甘肃冶金
甘肅冶金
감숙야금
Gansu Metallurgy
2015年
5期
66-69,73
,共5页
武小迪%张佳峰%高卫宏%陈明寿%张选固
武小迪%張佳峰%高衛宏%陳明壽%張選固
무소적%장가봉%고위굉%진명수%장선고
西坝岩体%石英闪长岩%灰黑色含炭红柱石板岩%红柱石
西壩巖體%石英閃長巖%灰黑色含炭紅柱石闆巖%紅柱石
서패암체%석영섬장암%회흑색함탄홍주석판암%홍주석
Xiba rock%quartz diorite%black carbonaceous slate%andalusite
西坝岩体位于陕西凤太铅锌金多金属矿田东南部,是矿田内最大的岩体,其南东与华阳花岗岩相接,有人认为是华阳花岗岩体的一部分,而华阳岩体又是宁陕岩体群的一个组成部分。《陕西省区域地质志》把西坝岩体划归华力西期石英闪长岩,而把华阳花岗岩归为印支期二长花岗岩,西坝岩体比华阳岩体更老。西坝岩体北部有宽约300~700 m宽的热力变质带,主要是黑云母角岩带。近几年在南带工作发现有约宽50~500 m不等的红柱石矿(化)带,其长度大于1000 m,局部达到了工业矿体的要求,含矿岩石主要为灰黑色含炭红柱石板岩。本区是寻找红柱石矿最有利的地区之一,值得关注。
西壩巖體位于陝西鳳太鉛鋅金多金屬礦田東南部,是礦田內最大的巖體,其南東與華暘花崗巖相接,有人認為是華暘花崗巖體的一部分,而華暘巖體又是寧陝巖體群的一箇組成部分。《陝西省區域地質誌》把西壩巖體劃歸華力西期石英閃長巖,而把華暘花崗巖歸為印支期二長花崗巖,西壩巖體比華暘巖體更老。西壩巖體北部有寬約300~700 m寬的熱力變質帶,主要是黑雲母角巖帶。近幾年在南帶工作髮現有約寬50~500 m不等的紅柱石礦(化)帶,其長度大于1000 m,跼部達到瞭工業礦體的要求,含礦巖石主要為灰黑色含炭紅柱石闆巖。本區是尋找紅柱石礦最有利的地區之一,值得關註。
서패암체위우협서봉태연자금다금속광전동남부,시광전내최대적암체,기남동여화양화강암상접,유인인위시화양화강암체적일부분,이화양암체우시저협암체군적일개조성부분。《합서성구역지질지》파서패암체화귀화력서기석영섬장암,이파화양화강암귀위인지기이장화강암,서패암체비화양암체경로。서패암체북부유관약300~700 m관적열력변질대,주요시흑운모각암대。근궤년재남대공작발현유약관50~500 m불등적홍주석광(화)대,기장도대우1000 m,국부체도료공업광체적요구,함광암석주요위회흑색함탄홍주석판암。본구시심조홍주석광최유리적지구지일,치득관주。
The Xiba granitoids in Shaanxi Phoenix too Pb Zn Au polymetallic ore field in southeastern is largest rock in the ore field, the southeast and Huayang granite is connected, is considered part of Huayang granite, and Huayang rock and Ningshan plutons of a part.The Shaanxi Province regional geology, the Xiba rock was placed under the Variscan quartz dio-rite, and the Huayang granite belongs to the Indosinian granite, Xiba rock Huayang rock than older.Northern Rock Xiba thermometamorphism width of about 300 to 700 meters wide, is mainly biotite hornfels zone.In recent years in the South with a width of 50-500 meters of andalusite ore ( ) with, the length of greater than 1000 meters, the local reached the re-quirements of industrial orebody, ore bearing rock is mainly gray and black carbon containing andalusite slate.This area is to find one of the most favorable areas of andalusite, worthy of attention.