山东国土资源Issue(12)：11-16,20,7.
内蒙古阿巴嘎旗必鲁甘干钼矿区地质特征及矿床成因浅析
王啟宴 1李山1
作者信息
- 1. 山东省第六地质矿产勘查院，山东 招远 265400
- 折叠
摘要
Abstract
According to traditional tectonic theory,tectonic position of Bilugangan molybdenum deposit in Abagaqiin Inner Mongoliain locates in Tianshan Inner Mongolia geosynclinal fold system,middle part of late Variscan fold belt,middle part of Abagaqi synclinorium which is the third tectonic unit,and core part of Chagan'aobo overturned anticline.Regional tectonic movements are mainly composed of late Variscan and Indosinian tectonic movements.Triassic intrusive rocks granite porphyry is closely related with min-eralization.Original magma in the deep part of crust intruded in sandy slate and mixed conglomerate rocks, <br> and country rocks have been eroded into all kinds of hornfels eclipse.After differentiation,ore forming materials have been concentrated largely and formed mineralization mother rock after condensation.Host structure will provide favorable space for migration,filling and replacement and mineral precipitation of ore bearing hydrothermal.Its mineralization range will be strictly controlled by hydrothermal alteration range.Multiple pulsation of hydrothermal has controlled multi stage mineralization of hydrothermal al-teration.Superimposed parts are favorable for mineralization and ore enrichment.It is regarded that in the inner and outer contact zone of granitic porphyry and its country rocks,porphyry molybdenum deposit can be formed easily.关键词
钼矿床/地质特征/矿床成因/控矿因素/必鲁甘干/内蒙古Key words
Molybdenum deposit/geological characteristics/deposit origin/ore controlling factors/Bilu-gangan area/Inner Mongolia分类
天文与地球科学引用本文复制引用
王啟宴,李山..内蒙古阿巴嘎旗必鲁甘干钼矿区地质特征及矿床成因浅析[J].山东国土资源,2013,(12):11-16,20,7.
