract: | The Zhaokalong iron-copper-polymetallic deposit was produced in the back-arc rift sedimentary basin during the late Triassic,with mineralization of iron,copper,gold,lead,zinc and other metallic ores.Ore bodies lie in the clastic rock of the upper Batang Group of Triassic,strictly controlled by the stratigraphy and lithology.The ore(body) group is divided into several different belts according to the ore body distribution.Volcanic eruptions(andesite) provided the material sources and heat for the mineralizat... |
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| Keywords: | iron-copper-polymetallic deposit rift andesite Zhaokalong north part of the Sanjiang metallogenic region |
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