摘要
对登龙、热加地区晚三叠世三个不同火山旋回玄武岩的地球化学特征与板块构造环境进行了分析，指出了义敦岛弧的张性特征及其与成矿作用的关系．
The geochemical characteristics and platetectonic environments of Late Trissic basalts from three volcanic cycles of DenglongRejia area are discussed in this paper.It indicates that Yidun volcanic arc was an extensional arc,the extension of the volcanic arc was an important metallogenetic factor.
出处
《武汉化工学院学报》
1998年第4期29-32,共4页
Journal of Wuhan Institute of Chemical Technology
基金
地矿部大型项目
关键词
玄武岩
地球化学
张性弧
成矿作用
板块构造
basalt
geochemitry
extensional arc
Late Trissic
Western Sichuan
