摘要
本文论述了新疆喀孜别克锡矿床的含矿岩休、矿床地质、成矿的物理化学条件和成矿地球化学的流体包裹体、硫、氧、铅、铷－锶同位素和稀土元素特征，确定矿床成因是与花岗岩有关的高－中温热液矿床．
The Kezbike tin deposit is studied with respect to the geological features,oreforming physicochemical conditions and metallogenetic geochemical characterishcs of the deposit.It is believed that the deposit is the granite-related hydrothermal deposit with high to medium temperature.
出处
《合肥工业大学学报（自然科学版）》
CAS
CSCD
1994年第1期160-164,共5页
Journal of Hefei University of Technology：Natural Science
关键词
锡矿床
成矿地球化学
矿床成因
tin deposit,metallogenetic geochemistry,Kezbike
