云南镇康县放羊山铅锌矿成矿特征及找矿方向
Metallogenetic Features and Prospecting Target of the Fangyangshan lead-zinc Deposit in Zhenkang County,Yunnan
放羊山铅锌矿床位于芦子园铅锌矿床NE部，矿区出露地层为上寒武统沙河厂组、保山组，矿体呈脉状、似层状、透镜状赋存于沙河厂组第二、三段之层间破碎带及断层破碎带中，矿体与围岩界线截然，矿床成因属热液充填-交代脉状矿床。
Fangyangshan lead-zinc deposit is located in the northeast of Luziyuan lead-zinc deposit. Upper Cambrian Shahechang Formation and Baoshan Formation occurred in the Fangyangshan region. The orebodies are occurred in vein , stratoid and lenticular shapes which hosted by interlaminar fracture zone and tectonic fracture zone of the second and thrid Member 0f Upper Cambrian Shahechang Formation. The orebodies are sharply bounded by wall rocks. Fangyangshan lead-zinc deposit is formed by filling and replacement and characterized by vein shape.
高林、赵飞、张权
地质学矿山地质、矿山测量
上寒武统放羊山破碎带热液充填交代
Upper Cambrian FormationFangyangshanFracture zoneHydrothermalFillingReplacement
高林,赵飞,张权.云南镇康县放羊山铅锌矿成矿特征及找矿方向[EB/OL].(2013-03-05)[2025-08-02].http://www.paper.edu.cn/releasepaper/content/201303-131.点此复制
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