云南元阳大坪金矿床成因及找矿方向

金属矿山 ›› 2016, Vol. 45 ›› Issue (03): 113-118.

云南元阳大坪金矿床成因及找矿方向

李兴俭¹，张达¹，张垚垚¹，狄永军¹，刘军²，卜星辰¹

1.中国地质大学（北京）地球科学与资源学院，北京 100083；2.元阳县华西黄金有限公司，云南红河 662406

出版日期:2016-03-15 发布日期:2016-05-17

Metallogenesis and Prospecting Direction of the Daping Gold Deposit in Yuanyang County，Yunnan Province

Li Xingjian¹，Zhang Da¹，Zhang Yaoyao¹，Di Yongjun¹，Liu Jun²，Bu Xingcheng¹

1.School of Earth Sciences and Resources，China University of Geosciences (Beijing)，Beijing 100083，China；2.Yuanyang Huaxi Gold Mining Co.，Ltd.，Honghe 662406,China

Online:2016-03-15 Published:2016-05-17

摘要/Abstract

摘要： 大坪金矿床为哀牢山金矿带的典型矿床之一，被视为产于碰撞造山环境下的金多金属矿床。为进一步查明矿床成因类型，结合区域成矿背景，以云南省元阳县大坪金矿床地质勘查成果为依据，深入分析了典型矿床的地质特征、矿物组合特征、围岩蚀变特征，划分了成矿期次，并对成矿物质基础研究成果和控矿构造特征进行了总结，结果表明：①矿床主要受左行走滑剪切作用控制，矿体主要赋存于张扭性-压扭性空间过渡部位。②矿床成矿物质来源多样，受多期次构造成矿作用、多成因热流体综合作用叠加改造，属中温热液脉型金多金属矿床。在上述研究成果的基础上，对区内找矿标志及找矿方向进行了讨论，认为区内找矿工作应在富碱斑岩发育和构造活动叠加的地区进行，重点找矿部位为煌斑岩和花岗斑岩出露地带，另外应注意多金属硫化物的富集部位。上述研究成果对于矿区深部找矿预测有一定的参考价值。

关键词: 矿体特征, 矿床成因, 围岩蚀变, 成矿期次, 找矿标志, 找矿方向, 深部找矿

Abstract: Daping gold deposit is one of the typical deposits in the Ailaoshan metallogenic belt，it is regarded as the vein-type gold poly-metallic sulfide deposit that is commonly developed in close association with the product of collision orogenic environment.In order to analyze the deposit genesis types of the Daping gold deposit in Yuanyang county,Yuannan province,based on the regional metallogenic background and the geological exploration results of the Daping gold deposit in Yuanyang county,Yunnan province,the typical deposit geological characteristics,mineral assemblage characteristics and wall rock alteration characteristics are discussed in depth,the metallogenic period is divided,besides that,the basic research results of the ore-forming materials and ore-controlling tectonic characteristics are also analyzed in detail.The results show that:①the gold deposit is controlled by sinistral strike-slipping shear,the main ore-bodies are developed in the transition part of tense-compression shearing space.②the metallogenic material source is varied,they are affected by multi-phase tectonic mineralization and superposition reconstructed by poly-genetic thermal fluid combination,so,the Daping gold deposit in Yuanyang county,Yunnan province is a vein-type poly-mental deposit with middle temperature.Based on the above research results,the prospecting indicators and prospecting direction in the mining area are discussed,the result show that the prospecting work in the mining area should be conducted in the area where the alkali-rich porphyry is developed and tectonic activities superposition,the key prospecting portion is the area where the lamprophyre and granite porphyry are exposed,in addition,the poly-metallic sulfide enrichment places should also be paid attention.The above research results can provide reference for the further deep prospecting and prediction in the mining area.

