摘要
芦子园铅锌矿产于镇康复背斜核部寒武系沙河厂组大理岩、板岩、片岩地层中,沿背斜轴部产生的断层及层间破碎带是主要的容矿构造,成矿物质来源于地层、酸性及基性岩浆热液,矿床成因为沉积-热液改造叠生型铅锌矿床。
The Luziyuan Pb- Zn deposit is occurred in the marble, slate and schist of Cambrian Shahechang Formation in the core of Zhenkang anticlinoria of Yunnan. And the fault and bedding fractured zone along the anticline axis are the main ore -bearing structures. The metallogenetic ele- ment originates from strata, thermal fluid of acidic and basic magma. The genesis of ore deposit belongs to the sedimentation -hydrothermal reformation superimpo sition type.
出处
《云南地质》
2007年第4期404-410,共7页
Yunnan Geology
关键词
沉积热液改造
层位岩性控矿
中温叠生矿床
芦子园镇康云南
Sedimentation - Hydrothermal Reformation
Horizon - Litholo gical CharacterOre - Control
Middle T Superimposition Ore Deposit
Luziyuan, Zhenkang
