摘要
宁蒗地区喜山期斑岩带受近南北向的包都－波罗弧形断裂带控制，由壳幔混源型岩浆被动侵位而成，总体上呈向北逐渐倾伏的趋势。该斑岩带斑岩属钙碱性系列、中酸性岩类。通过对该斑岩带各斑岩体（群）地质特征、岩石化学特征的综合分析，表明其为含铜斑岩或铜（钼）斑岩，具良好的成矿前景。
Formed by passive emplacent of crust_mantle mixed type of magma and controlled by nearly NS_trending Baodu-Boluo arcuate fault zone, the Himalayan porphyry belt in Ninglang area tends generally to plunge northward. Porphyry rocks in this belt are intermediate_acid rocks of calc_alkaline series. An integrated analysis of geological and petrochemical characteristics of various porphyry bodies(groups) in this porphyry belt show that porphyry bodies in this belt are cupreous or copper (molybdenum) ones which have good metallogenic prospects.
出处
《岩石矿物学杂志》
CAS
CSCD
北大核心
1998年第2期136-144,共9页
Acta Petrologica et Mineralogica
关键词
宁蒗地区
喜山期
斑岩带
岩石化学
成矿性
Ninglang area
Himalayan period
porphyry belt
petrochemistry
ore potentiality
magma souce
