地球学报Issue(z1)：202-206,5.DOI:10.3975/cagsb.2013.s1.31
全球红土型镍矿床的基本成矿规律
The Basic Metallogenic Regularity of Global Lateritic Nickel Ore Deposits
陈百友 1刘洪滔 2杨平 3孙媛1
作者信息
- 1. 云南省有色地质局，云南昆明 650051
- 2. 云南省有色地质局地质地球物理化学勘查院，云南昆明 650216
- 3. 云南省有色地质局地质研究所，云南昆明 650216
- 折叠
摘要
Abstract
The global lateritic nickel ore deposits have distinct temporal and spatial distribution regularity, and the lateritic nickel ore bodies are characterized by apparent vertical zoning. The intensity of lateritic nickel mineralization is obviously influenced and controlled by the components of ore-forming parent rock (such as nickel content and lithogeochemical and mineral composition), climate, topography, hydrogeology, structural geology, duration of ore-forming process, and maturity of the weathering crust. Types of lateritic nickel ore deposits are mainly controlled by climate, tectonic setting and the state of structural uplift and also influenced by topography, drainage condition, lithology of ore-forming parent rock and its serpentinization.关键词
红土型镍矿床/基本成矿规律/全球Key words
lateritic nickel ore deposit/basic metallogenic regularity/global分类
天文与地球科学引用本文复制引用
陈百友,刘洪滔,杨平,孙媛..全球红土型镍矿床的基本成矿规律[J].地球学报,2013,(z1):202-206,5.
