Wechat
J4 ›› 2011, Vol. 19 ›› Issue (5): 7-10.
• article • Previous Articles Next Articles
XIE Qinjiang,FANG Yuexin
Received:
Revised:
Online:
Published:
Abstract:
Mulutang gold deposit is located in the holding location of Ailaoshan and Tengtiaojiang fault,the fracture is general development in this area,which provides a good channel and place for enrichment of gold.The magmatic activity is strong in this area,which has the characteristics of multi-phase and multi-stage acitivities,and undergo three major magmatic activity periods,inclulding Lvliang,Variscan and Indosinian period,also provides sufficient material source and thermal power for mineralization.We think that pyrite,arsenopyrite and silicification alteration are related to gold mineralization by summarizing geological characteristics and wall rock alteration of the deposit,we infer that genesis is structure altered rock type and secondary oxidized.In addition,we delineat favorable abnormal area by geophysical and geochemical explorating,and suggest that this area has better prospecting.
Key words: Geological characteristics, Genesis, Magmatic activity, Malutang gold mine, Yunnan Province
CLC Number:
XIE Qinjiang,FANG Yuexin. Discussion on the Geological Characteristics and Genesis of Malutang Gold Deposit,Yunnan Province[J].J4, 2011, 19(5): 7-10.
0 / / Recommend
Add to citation manager EndNote|Reference Manager|ProCite|BibTeX|RefWorks
URL: http://www.goldsci.ac.cn/EN/
http://www.goldsci.ac.cn/EN/Y2011/V19/I5/7
[1]李文昌,莫宣学.西南“三江”地区新生代构造及其成矿作用[J].云南地质,2001,20(4):333-346. [2]宋梦麟,易恪刚,谢覃江.云南省马鹿塘矿区及外围岩金普查[R].宁乡:武警黄金第十支队,2002 [3]张玉泉,谢应雯,涂光炽.哀牢山—金沙江富碱侵入岩及其与裂谷构造关系初步研究[J].岩石学报,1987,(1):17-25. [4]沈敢富,吕伯西.西南三江地区新生代侵入岩的成岩与成矿[M ].北京:地质出版社,2002. [5]李树海,王迎春.云南省马鹿塘矿区及外围岩金普查报告[R].宁乡:武警黄金第十支队,2009. [6]刘海兴,宋梦麟,李树海.滇黔桂细浸染型金矿地质特征及找矿标志[R].宁乡:武警黄金第十支队,2005. [7]韦龙明.秦岭地区和滇黔桂接壤区微细浸染型金矿地质地球化学特征对比[J].黄金科学技术,1995,3(5):49-52. [8]谢覃江,皮清明.云南马鹿塘金矿床地质特征及找矿远景[J].四川地质学报,2006,(3):138-140.
Cited