摘要
川滇新裂谷作用伴有强烈的岩浆活动,除大量玄武质岩浆喷溢外,在元谋朱布、黑泥坡等地见超基性岩体侵入,赋存有铂钯矿床。文章通过分析黑泥坡、朱布超基性岩体的土壤地球化学特征和岩石地球化学特征,结合元谋地区地质特征,提出了元谋地区超基性岩体铂钯矿床的成矿模式。
Sichuan-Yunnan new rifting is acompanied by strong magmatic activity. In addition to voluminous effused basaltic magma flow basic intrusion with Pt-Pd deposit occur at Zhubu and Heinipo. Combined with geological characteristics of Yuanmu area metallogenic model of Pt-Pd deposit in the ultra-basic intrusion is put forward on basis of analysing soil and rock geochemical characteristics of the ultra-basic intrusion.
出处
《地质找矿论丛》
CAS
CSCD
2011年第4期393-398,共6页
Contributions to Geology and Mineral Resources Research
关键词
裂谷作用
超基性岩
铂钯矿
成矿模式
元谋
云南省
rifting
ultra-basic rock
Pt-Pd deposit
metallogenic model
Yunan province
