海南罗葵洞斑岩型钼矿地质特征及矿床成因  

Metallogenic characteristics of Luokuidong porphyry molybdenum deposit in the Baoting County,Hainan Province

作　　者：王国君 刘君 曹玉莲 张馨宁 

机构地区：[1]辽宁省有色地质局一0八队,沈阳110013

出　　处：《矿产勘查》2010年第5期453-457,共5页Mineral Exploration

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。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.

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 

分 类 号：P611[天文地球—矿床学] P618.65[天文地球—地质学]