Key words: Ore-body characteristics, Deposit genesis, Wall rock alteration, Metallogenic period, Prospecting indicators, Prospecting direction, Deep prospecting

李兴俭, 张达, 张垚垚, 狄永军, 刘军, 卜星辰. 云南元阳大坪金矿床成因及找矿方向[J]. 金属矿山, 2016, 45(03): 113-118.

LI Xing-Jian, ZHANG Da, ZHANG Yao-Yao, DI Yong-Jun, LIU Jun, BU Xing-Chen. Metallogenesis and Prospecting Direction of the Daping Gold Deposit in Yuanyang County，Yunnan Province[J]. Metal Mine, 2016, 45(03): 113-118.

[1]	田九玲. 基于证据权模型的赤峰—呼伦贝尔成矿带找矿预测[J]. 金属矿山, 2020, 49(09): 167-172.
[2]	刘大勇, 彭桥梁, 苏特. 万家坪锰矿地质地球化学特征及找矿远景[J]. 金属矿山, 2020, 49(08): 119-128.
[3]	张恺, 毛瑞芬, 李琛, 范晓磊. 河南省大古石沟地区地质特征及铅锌矿找矿方向[J]. 金属矿山, 2020, 49(07): 130-137.
[4]	刘幼建, 谢焱石, 谭凯旋, 韩世礼, 王鹏, 康春晖. 深部元素地气迁移的分量化探证据：以郴州金狮岭铀多金属矿床为例[J]. 金属矿山, 2020, 49(07): 146-154.
[5]	占文锋, 王强, 刘太福. 内蒙古维拉斯托矿区隐伏矿体大功率激电综合找矿勘查[J]. 金属矿山, 2020, 49(04): 118-129.
[6]	魏均启, 戚新世, 周玉华, 王芳, 朱丹, 鲁力. 鄂东南鸡冠嘴铜金矿床黄铁矿特征及深部成矿潜力[J]. 金属矿山, 2019, 48(11): 132-141.
[7]	杨瑞西, 许国丽, 楚卢凯, 蔡仲明, 刘百顺. 河南郁山—礼庄寨地区铝土矿重力-CSAMT综合成矿预测[J]. 金属矿山, 2019, 48(09): 113-122.
[8]	李万忠, 方怀宾, 柴重阳, 李珂莹. 河南栾川大竹园沟钨钼矿区地质特征及找矿远景[J]. 金属矿山, 2019, 48(09): 123-131.
[9]	李进喜, 方怀宾, 曹宇岗, 黄正将, 程远秋, 赵德鑫, 高强. 内蒙古边墙里矿区银铜铅锌矿床成矿地质条件及找矿模型[J]. 金属矿山, 2019, 48(09): 132-140.
[10]	黄涛. 安徽省马鞍山市象塘铁矿地质特征及成因[J]. 金属矿山, 2019, 48(09): 141-146.
[11]	魏军, 王恩德, 刘福兴, 王伟. 辽宁凤城白云金矿带地质特征、矿床成因及找矿方向[J]. 金属矿山, 2019, 48(08): 120-130.
[12]	陈建立, 郭鹏, 陈英男, 赵焕, 魏从玲, 张宏燕. 豫西南老湾金矿原生晕地球化学特征及深部成矿预测[J]. 金属矿山, 2019, 48(07): 124-134.
[13]	胡加昆, 陶猛, 王远高, 赵福国, 杨福全, 李应武. 云南省会泽县大水井铅锌矿成矿规律及找矿预测[J]. 金属矿山, 2019, 48(07): 135-144.
[14]	巩庆伟, 黄正将, 巩一帆, 程远秋, 易和朝. 内蒙古温都尔各脱铅锌矿矿床地质特征及综合找矿模型[J]. 金属矿山, 2019, 48(07): 145-152.
[15]	胡加昆, 邹进超, 解康, 倪尔建, 李贵祥, 李星. 云南省江城县岩脚—牛倮河铅锌矿矿床成因及找矿方向[J]. 金属矿山, 2019, 48(05): 93-106.