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西藏羌堆斑岩-夕卡岩复合型铜矿地质特征及找矿前景
引用本文:江善元,陈自康,韩逢杰.西藏羌堆斑岩-夕卡岩复合型铜矿地质特征及找矿前景[J].地质找矿论丛,2006,21(Z1):22-26.
作者姓名:江善元  陈自康  韩逢杰
作者单位:中国冶金地质勘查工程总局,第二地质勘查院,福建,莆田,351111
基金项目:中国地质调查局地质调查项目
摘    要:羌堆铜矿位于冈底斯斑岩型铜(钼)成矿带中东段的拉抗俄-吹败子铜(钼)矿集区内,是斑岩-夕卡岩复合型矿床,含矿斑岩体为花岗斑岩及石英斑岩,具全岩矿化特征,斑岩体与白垩系门中组灰岩的接触带形成夕卡岩型矿床.研究表明,地表和浅部出露的含矿斑岩体只是其岩枝,矿床剥蚀程度低,主斑岩体尚未出露,深部找矿潜力巨大.

关 键 词:羌堆铜矿  斑岩-夕卡岩复合型矿床  找矿前景  西藏自治区
文章编号:1001-1412(2006)S0-0022-05
修稿时间:2005年11月28

GEOLOGICAL CHARACTERISTICS AND POTENTIAL OF QIANGDUI PORPHYRY-SKARN COMPLEX COPPER DEPOSIT IN TIBET
JIANG Shan-yuan,CHENG Zi-kang,HAN Feng-jie.GEOLOGICAL CHARACTERISTICS AND POTENTIAL OF QIANGDUI PORPHYRY-SKARN COMPLEX COPPER DEPOSIT IN TIBET[J].Contributions to Geology and Mineral Resources Research,2006,21(Z1):22-26.
Authors:JIANG Shan-yuan  CHENG Zi-kang  HAN Feng-jie
Abstract:Qiangdui copper deposit is a porphyry-skarn complex copper(molybdenum) deposit located at the copper(molybdenum) deposit-concentrated Lahange-Cuibaizi area in the central east Gangdise porphyry copper(molybdenum) ore belt.The host rock is granitic porphyry and quartz porphyry which are wholly mineralized. The skarn copper(molybdenum) deposit occurs at the contact zone of the porphyry and limestone of Cretaceous Menzhong Formation.Our study reveals that the ore-bearing porphyry exposed at surface is only the apophyses and intense erosion did not take place thus the main porphyry are still at depth and it is potential for discovering big porphyry deposit to depth.
Keywords:Qiangdui copper deposit  the porphyry-skarn complex copper(molybdenum) deposit  ore potential  Tibet
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