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小兴安岭北段林海林场花岗岩年代学、地球化学特征及构造意义

牟福权 许国雨 卢鸿雁 崔雪文 常亮 娄雨雷 祁迎圣 邱信东

地质与资源2025,Vol.34Issue(1):1-10,102,11.
地质与资源2025,Vol.34Issue(1):1-10,102,11.DOI:10.13686/j.cnki.dzyzy.2025.01.001

小兴安岭北段林海林场花岗岩年代学、地球化学特征及构造意义

Geochronology and geochemistry of granites in Linhai forest farm,northern Xiaoxinganling Mountains:Tectonic implication

牟福权 1许国雨 1卢鸿雁 2崔雪文 1常亮 1娄雨雷 1祁迎圣 1邱信东1

作者信息

  • 1. 中国地质调查局牡丹江自然资源综合调查中心,黑龙江 牡丹江 157021
  • 2. 辽宁省自然资源事务服务中心,辽宁沈阳 110033
  • 折叠

摘要

Abstract

A series of highly fractionated I-type granites,mainly composed of marginal facies fine-grained monzogranite and central facies fine-medium-grained monzogranite,is developed in Linhai forest farm area of the Xiaoxinganling-Zhangguangcailing mountains.The granites are characterized by high Si and total alkali(Na2O+K2O),rich Al,and poor Fe,Mg,Ca and Ti,belonging to quasi-aluminous,high-K calc-alkaline series,with enriched LILEs and LREEs,depleted HFSEs,and moderately strong negative Eu anomaly.The LA-ICP-MS zircon U-Pb age results show that the granites were formed at 191.6±2.9 Ma.According to the geochemical compositions,it is considered that the granites are mainly derived from the partial melting of shallow continental crust materials in Early Mesozoic.The discovery of highly fractionated I-type granites indicates that large-scale magmatic intrusion occurred in the Early Jurassic,which may be closely related to the regional extensional environment under the westward subduction of paleo-Pacific plate.

关键词

早侏罗世/花岗岩/地质年代学/地球化学/构造背景/小兴安岭/张广才岭

Key words

Early Jurassic/granite/geochronology/geochemistry/tectonic setting/Xiaoxinganling/Zhangguangcailing

分类

天文与地球科学

引用本文复制引用

牟福权,许国雨,卢鸿雁,崔雪文,常亮,娄雨雷,祁迎圣,邱信东..小兴安岭北段林海林场花岗岩年代学、地球化学特征及构造意义[J].地质与资源,2025,34(1):1-10,102,11.

基金项目

黑龙江省国土资源厅项目"黑龙江省逊克县福民林场、永胜经营所幅1∶5万区域地质矿产调查"(HLJKD2006-10). (HLJKD2006-10)

地质与资源

1671-1947

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