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大兴安岭北部雄关地区倭勒根岩群大网子岩组火山岩地球化学特征

姜迎久 舒广龙 胥嘉 冯德胜 王春光

地质与资源2019,Vol.28Issue(3):223-230,253,9.
地质与资源2019,Vol.28Issue(3):223-230,253,9.

大兴安岭北部雄关地区倭勒根岩群大网子岩组火山岩地球化学特征

GEOCHEMISTRY OF THE VOLCANIC ROCKS OF DAWANGZI ROCK FORMATION IN NORTHERN DAXINGANLING MOUNTAINS

姜迎久 1舒广龙 2胥嘉 2冯德胜 1王春光3

作者信息

  • 1. 黑龙江省有色地质勘查706队,黑龙江齐齐哈尔161006
  • 2. 中国地质调查局沈阳地质调查中心,辽宁沈阳110034
  • 3. 吉林省地质勘查基金管理中心,吉林长春130061
  • 折叠

摘要

Abstract

The Dawangzi rock formation of Wolegen rock group in Xiongguan area,northern Daxinganling Mountains, is composed of mainly meta﹣clastic rocks with metarhyolite and meta﹣trachyandesite. The zircon U﹣Pb dating of the trachyandesite by ICP﹣MS yields the 206Pb/238U age of 443.8﹣783.8 Ma,with the zircon U﹣Pb concordia age of 463.7 ± 2.1 Ma,and the weighted mean age of 463.6 ± 6.4 Ma (n=10,MSWD = 0.073). The tested zircons show developed oscillation rings,with the Th/U ratio generally ranging from 0.42 to 1.76,indicating a magmatic origin. This age represents the forming age of the trachyandesite,which is believed to be formed in Middle Ordovician,consistent with the formation time of regional Dawangzi rock formation (Cambrian﹣Early Silurian). The trachyandesite,belonging to alkali﹣calcic quasi﹣aluminous rocks,is characterized by unobvious Eu anomaly,depletion of HFSEs and enrichment of LILEs. The rocks have the features of crust﹣mantle mixed source,which was formed in the continental margin environment and related to the subduction of Paleo﹣Asian Ocean crust.

关键词

锆石U﹣Pb年龄/地球化学特征/大网子岩组/大兴安岭北部

Key words

zircon U﹣Pb age/geochemical characteristics/Dawangzi rock formation/northern Daxinganling Mountains

分类

天文与地球科学

引用本文复制引用

姜迎久,舒广龙,胥嘉,冯德胜,王春光..大兴安岭北部雄关地区倭勒根岩群大网子岩组火山岩地球化学特征[J].地质与资源,2019,28(3):223-230,253,9.

基金项目

黑龙江省财政拨款"黑龙江省呼中区幅、大白山幅1:5万区域地质矿产调查"(编号:HLJKD2014-18). (编号:HLJKD2014-18)

地质与资源

OACSTPCD

1671-1947

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