文章摘要
王国君,刘君,曹玉莲,张馨宁.海南罗葵洞斑岩型钼矿地质特征及矿床成因[J].矿产勘查,2010,1(5):453-457
海南罗葵洞斑岩型钼矿地质特征及矿床成因
Metallogenic characteristics of Luokuidong porphyry molybdenumdeposit in the Baoting County,Hainan Province
投稿时间:2009-12-25  
DOI:
中文关键词: 罗葵洞  钼矿  中浅成侵入岩  火山机构  大型斑岩钼矿床
英文关键词: molybdenum deposit  shallow-middle intrusive rock  volcanic mechanism  large porphyry molybdenum deposit  Luokuidong
基金项目:
作者单位
王国君 辽宁省有色地质局一0八队, 沈阳 110013 
刘君 辽宁省有色地质局一0八队, 沈阳 110013 
曹玉莲 辽宁省有色地质局一0八队, 沈阳 110013 
张馨宁 辽宁省有色地质局一0八队, 沈阳 110013 
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中文摘要:
      罗葵洞钼矿区位于海南省南端,测区出露的岩石为一套与火山机构有关的中酸性火山岩、火山碎屑岩及浅至中深成侵入岩。钼矿赋存在隐伏似斑状花岗岩顶部及其外带火山岩中,是一处受中浅成侵入岩及火山机构联合控制的大型斑岩钼矿床。
英文摘要:
      Luokuidong molybdenum deposit, which is found through stream sediment survey, is situated in southern end of Hainan Province. It is believed that the rock exposed in the working area belongs to acidic volcanic rocks, pyroclastic and shallow to middle intrusive rocks, which are related with volcanic mechanism. The molybdenum deposit, located at the top concealed porphyritic granite and the exterior volcanic rocks, is a large porphyry molybdenum deposit jointly controlled by shallow to middle intrusive rocks and volcanic mechanism. 
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