矿床地质2017，Vol.36Issue(4)：935-950,16.DOI:10.16111/j.0258-7106.2017.04.010
岩浆黑云母和热液黑云母矿物化学研究进展
Progress in study of mineral chemistry of magmatic and hydrothermal biotites
摘要
Abstract
Biotite is an important hydrated ferromagnesian silicate mineral in most magmatic rock.Its composition is useful in understanding magmatic properties,hydrothermal alteration and ore-forming processes.Based on the research results of previous researchers and the authors,this paper systematically summarizes chemistry application of biotite mineral in such aspects as classification,geothermometer,geothermobarometry and oxygen fugacity,its indicating significance for petrogenesis and tectonic setting,the halogen and halogen fugacity ratios evaluating magmatic hydrothermal process,and the exploration evaluation.These data provide the latest mineralogical evidence for metallogenic prediction and prospecting evaluation of porphyry Cu polymetallic deposits.This paper also analyzes some problems in the study and points out the work that needs to be done in this area in future.关键词
地质学/岩浆黑云母/热液黑云母/矿物化学/研究进展/斑岩矿床Key words
geology/magmatic biotites/hydrothermal biotites/mineral chemistry/progress in research/porphyry deposit分类
天文与地球科学引用本文复制引用
唐攀,唐菊兴,郑文宝,冷秋锋,林彬..岩浆黑云母和热液黑云母矿物化学研究进展[J].矿床地质,2017,36(4):935-950,16.基金项目
本文由公益性行业专项(编号:201511022-02,201511017)、国家自然科学基金项目(编号:41302060)和中国地质科学院基本科研业务费(编号:YYWF201608)联合资助 （编号:201511022-02,201511017）
