加里曼丹中部浅成低温热液金矿地球化学分带及构造背景
摘要
本研究以加里曼丹新生代岩浆岩和相关的浅成低温热液型矿床为研究对象。初步研究表明,加里曼丹中部的巽他大陆北缘发育新生代多期岩浆活动,直接记录了由于南海扩张推动卢卡尼亚陆块向南运移俯冲碰撞的过程(Hotchison,2004)。由于这个过程中的多期岩浆活动,产生了浅成低温热液金矿带(Carlile and Mitchell,1994)。
出处
《矿物学报》
CAS
CSCD
北大核心
2015年第S1期1092-1093,共2页
Acta Mineralogica Sinica
基金
国家自然科学基金项目(批准号:41573039)
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