金属矿山
金屬礦山
금속광산
Metal Mine
2015年
11期
104-108
,共5页
王长江%叶文荣%张明阳%史俊龙%周清
王長江%葉文榮%張明暘%史俊龍%週清
왕장강%협문영%장명양%사준룡%주청
矿床分布规律%地质特征%矿化类型%控矿因素%找矿模式%找矿预测
礦床分佈規律%地質特徵%礦化類型%控礦因素%找礦模式%找礦預測
광상분포규률%지질특정%광화류형%공광인소%조광모식%조광예측
Distribution regularities of deposit%Geological characteristics%Mineralization type%Ore-controlling factors%Prospecting pattern%Prospecting prediction
为了解浙东山门地区铜矿床的分布规律及地质特征,并对该地区铜矿床进行找矿预测,首先系统分析了区内地质、物化遥特征,然后对产出于该地区的半岭—黄施岙一带铜矿床(山门铜矿床)的产出状态、地质特征、矿化类型、围岩蚀变、控矿因素进行了详细讨论,结果表明:①区内铜矿床成矿的同时具有浅成热液和斑岩成矿系列的某些特点,简单地以构造热液充填或典型的斑岩成矿理论指导找矿是不合理的,应以与次火山岩有关的浅成热液型铜多金属矿作为主攻对象;②矿区所见矿化大多属高位或远端的矿化,其延深部位是现阶段找矿的主要目标,而斑岩成矿则可能在更深处。在上述分析的基础上,提出了矿区“五位一体”的找矿模式,即针对NW向断裂裂隙带、次级火山机构、多期次的潜火山-侵入岩、蚀变分带特征和物化探异常等5种不同的矿化类型提出了具体的找矿思路,为区内矿产勘查工作提供参考。
為瞭解浙東山門地區銅礦床的分佈規律及地質特徵,併對該地區銅礦床進行找礦預測,首先繫統分析瞭區內地質、物化遙特徵,然後對產齣于該地區的半嶺—黃施岙一帶銅礦床(山門銅礦床)的產齣狀態、地質特徵、礦化類型、圍巖蝕變、控礦因素進行瞭詳細討論,結果錶明:①區內銅礦床成礦的同時具有淺成熱液和斑巖成礦繫列的某些特點,簡單地以構造熱液充填或典型的斑巖成礦理論指導找礦是不閤理的,應以與次火山巖有關的淺成熱液型銅多金屬礦作為主攻對象;②礦區所見礦化大多屬高位或遠耑的礦化,其延深部位是現階段找礦的主要目標,而斑巖成礦則可能在更深處。在上述分析的基礎上,提齣瞭礦區“五位一體”的找礦模式,即針對NW嚮斷裂裂隙帶、次級火山機構、多期次的潛火山-侵入巖、蝕變分帶特徵和物化探異常等5種不同的礦化類型提齣瞭具體的找礦思路,為區內礦產勘查工作提供參攷。
위료해절동산문지구동광상적분포규률급지질특정,병대해지구동광상진행조광예측,수선계통분석료구내지질、물화요특정,연후대산출우해지구적반령—황시오일대동광상(산문동광상)적산출상태、지질특정、광화류형、위암식변、공광인소진행료상세토론,결과표명:①구내동광상성광적동시구유천성열액화반암성광계렬적모사특점,간단지이구조열액충전혹전형적반암성광이론지도조광시불합리적,응이여차화산암유관적천성열액형동다금속광작위주공대상;②광구소견광화대다속고위혹원단적광화,기연심부위시현계단조광적주요목표,이반암성광칙가능재경심처。재상술분석적기출상,제출료광구“오위일체”적조광모식,즉침대NW향단렬렬극대、차급화산궤구、다기차적잠화산-침입암、식변분대특정화물화탐이상등5충불동적광화류형제출료구체적조광사로,위구내광산감사공작제공삼고。
The ore-forming geological conditions of eastern Zhejiang volcanic depressions is good,a large number of cop-per-gold polymetallic deposits are distributed in this area. In order to understand the distribution regularity and geological char-acteristics of the copper deposits in this area and conduct prospecting prediction of the copper deposits in this area,firstly,the regional geological characteristics and physical, chemical, remote sensing characteristics of Shanmen area, eastern Zhejiang province are analyzed in depth;then,the output condition,geological characteristics,mineralization type and ore-controlling fac-tors of the Shanmen copper deposit that is located in Banling-Huangshiao area in Shanmen area,eastern Zhejiang province are discussed in detail. The reslts show that:①the copper deposit mineralization in this area with certain characteristics of epither-mal and porphyry metallogenic series,so,it is unreasonable to adopt the tectonic hydrothermal filling or typical porphyry metal-logenic theory to guide the prospecting work in this area,the epithermal type copper polymetallic deposits related to the sub-volcanic rocks should be taken as the main prospecting object;②most of the mineralization happened in the mining area are high mineralizaiton or distal mineralization,the extending area of the mineralization is the main prospecting goal,the phenome-non of porphyry mineralization may be happened in deeper place. Based on the above results,the prospecting pattern of "one whole with five pars"is proposed,that is to say,the detailed prospecting ideas of the five kinds of mineralization types( NW-di-rection fault fracture zone,secondary volcanic institutions,multi-stages latent volcano-intrusive rocks,alteration zoning charac-teristics and geophysical-geochemical anomalies) ,to provide reference for the prospecting work in this area.