攀西铁矿成矿带地质矿产特征及找矿方向  

Geology and exploration of the iron metallogenic belts in the Panzhihua-Xichang zone,southwestern Sichuan

作　　者：王子正[1,2] 范文玉[1] 高建华[1] 林明[1] 周邦国[1] 

机构地区：[1]成都地质矿产研究所,四川成都610081 [2]中国地质大学地球科学与资源学院,北京100083

出　　处：《沉积与特提斯地质》2012年第1期97-105,共9页Sedimentary Geology and Tethyan Geology

摘　　要：本文通过对攀西地区区域地质、区域矿产特征的分析,综合地球物理、遥感解译资料,共划分出4个找矿远景区:冕宁泸沽-喜德登相营富铁矿找矿远景区、盐源矿山梁子-牛厂富铁矿找矿远景区、太和-攀枝花钒钛磁铁矿远景区、西昌德昌兴隆-会理龙泉铁矿远景区。指出远景区内岩浆晚期分异型铁矿床、火山沉积变质型铁矿床等为主攻矿种。Four areas of ore prospecting for the iron ore deposits in the Panzhihua-Xichang zone, southwestern Sichuan are delineated according to regional geology, distribution of the ore deposits, geophysical properties and remote-sensing interpretation. They are the Lugu （in Mianning）-Dengxiangying （in Xide） iron-rich ore prospecting area, Kuangshanliangzi-Niuchang （in Yanyuan ） iron-rich ore prospecting area, Taihe-Panzhihua vanadiotitanomagnetite ore prospecting area, and Xinglong （in Dechang）-Longquan （in Huili） iron ore prospecting area. The key types of iron deposits for the further exploration should be concentrated in the late-magmatic differentiational iron deposits and volcanic-sedimentary-metamorphic iron deposits.

关 键 词：攀西地区 找矿远景区 岩浆晚期分异型铁矿 主攻矿种 

分 类 号：P622[天文地球—地质矿产勘探]