摘要
在对该区野外地质调查的基础上,本文对该铅锌矿化带的成矿构造背景、矿化体特征进行了初步分析与总结,认为该矿受区域构造断裂控制,矿床类型为中低温热液脉状铅锌多金属矿床。该区成矿地质条件优越,矿化体较多,矿体在走向和倾向延伸方向仍可有新突破,并有找到新矿体的可能。
Based upon the field geological survey in this area, the metallogenesis structure setting and metal- logenetic body feature of this Pb-Zn metallogenesis zone are preliminarily analyzed and summed up in this pa- per. We think this orefield is controlled by regional structure fault, the ore deposit type belongs to the middle-low T veined hydrothermal Pb-Zn multimetallic deposit. The geological conditions of metallogenesis are excellent, there are many metallogenetic bodies, the orebody prospecting can achieve the new breakthrough in strike and dipping direction, and possibly find out the new orebodies.
出处
《云南地质》
2014年第1期141-143,共3页
Yunnan Geology
