摘要
在星子变质核杂岩和武功山变质核杂岩中发现了高 Sr低 Y型花岗岩。这是变质核杂岩构造中高 Sr低 Y型花岗岩的首次报道。地球化学研究结果表明 ,它们具有与adakite相似的地球化学特征。在时空分布上 ,属于中国东部 adakite。它们是由玄武岩岩浆底侵到加厚的陆壳底部导致下地壳麻粒岩部分熔融形成的。结合花岗岩的地球化学特征及现有的资料探讨高 Sr低
The high Sr and low Y granites were found for the first time in Xingzi and Wugongshan metamorphic core complexes.Geochemical studies indicate that the geochemical characteristics of these granites are similar to those of the adakite. They belong to 'Yanshan adakites area' in east China. It is probably a product of partial melting of the lower crust granulite in the thickened crust resulted from underplating of basaltic magma. This paper presents the geochemical characteristics of these granites and discusses the genetic relationship between high Sr,low Y granite and metamorphic core complex.
出处
《矿物岩石》
CAS
CSCD
北大核心
2002年第4期16-20,共5页
Mineralogy and Petrology
基金
中国科学院创新重要方向性项目 (KZCX2 -10 2 )
国家自然科学基金 (4 9873 0 0 8)
关键词
花岗岩
变质核杂岩
成因关系
地球化学
麻粒岩
high Sr low Y granite
metamorphic core complex
genetic relationship