CAJ | 학술논문

依据青海索拉沟铜多金属矿床地质地球化学特征，特别是矿床物质来源、矿物、元素分带、成矿热液演化中铜多金属矿床的性状，对该矿床的地质特征、矿床成因及控矿条件进行了研究。研究表明，该索拉沟铜多金属矿床属火山沉积—热液改造型矿床，其矿床经历了沉积成岩和热液改造两个阶段。中三叠世海底火山喷发喷气活动携带大量成矿物质，在浅海台地相对低洼的部位（还原条件下）与火山碎屑物、陆源物一起沉积下来，形成了最初的“矿源层”或贫矿层，在随后的（印支期）造山过程中，受强烈构造-岩浆活动的作用，地层中岩石脱水、成矿元素活化、聚集形成富矿溶液，并沿地层层理、岩石破裂运移，交代岩石中化学性活泼的组分或充填于岩石裂隙中富集成矿。
의거청해색랍구동다금속광상지질지구화학특정，특별시광상물질래원、광물、원소분대、성광열액연화중동다금속광상적성상，대해광상적지질특정、광상성인급공광조건진행료연구。연구표명，해색랍구동다금속광상속화산침적—열액개조형광상，기광상경력료침적성암화열액개조량개계단。중삼첩세해저화산분발분기활동휴대대량성광물질，재천해태지상대저와적부위（환원조건하）여화산쇄설물、륙원물일기침적하래，형성료최초적“광원층”혹빈광층，재수후적（인지기）조산과정중，수강렬구조-암장활동적작용，지층중암석탈수、성광원소활화、취집형성부광용액，병연지층층리、암석파렬운이，교대암석중화학성활발적조분혹충전우암석렬극중부집성광。
Based on Solagol copper polymetallic ore deposit geological, geochemical characteristics, especially ore deposit material provenance, minerals, elements zoning, copper polymetallic ore deposit properties and state during ore forming hydrothermal evolution carried out studies on ore deposit geological features, deposit genesis and deposit controlling factors. The study has shown that the ore deposit belongs to volcanic deposit—hydrothermal transformed type has experienced two stages of deposit and transform. Middle Trias?sic submarine volcanic eruption brought along a mass of ore-forming material, then deposited with pyroclasts and terrigenous composi?tions on relatively low part of shallow sea platform (under reducing condition) and formed initial“source bed”or“lean bed”, during the following Indo-Chinese epoch orogenic process, impacted by strong structural and magmatic activities, rock dehydration, metallogenic element activated, brought together and formed pay solution, then migrated along strata bedding, rock fractures and replaced chemical?ly active components in rocks or filled in fractures enriched into ore deposit.