海南王五-文教深大断裂带西南侧铷矿成矿(矿化)规律的认识  

Understanding of Ru metallogenic(mineralization)law on the southwest side of the Wangwu-Wenjiao deep fault zone in Hainan

作　　者：黄仕锐 邓开章 孙龙飞 HUANG Shirui;DENG Kaizhang;SUN Longfei(Marine Geological Institute of Hainan Province,Haikou 570206,China)

机构地区：[1]海南省海洋地质调查研究院,海南海口570206

出　　处：《中国矿业》2020年第S02期205-207,214,共4页China Mining Magazine

基　　金：海南省财政厅划拨专项地质勘查基金项目“海南岛北部王五-文教深大断裂带西段南侧加来地区稀有金属矿产资源预查-普查”资助。

摘　　要：海南岛北部王五-文教深大断裂带西南侧加来勘查区位于洛基-南丰-仁兴多金属成矿远景区,勘查区内矿产资源丰富,西部为洛基-南丰金、锡、铌、钽矿鼓励勘查区,南侧为南报-仁兴金、银矿鼓励勘查区。本文结合勘查区大地构造位置,地球化学背景,地层、构造、岩浆岩条件及岩浆岩的含矿性,提出勘查区铷矿成矿(矿化)规律特征的四点认识,为该区域铷矿的下一地质找矿工作提供帮助。The Jialai area on the southwes side of the Wangwu-Wenjiao deep fault zone in the northern part of Hainan is located in the Luoji-Nanfeng-Renxing polymetallic mineralization prospective area.The exploration area is rich in mineral resources,and the west is Luoji-Nanfeng Gold,the prospecting area for tin,niobium and tantalum mines is encouraged,and the Nanbao-Renxing gold and silver mines are encouraged to be explored to the south.Based on the geotectonic location,geochemical background,stratum,structure,magmatic rock conditions,and ore-bearing properties of magmatic rocks in the exploration area,this paper proposes four preliminary understandings of the regular characteristics of rubidium metallogenic(mineralization)in the exploration area.Provide help for the next geological prospecting work of the mine.

关 键 词：王五-文教深大断裂带 铷矿 岩浆岩的含矿性 成矿(矿化)规律 海南 

分 类 号：P612[天文地球—矿床学]