摘要
安徽女山碱性玄武岩中具丰富的各类深源包体:二辉橄榄岩包体、辉石岩包体、复合包体和麻粒岩包体等.本文详细研究了这些包体的结构构造、矿物组合,分析了它们的矿物化学成分;通过对各种包体的平衡温压估算,结合地震测深资料,限定了女山地区壳幔边界及尖晶石/石榴石相转变带深度,并讨论了各类深源包体的原始层位.
There are abundant deepseated xenoliths in Nushan alkali basalts, Anhui province, such as lherzolites, pyroxenites, composite xenoliths and granulite xenoliths. In this paper, the textures and mineral assemblages of these xenoliths are in detail studied, and the mineral compositions of different phase are carefully analyzed by electron microprobe. By calculating the equilibrium temperatures and pressures, integrating the deep seismic sounding profile HQ13, the depths of the crustmantle boundary and the garnetspinel transitional zone are defined, at the same time, the original depths of the various deepseated xenoliths are also discussed.
出处
《南京大学学报(自然科学版)》
CAS
CSCD
1998年第3期292-302,共11页
Journal of Nanjing University(Natural Science)
基金
国家自然科学基金
国家教委博士点基金
关键词
深源包体
复合包体
矿物化学
碱性玄武岩
deepseated xenolith, composite xenolith, mineral chemistry, equilibrium TP