| 刘悟辉,戴塔根,廖启林.新疆富蕴县乔夏哈拉铜(金)矿床成因探讨[J].地质找矿论丛,2006,(4):232-235,252 |
| 新疆富蕴县乔夏哈拉铜(金)矿床成因探讨 |
| DISCUSSION ON GENESIS OF QIAOXIHALA COPPER-(GOLD) ORE DEPOSIT,FUYUN COUNTY,XINJIANG |
| 投稿时间：2005-11-08 修订日期：2006-04-04 |
| DOI：10.6053/j.issn.1001-1412.2006.4. 002 |
| 中文关键词: 乔夏哈拉金(铜)矿床 矿床成因 火山喷流沉积 层控夕卡岩 新疆 |
| 英文关键词:Qiaoxiahala Cu(Au) deposit ore genesis volcanic Sedex stratabound skarn Xinjiang |
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| 中文摘要: |
| 新疆乔夏哈拉铜(金)矿床的成因前人认识不一。文章通过成矿环境、成矿规律、火山成矿作用及成矿物质来源等分析研究,认为矿床为产于陆缘裂谷带中的火山岩块状硫化物层控矿床,层状夕卡岩直接控制矿体,成矿物质源于上地慢或深部地壳,成矿热液主要来自火山热液加大气降水,属于海相火山岩喷流沉积成因的层控夕卡岩型铜(金)矿体。 |
| 英文摘要: |
| It is controversial for genesis of Qiaoxiahala Cu(Au) deposit.Through researches on metallogenic environment,regularity,volcanic metallogeny and ore material sources it is concluded that the deposit is a volcanic massive sulfide deposit formed in rift.Ore bodies are controlled by layered skarn.Ore materials come from upper mantle or deep crust and ore fluid is volcanic hydrothermal fluid incorporated with meteoric water.Genetically,it is a marine volcanic Sedex stratabound skarn Cu(Au) deposit. |
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