摘要
从成矿地质背景、地质概况、地球物理特征、矿产特征等方面对青海省茫崖镇红垭豁地区铜锡多金属矿进行了探讨,并进行了综合分析。研究区成矿地质条件优越,成矿事实明显,与已发现矿床有极其相似的成矿地质背景,具有很大的找矿前景。
This paper comprehensively analyzed the copper-tin polymetallic deposits located in the Hongyahuo area in Mangya Town of Qinghai Province from the aspects of metallogenic geological background, geological profile, geophysical characteristics and mineral characteristics. The geological conditions of ore-forming in the research area are superior, and the facts of ore-forming are obvious. The ore deposit has similar ore-forming geological background to the discovered deposits and has great prospecting prospects.
引文
[1]张爱奎,刘光莲,莫宣学,等.青海祁漫塔格晚古生代—早中生代侵入岩构造背景与成矿关系[J].西北地质,2012(1):9-19.
[2]余宏全,张德全,景向阳,等.青海省乌兰乌珠尔斑岩铜矿床地质特征及成因[J].中国地质,2007,34(2):306-314.