CAJ | 학술논문

西峡县竹园铜矿脉赋存于含矿构造破碎带中，寨根北韧性剪切带区域性构造控制了铜矿床（点）和化探异常的分布。铜矿体受到破碎带控制，破碎带产状变化处，特别是由陡变缓处往往为铜矿化最富集的部位。区内成矿作用主要表现为构造-流体成矿，成矿方式以充填作用为主，成矿流体在长期构造活动过程中，在破碎带裂隙、角砾间沉淀形成脉状矿体。根据矿物共生组合特征，其矿床成因类型应属中温热液矿床。
서협현죽완동광맥부존우함광구조파쇄대중，채근북인성전절대구역성구조공제료동광상（점）화화탐이상적분포。동광체수도파쇄대공제，파쇄대산상변화처，특별시유두변완처왕왕위동광화최부집적부위。구내성광작용주요표현위구조-류체성광，성광방식이충전작용위주，성광류체재장기구조활동과정중，재파쇄대렬극、각력간침정형성맥상광체。근거광물공생조합특정，기광상성인류형응속중온열액광상。
Zhuyuan?copper?ore?veins?of?Xixia?County?are?occurred?in?ore-bearing?fracture?zone,?and?the?domain?structure?Zhaigen?northern?ductile?shear?zone?has?controlled?the?distribution?of?copper?deposit?(points)?and?regional?geochemical?anomalies.?The?copper?are?dominated?by?shuttered?zone,?copper?mineralization?zone?enrich?in?fracture?occurrence,?especially?where?from?steep?to?gentle.?Mineralization?in?this?area?is?tectonic?fluid,?mainly?by?filling.?Mineralization?in?the?area?are?mainly?structure?-?fluid?mineralization,?metallogenic?mode?is?filling?function,?the?ore?fluid?in?the?process?of?long-term?tectonic?activities,?in?the?fracture?zone?cracks,?breccia?precipitation?formation?into?vein?orebody.?According?to?mineral?assemblage?characteristics,?the?genetic?type?deposit?belongs?to?mesothermal?deposit.