摘要
本文论述了洼村粘土矿床地质特征,成矿模式。根据成矿物质来源等方面研究,认为含矿岩系的物源主要来自碳酸盐岩的红土风化壳。矿床是在海侵过程中风化壳解体,经搬运、沉积、成岩及表生作用形成。
The geological characters and the metallogenic model of Wacun clay mine are introduced in the paper. According to the study of source of minerals etc. the ore-bearing minerals are mainly derived from the laterite weathering of carbonate rock. The deposit is formed in marine invasion by weathering crust transportation, sedimentation, diagenesis and supergenesis.
出处
《资源调查与环境》
2005年第3期199-204,共6页
Resources Survey & Environment
