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

额尔古纳地区中生代火山岩形成环境的研究
引用本文:张宏,金成洙.额尔古纳地区中生代火山岩形成环境的研究[J].国土资源,1999(1).
作者姓名:张宏  金成洙
作者单位:沈阳地质矿产研究所(张宏),东北大学资源与土木工程学院(金成洙)
基金项目:地矿部“九五”攻关项目
摘    要:额尔古纳地区中生代火山活动强烈,其主要的活动期间为晚侏罗世至早白垩世(150~100Ma)。根据新的岩石化学、稀土、微量元素、稳定同位素、构造等方面的分析结果得出以下认识:1.该区中生代火山岩来源较深,具幔源特征,岩浆形成在总体呈挤压背景的环境中,使得岩浆在演化过程中混入了大量的壳源物质;2.中生代火山岩大致分两个亚旋回,其中塔木兰沟组(J3t)火山岩和上库力组(K1s)火山岩是同一岩浆亚旋回的产物。

关 键 词:额尔古纳  中生代  火山岩  形成环境

FORMING BACKGROUND OF MESOZOIC VOLCANIC ROCKS IN ERGUN REGION
Zhang Hong.FORMING BACKGROUND OF MESOZOIC VOLCANIC ROCKS IN ERGUN REGION[J].Land & Resources,1999(1).
Authors:Zhang Hong
Abstract:In Ergun region the volcanic activities are very violent in Mesozoic era ,the volcanic rocks are mainly formed in late Jurassic to early Cretaceous (150-100Ma).According to the analysis on petrochemistry, REE, trace element, stable isotope,tectonics, the conclusions can be drawn as following: 1.The Mesozoic volcanic rocks source from the mantle,the magma are formed in pressed background.That is why there is much materials of crust source added in the Mesozoic magma. 2.The Mesozoic volcanic activities can be divided into two subcircles, among them, Tamulangou Formation(J 3 t ) and shangkuli Formation(K 1 s )are formed in the same subcircle.
Keywords:Ergun region  Mesozoic volcanic rock  Forming background  
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