云南兰坪区吾含银铜矿矿床成因分析  

A PRELIMINARY GENESIS ANALYSIS OF QUWU AG-BEARING CU DEPOSIT OF LANPING,YUNNAN

作　　者：解文伟 刘俊 王本新 

机构地区：[1]云南省有色地质局三O六队,云南昆明650216

出　　处：《云南地质》2013年第3期289-291,302,共4页Yunnan Geology

摘　　要：银矿赋存于上三叠统石钟山组三段泥晶灰岩中。北东向推覆构造控矿。赋矿层位稳定,找矿标志明显。矿床属地层、构造控制及热液叠加层控矿床。The Ag deposit is in the argillo -crystalline limestone of Upper Permian Shizhongshan Formation Member 2, controlled by the NE nappe structure. The ore - bearing bed is stable and the prospecting criteria are clear. It belongs to the stratabound deposit of strata, structure control and hydrothermal superimposition.

关 键 词：层控含银铜矿 构造热液叠加 类质同像 石钟山组二段 云南兰坪区吾 

分 类 号：P618.510.1[天文地球—矿床学]