首页 | 本学科首页   官方微博 | 高级检索  
     检索      

云和盆地早白垩世双峰式火山岩特征
引用本文:杨晓春.云和盆地早白垩世双峰式火山岩特征[J].浙江国土资源,1996(2).
作者姓名:杨晓春
作者单位:浙江省第七地质大队!丽水,323000
摘    要:本文从岩石学、岩石化学、微量元素及稀土元素等方面,对云和盆地早白垩世馆头组火山岩特征进行了论述,并对其形成环境及成因作了探讨.认为该套火山岩由基性岩及酸性岩构成,缺少SiO2含量在53.17%~68.57%的中性岩,是一套典型的双峰式火山岩组合。指出盆地内火山岩为拉张构造背景下形成,其基性岩和酸性岩具有不同源区,前者源于部分上地幔融熔物质(受陆壳物质混染);后者来自部分地壳融熔的产物。

关 键 词:双峰式火山岩  基性岩  酸性岩  早白垩世馆头组  云和盆地

FEATURES OF LOWER CRETACEOUS BIMIDAL VOLCANIC ROCKS IN ZHEJIANG YUNHE BASIN
Authors:Yang Xiaochun
Abstract:The volcanic rocks of lower cretaceous Guantou formation in south-west Zhejiang consist ofbasic rocks and acid rocks, without neutral rocks, of which silica are between 53. 17% and 68.57%. It is a set of. typical bimedal volcanic rock assemblage. On the basin of petrology, Petrc-chemistry, microelement and rare earth element, this paper expounded the features of the volcanic rocks, and discussed its forming environment and genesis.
Keywords:bimodal volcanic rock  basic rock  acid rock  Guantou formaytion  Yunhe basin  
本文献已被 CNKI 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号