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大兴安岭呼中地区满克头鄂博组火山岩地球化学特征、锆石U-Pb年龄及构造环境

于跃江 李慧 李新鹏 江峰 梁景龙 李金明 卜程丹

东北石油大学学报2025,Vol.49Issue(3):29-40,12.
东北石油大学学报2025,Vol.49Issue(3):29-40,12.DOI:10.3969/j.issn.2095-4107.2025.03.003

大兴安岭呼中地区满克头鄂博组火山岩地球化学特征、锆石U-Pb年龄及构造环境

Geochemical characteristics,Zircon U-Pb ages and tectonic setting of the Manketou'ebo Formation volcanic rocks in the Huzhong Area,Great Xing'an Range

于跃江 1李慧 2李新鹏 1江峰 2梁景龙 1李金明 1卜程丹3

作者信息

  • 1. 黑龙江省自然资源调查院,黑龙江哈尔滨 150036
  • 2. 黑龙江省第三地质勘查院,黑龙江哈尔滨 150300
  • 3. 黑龙江省地质测绘地理信息院,黑龙江哈尔滨 150030
  • 折叠

摘要

Abstract

This study investigates the volcanic rocks of the Manketou'ebo Formation in the Huzhong Area of the Great Xing'an Range using geological survey methods,petrological and geochemical analyses,and zircon U-Pb dating via LA-ICP-MS.The research systematically examines the petrology,major and trace element geochemistry,and geochronological characteristics of the volcanic rocks,with the aim of elucidating their magmatic source,petrogenesis,and tectonic setting.The results indicate that the Man-ketou'ebo Formation volcanic rocks have SiO2 contents ranging from 76.82%to 77.82%,Al2O3 con-tents ranging from 11.83%to 12.55%,K2O contents ranging from 1.50%to 4.72%,and Na2O con-tents ranging from 3.10%to 5.24%,classifying them as high-potassium calcalkaline aluminosilicate rocks.The total rare earth element(REE)content is(102.54-141.50)×10-6,which is enrichment of light rare earth elements,mass fraction of LREEs is(95.75-132.66)×10-6 and heavy rare earth element deficit,mass fraction of HREEs is(6.79-9.87)×10-6.The rocks show enrichment in elements such as Rb,K,Th,La,Ce,Nd,and Hf,while Ba,Sr,Nb,P,and Ti are depleted.A pronounced negative Eu anomaly is also observed.Geochemical evidence suggests that the volcanic magma originated from partial melting of crustal material with sedimentary input.The zircon U-Pb age of(164.6±1.8)Ma was obtained from the acidic volcanic rocks of the Manketou'ebo Formation,which was formed in the Late Jurassic.The tectonic environment of the Manketou'ebo Formation is interpreted as an active continental margin related to the subduction of the Paleo-Pacific Plate.These findings provide critical insights into the chronology and tectonic framework of the volcanic belt in the Great Xing'an Range.

关键词

火山岩/锆石U-Pb年龄/地球化学特征/构造环境/晚侏罗世/满克头鄂博组/呼中地区/大兴安岭

Key words

volcanic rock/zircon U-Pb age/geochemical characteristics/tectonic setting/Late Jurassic/Manketou'ebo Formation/Huzhong Area/Great Xing'an Range

分类

天文与地球科学

引用本文复制引用

于跃江,李慧,李新鹏,江峰,梁景龙,李金明,卜程丹..大兴安岭呼中地区满克头鄂博组火山岩地球化学特征、锆石U-Pb年龄及构造环境[J].东北石油大学学报,2025,49(3):29-40,12.

基金项目

黑龙江省1∶5万区域地质矿产调查项目(HLJKD2015-07) (HLJKD2015-07)

东北石油大学学报

OA北大核心

2095-4107

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