地球学报
地毬學報
지구학보
ACTA GEOSCIENTIA SINICA
2013年
z1期
49-55
,共7页
莫向云%崔银亮%姜永果%薛步高
莫嚮雲%崔銀亮%薑永果%薛步高
막향운%최은량%강영과%설보고
海相火山岩%铜矿%成因%滇东南
海相火山巖%銅礦%成因%滇東南
해상화산암%동광%성인%전동남
marine volcanic rock%copper deposit%origin%southeast Yunnan
滇东南海相火山岩型铜矿系统研究程度较低,找矿潜力较大。区内3个典型铜矿床地质特征及地球化学研究表明,它们均为与海相火山岩有关的火山沉积改造型铜矿床。矿体受地层层位控制,与中三叠世含矿变基性火山岩系关系密切。同时,矿体受后期构造和热液改造,经历了强烈的变质作用,矿区侵入岩可能为矿体的二次富集提供了热液和物质来源。3个矿区的火山岩具有共性,都具备成为矿源层的条件,但成岩微构造环境有一定差异。区内找矿潜力较大,在加强深部找矿的同时,应重视火山岩的系统综合研究,以选定新靶区。
滇東南海相火山巖型銅礦繫統研究程度較低,找礦潛力較大。區內3箇典型銅礦床地質特徵及地毬化學研究錶明,它們均為與海相火山巖有關的火山沉積改造型銅礦床。礦體受地層層位控製,與中三疊世含礦變基性火山巖繫關繫密切。同時,礦體受後期構造和熱液改造,經歷瞭彊烈的變質作用,礦區侵入巖可能為礦體的二次富集提供瞭熱液和物質來源。3箇礦區的火山巖具有共性,都具備成為礦源層的條件,但成巖微構造環境有一定差異。區內找礦潛力較大,在加彊深部找礦的同時,應重視火山巖的繫統綜閤研究,以選定新靶區。
전동남해상화산암형동광계통연구정도교저,조광잠력교대。구내3개전형동광상지질특정급지구화학연구표명,타문균위여해상화산암유관적화산침적개조형동광상。광체수지층층위공제,여중삼첩세함광변기성화산암계관계밀절。동시,광체수후기구조화열액개조,경력료강렬적변질작용,광구침입암가능위광체적이차부집제공료열액화물질래원。3개광구적화산암구유공성,도구비성위광원층적조건,단성암미구조배경유일정차이。구내조광잠력교대,재가강심부조광적동시,응중시화산암적계통종합연구,이선정신파구。
The systematic study of the marine volcanic type copper deposits in southeast Yunnan Province is relatively insufficient, and the prospecting potential for this type of ore deposit is very promising in this area. Researches on three typical copper deposits show that they all belong to volcanic-sedimentary reformation type copper deposits related to marine volcanic rocks, and that ore bodies were controlled by stratigraphic horizons and gradually reformed into economic ore bodies by tectonic and hydrothermal activities. Volcanic rocks in the three studied ore deposits show some generality and all possess the conditions to serve as the ore resource beds;nevertheless, their rock-forming microstructural environments are somewhat different from each other. The ore-prospecting potential is fairly great in this area and, while strengthening the work of deep prospecting, we should also pay attention to the systematic and integrated study of the volcanic rocks so as to delineate new target areas.