CAJ | 학술논문

　　汝阳王坪西沟大型铅锌银矿床，属构造蚀变岩型热液矿床，主要工业矿体呈似层状或大透镜状赋存于断裂破碎带中。矿床产状与矿带一致，属陡斜倾矿体，在走向或倾向上呈舒缓波状，膨缩特征明显。铅含量大于锌，银以类质同象赋存于方铅矿品格中，铅与银呈正比变化。诚然，在能圈出富矿体的铅锌矿体部位，也是银矿体的分布空间；矿石组构方面，硫化矿石结构主要有半自形-它形粒状结构为主；构造则以细脉浸染状构造和脉状块状构造为主。
　　여양왕평서구대형연자은광상，속구조식변암형열액광상，주요공업광체정사층상혹대투경상부존우단렬파쇄대중。광상산상여광대일치，속두사경광체，재주향혹경향상정서완파상，팽축특정명현。연함량대우자，은이류질동상부존우방연광품격중，연여은정정비변화。성연，재능권출부광체적연자광체부위，야시은광체적분포공간；광석조구방면，류화광석결구주요유반자형-타형립상결구위주；구조칙이세맥침염상구조화맥상괴상구조위주。
Large?sized?Wangpingxigou?lead?and?zinc?silver?deposit?of?Ruyang?belongs?to?the?tectonic?altered?rock?type?of?hydrothermal?deposit.?Major?industrial?ore?bodies?show?layer?or?lenticular?occurrence?in?fault?fracture?zone.?Occurrence?of?ore?deposits?and?ore?belt?is?consistent,?belongs?to?the?steep?inclined?dip?orebody.?It?is?on?to?or?tends?to?slow?wave;?the?characteristic?of?bulk?shrinkage?is?obvious.?Lead?content?is?greater?than?the?zinc,?silver?with?such?quality?as?occurrence?in?galena?character,?lead?and?silver?were?in?positively?relation.?It?is?true,?where?can?circle?the?lead-zinc?mine?rich?ore?body,?also?existed?the?silver?ore?bodies;?On?ore?fabric,?structure?of?sulfide?ores?are?mainly?hypidiomorphic,?and?the?structure?with?fine?vein?disseminated?and?vein?block?structure?are?dominant.