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栾川群大红口组火山岩研究初探
引用本文:王跃峰.栾川群大红口组火山岩研究初探[J].河南国土资源,2000(3).
作者姓名:王跃峰
作者单位:河南省地矿厅区调队!河南平顶山467021
摘    要:河南省栾川群大红口组火山岩 ,岩性以碱性粗面质熔岩为主 ,经受不同程度的区域变质、动力变质及热液变质作用。喷发类型以裂隙式为主 ,有 4个喷发韵律 ,喷发环境为浅海 ;岩石地球化学特征显示 :其碱性火山岩属钾质型 ,形成于板内裂谷环境 ,与其伴生的辉长岩为同源岩浆成因 ,均来源于上地幔与下地壳的部分熔融产物

关 键 词:大红口组  碱性火山岩  钾质型  板内裂谷  熔融产物

PRELIMINARY RESEARCHING ON THE VOLCANIC ROCK OF DAHONGKOU FORMATION, LUANCHUAN GROUP
WANG,Yue-Feng.PRELIMINARY RESEARCHING ON THE VOLCANIC ROCK OF DAHONGKOU FORMATION, LUANCHUAN GROUP[J].Henan Land & Resources,2000(3).
Authors:WANG  Yue-Feng
Abstract:The main lithology of volcanic rocks of Dahongkou formation, Luanchuan Group of Henan is alkalilc trchytic lava, which underwent different grade of regional metamorphism, dynamic and hydrothermal metamorphism. The main types of eruption was fracture, there were four erupting sequence and the eruption setting was shallow sea. The characteristics of petrogeochemistry showed that the alkalic volcanic rock belonged to patassium type which formed in intraplate rift setting and the companied gabbro was automagma gness, these all came from the product of partial melt of upper mantle and lower crust.
Keywords:Dahongkou  formation  alkalic  volcanic  rock  patassim  type  intraplate  rift  melting  product  
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