合肥工业大学学报(自然科学版)
閤肥工業大學學報(自然科學版)
합비공업대학학보(자연과학판)
JOURNAL OF HEFEI UNIVERSITY OF TECHNOLOGY(NATURAL SCIENCE)
2013年
12期
1504-1510
,共7页
矿床地质特征%矿床成因类型%锌金矿床%矽卡岩型矿床%沙滩脚矿田%安徽铜陵
礦床地質特徵%礦床成因類型%鋅金礦床%矽卡巖型礦床%沙灘腳礦田%安徽銅陵
광상지질특정%광상성인류형%자금광상%석잡암형광상%사탄각광전%안휘동릉
geological characteristics of ore deposit%genetic type of ore deposit%zinc-gold deposit%skarn type deposit%Shatanjiao ore field%Tongling in Anhui Province
沙滩脚矿田位于长江中下游成矿带铜陵矿集区的东部,是该矿集区具有重要成矿潜力的矿田。沙滩脚矿田共有13个矿床(点),其中特大型矿床1处(姚家岭),其余为小型矿床及矿点(沙滩脚、朱家冲、戴腰山、凤形山、小工山等),矿床类型主要为中低温热液型、矽卡岩型矿床,矿化组合以Zn-Au-Cu多金属元素为主。区内沙滩脚岩体及姚家岭岩体、二叠系及石炭系碳酸盐岩分别为重要的成矿岩体和赋矿地层。沙滩脚矿田的成矿作用是铜陵矿集区燕山期成矿作用的有机组成部分。
沙灘腳礦田位于長江中下遊成礦帶銅陵礦集區的東部,是該礦集區具有重要成礦潛力的礦田。沙灘腳礦田共有13箇礦床(點),其中特大型礦床1處(姚傢嶺),其餘為小型礦床及礦點(沙灘腳、硃傢遲、戴腰山、鳳形山、小工山等),礦床類型主要為中低溫熱液型、矽卡巖型礦床,礦化組閤以Zn-Au-Cu多金屬元素為主。區內沙灘腳巖體及姚傢嶺巖體、二疊繫及石炭繫碳痠鹽巖分彆為重要的成礦巖體和賦礦地層。沙灘腳礦田的成礦作用是銅陵礦集區燕山期成礦作用的有機組成部分。
사탄각광전위우장강중하유성광대동릉광집구적동부,시해광집구구유중요성광잠력적광전。사탄각광전공유13개광상(점),기중특대형광상1처(요가령),기여위소형광상급광점(사탄각、주가충、대요산、봉형산、소공산등),광상류형주요위중저온열액형、석잡암형광상,광화조합이Zn-Au-Cu다금속원소위주。구내사탄각암체급요가령암체、이첩계급석탄계탄산염암분별위중요적성광암체화부광지층。사탄각광전적성광작용시동릉광집구연산기성광작용적유궤조성부분。
The Shatanjiao polymetallic ore field ,located in the eastern of Tongling uplift district in the Middle-Lower Yangtze River Valley metallogenic belt ,is a significant potential mineralization area . There are thirteen deposits in the area ,including a super-large deposit called Yaojialing ,and some other small deposits called Shatanjiao ,Zhujiachong ,Daiyaoshan ,Fengxingshan ,Xiaogongshan and so on .The major types of the deposit are medium-low hydrothermal deposits and skarn type deposits . Mineralization assemblages are mainly composed of zinc-gold-copper polymetallic elements .Shatanjiao and Yaojialing intrusive rocks are both important related rocks for mineralization ,and the dominant ore-forming related formations are Carbonic-Permian carbonatite rocks .The metallogenetic process of Shatanjiao ore field is a part of Yanshannian mineralization in Tongling ore district .