摘要
驼路沟钴矿床位于东昆仑南部昆南陆缘活动造山带的中段,是近年来发现的容矿于奥陶-志留纪火山-沉积岩系中的喷流沉积型钴矿床。东昆仑造山带是一个多旋回造山带,多期变形-变质作用使该矿床经历了成矿及成矿后的改造作用,使矿体分布和成因复杂化。本文从矿床地质特征、地球化学异常及其成因,分析其找矿前景,认为南矿带矿段间及深部、北矿带西段和外围AS04异常区找矿潜力大、前景较好,通过进一步工作,有望使该矿床达到大型矿床规模。
Tuolugou cobalt ore deposits located in the south east kunlun, The south margin activities through the middle of the orogenic belt, In recent years is found let mine in ordovician of volcanic sedimentary beings - in the department of Spra- ying flow type cobalt ore deposits. East kunlun orogenic belt is a polycyclic orogenic stage, the deformation - metamorphism deposit metallogenic experience after the renovation and mineralization, ore formation and distribution to complicate. From this geological features, from the geochemical anomalies and causes, and analyzes its prospecting, ore belt between the south and the north of deep, ore belt and peripheral AS04 his-pei ore-prospecting potential abnormal area, further work is good, through the deposits, is expected to reach a large scale deposits.
出处
《甘肃冶金》
2010年第1期70-74,共5页
Gansu Metallurgy
基金
国土资源大调查矿产资源评估及青海省地质勘查基金项目部分成果
关键词
钴矿床
地质特征
地球化学异常
找矿前景
驼路沟
青海
cobalt ore deposits
geological characteristics
the geochemical anomalies
prospecting propects
Tuolugou
Qing- hai
