科洛新生代火山群富钾火山岩中的幔源包体特征及上地幔热状态  

Discussion on the Character of Mantle-derived Inclusion and the Heat State of Upper Mantle in the Cenozoic Rich Potassium Volcanic Rocks of the Keluo

作　　者：刘勇[1] 赵寒冬[1] 徐受民[1] 宋亚琴 柳震 马丽玲 赵焱 崔建伟 

机构地区：[1]中国地质大学,北京100083 [2]黑龙江省地质调查研究总院,黑龙江哈尔滨150036 [3]黑龙江省地质矿产测试应用研究所,黑龙江哈尔滨150036

出　　处：《东华理工大学学报（自然科学版）》2008年第1期1-6,共6页Journal of East China University of Technology(Natural Science)

基　　金：国家基础地质调查"中国地质调查局1:5万五大连池农场等四幅联测项目"(0100123057)

摘　　要：黑龙江省科洛火山群富钾火山岩主要岩石组合为碱玄岩、响岩等岩石,岩石学、岩石化学、地球化学、同位素等特征研究表明,其岩浆来自上地幔并为板内裂谷环境,是上地幔岩部分熔融形成的岩浆喷至地表冷凝形成的。岩石中幔源金云母、尖晶石二辉橄榄岩包体研究表明,科洛地区的上地幔是"过热"的,这种"过热"的状态,正是诱发大陆裂谷构造形成的根本原因。Main combination of the rich potassium volcanic rocks of the Kelou irl Heilongjiang Province, are alkali basalt, phonolite, latite, etc.. Studying the character of the lithology, petrochemistry, geochemistry, isotope, it indicate that the magma come fronl the upper mantle, and environment is the inner plate rift. They are formed by extrusion to the earth＇s surface and condensation, a part of melting magma of upper mantle. Studying the character of the mantle-derived inclusion such as the inclusion of the phlogopite, spinel lherzolite, the upper mantle of the Kelou is ＂over heat＂, the state of the ＂over heat＂ is the fundamental reason of place a premium on continental rift.

关 键 词：富钾火山岩 幔源包体 大陆裂谷 科洛 黑龙江 

分 类 号：P588.14[天文地球—岩石学]