摘要
湘南中生代玄武岩浆成因与岩石圈—软流圈相互作用＠郭锋＠范蔚茗＠林舸￥中国科学院长沙大地构造研究所玄武岩浆，成因，岩石圈—软流圈相互作用，中生代，湘南湘南中生代玄武岩浆成因与岩石圈—软流圈相互作用郭锋范蔚茗林舸（中国科学院长沙大地构造研究所，长沙４１００１...
Based on data of REE geochemistry,K-Ar dating and Nd isotopic compositions of Mesozoic basalts and gabbro xenoliths in NingyuanDaoxian region,Hunan Province,the evolution of mafic magmas and genesis of basalts have been discussed.From the indicative significance of basalts,the model of lithosphereasthenosphere interaction in Mesozoic in this region have been proposed.
出处
《矿物岩石地球化学通报》
CAS
CSCD
1998年第1期3-6,共4页
Bulletin of Mineralogy, Petrology and Geochemistry
基金
国家自然科学基金
中国科学院王宽诚基金
关键词
玄武岩浆
成因
岩石圈—软流圈相互作用
中生代
湘南
:genesis of basalts
lithosphereasthenosphere interaction
Mesozoic
South Hunan Province
