摘要
银厂坡金矿位于金平断凹西部哀牢山深大断裂南缘。控矿因素为地层、构造、岩浆岩。为岩浆期后热液通过富集作用形成的残坡积土型金矿。系统介绍银厂坡金矿地质特征和成矿规律,给出该区理想的成矿模式。
The Yinchangpo Au deposit is located along the S margin of Ailaoshan megafault in the W part of Jinping fault sag.The ore control factor includes strata,structure and magmatic rock.It is the eluvial-slope wash Au deposit formed by the postmagmatic hydrothermal enrichment.In this paper,we introduce systematically the geological characteristics,metallogenetic rule of Yinchangpo Au deposit and the ideal metallogenetic model of this orefield.
出处
《云南地质》
2010年第2期168-171,共4页
Yunnan Geology
关键词
残坡积型金矿
微粒自然金
控矿因素
金矿成矿模式
云南金平银厂坡
Eluvial-Slope Wash Au Deposit
Micrograined Natural Au
Ore Control Factor
Metallogenetic Model of Au Deposit
Yinchangpo
Jinping
Yunnan
