首页|早侏罗世粗中粒黑云母二长花岗岩岩石地球化学、LA-ICP-MS锆石U-Pb年代学特征及成因——以大兴安岭北段潮满林场地区为例

早侏罗世粗中粒黑云母二长花岗岩岩石地球化学、LA-ICP-MS锆石U-Pb年代学特征及成因——以大兴安岭北段潮满林场地区为例

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以大兴安岭北段额尔古纳地块北缘潮满林场地区粗中粒黑云母二长花岗岩为研究对象,采用地质调查、岩石地球化学和LA-ICP-MS锆石U-Pb年代学方法,分析粗中粒黑云母二长花岗岩岩石学、主量元素、微量元素和年代学等特征,探讨成因及构造环境.结果表明:潮满林场地区粗中粒黑云母二长花岗岩具有Ⅰ型花岗岩特征,属于弱过铝质高钾钙碱性花岗岩;粗中粒黑云母二长花岗岩中SiO2的质量分数为68.92%~72.44%,Na2O的质量分数为4.65%~4.85%,K2O的质量分数为3.33%~4.41%,Al2O3的质量分数为15.25%~16.75%,里特曼指数为0.95~2.84;稀土元素总量的质量分数为(101.24~152.40)×10-6,轻、重稀土元素分馏明显,轻稀土元素富集,重稀土元素亏损,其中富集Rb、Th、Ce、Zr等元素,相对亏损Ta、Nb、P、Ti等元素.粗中粒黑云母二长花岗岩岩浆来源于新增生下地壳物质的部分熔融,形成于早侏罗世(192.1 ± 1.6)Ma.研究区早侏罗世粗中粒黑云母二长花岗岩的形成环境为与蒙古—鄂霍茨克洋南向俯冲—碰撞作用相关的活动大陆边缘火山弧环境.该结果为研究大兴安岭北段潮满林场地区粗中粒黑云母二长花岗岩岩体构造背景和年代学提供依据.
Geochemistry and LA-ICP-MS zircon U-Pb chronology and genetic mechanism of the Early Jurassic coarse to medium grained biotite monzogranite:a case study of the Chaoman Forest Farm area in the Northern Great Xing'an Range
The study focuses on the coarse to medium grained biotite monzogranitein Chaoman Forest Farm on the northern edge of the Erguna Block in North Great Xing'an Range.Adopting geological sur-veys,rock geochemistry,and LA-ICP-MS zircon U-Pb geochronology research methods is to analyze the petrological,major element,trace element,and chronological characteristics of the coarse to medium grained biotite monzogranite and to discuss its genesis mechanism and tectonic environment.The results show that the coarse to medium grained biotite monzogranite in the Chaoman Forest Farm area has I-type granite characteristics and belongs to weakly peraluminous and high potassium-cala-alkaline gran-ite,the w(SiO2)of monzogranite is 68.92%-72.44%,w(Na2O)is 4.65%-4.85%,w(K2O)is 3.33%-4.41%,andw(Al2O3)is 15.25%-16.75%,rittman index(a)is 0.95-2.84.Total rare earth content is(101.24-152.40)×10-6.There are significant fractionation of light and heavy rare earths,enrichment of light rare earths,loss of heavy rare earths,enriched in elements such as Rb,Th,Ce,Zr and relative-ly depleted in elements such as Ta,Nb,P,and Ti.The magma of the coarse to medium grained biotite monzogranite originates from the partial melting of newly accreted lower crustal materialand was formed in the Early Jurassic(192.1±1.6)Ma.The tectonic environment of the Early Jurassic coarse to medi-um grained biotite monzogranite in the study area is an active continental margin volcanic arc environ-ment related to the south ward subduction collision of the Mongolian-Okhotsk Ocean.This result pro-vides evidence for the study of the tectonic background and chronology of the coarse to medium grained biotite monzogranite in the Chaoman Forest Farm area of the northern section of the Great Xing'an Range.

LA-ICP-MS zircon U-Pb chronologygeochemistrycoarse to medium grained biotite monzograniteEarly JurassicChaoman Forest FarmNorth Great Xing'an Range

于喜洹、崔锡彪、陆胜、王野、李新鹏、孙江军、陈旭峰、温丹

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黑龙江省自然资源调查院,黑龙江哈尔滨 150036

黑龙江省第五地质勘查院,黑龙江哈尔滨 150090

黑龙江省地球物理地球化学勘查院,黑龙江哈尔滨 150030

LA-ICP-MS锆石U-Pb年代学 地球化学 粗中粒黑云母二长花岗岩 早侏罗世 潮满林场地区 大兴安岭北段

黑龙江省1∶5万区域地质矿产调查项目

HLJKD2015-04

2024

东北石油大学学报
东北石油大学

东北石油大学学报

CSTPCD北大核心
影响因子:1.274
ISSN:2095-4107
年,卷(期):2024.48(2)