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攀西铁矿成矿带地质矿产特征及找矿方向 被引量:7

Geology and exploration of the iron metallogenic belts in the Panzhihua-Xichang zone,southwestern Sichuan
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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.
出处 《沉积与特提斯地质》 CAS CSCD 2012年第1期97-105,共9页 Sedimentary Geology and Tethyan Geology
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 Panzhihua-Xichang zone ore prospecting area late-magmatic differentiational iron deposit key typesof iron deposits
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