世界地质2024,Vol.43Issue(1) :1-18.DOI:10.3969/j.issn.1004-5589.2024.01.001

大兴安岭阿尔山地区宝力高庙组浅变质岩年代学、地球化学特征及原岩建造探讨

Chronology,geochemical characteristics and protolith formation of low-grade metamorphic rocks from Baoligaomiao Formation in Aershan area,Da Hinggan Ling(Mts.)

王之晟 高天栋 王洪志 郭恒飞 马振宇 于兵
世界地质2024,Vol.43Issue(1) :1-18.DOI:10.3969/j.issn.1004-5589.2024.01.001

大兴安岭阿尔山地区宝力高庙组浅变质岩年代学、地球化学特征及原岩建造探讨

Chronology,geochemical characteristics and protolith formation of low-grade metamorphic rocks from Baoligaomiao Formation in Aershan area,Da Hinggan Ling(Mts.)

王之晟 1高天栋 1王洪志 1郭恒飞 1马振宇 1于兵1
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作者信息

  • 1. 核工业二四三大队,内蒙古赤峰 024000
  • 折叠

摘要

大兴安岭阿尔山地区宝力高庙组为一套以沉积碎屑岩、安山岩为主的陆相沉积-火山岩系,经历了区域变质作用后转变为低绿片岩相.笔者对宝力高庙组浅变质岩开展了锆石U-Pb定年、地球化学的研究,结合岩性岩相学和变质变形特征,试图恢复其原岩建造,并在此基础上,探讨了沉积背景.结果表明,阿尔山地区变质安山岩LA-ICP-MS锆石U-Pb年龄为(312.1±1.2)Ma,地质时代属晚石炭世—早二叠世,将其厘定为宝力高庙组,原岩组合属典型的滨湖相陆源中酸性火山-沉积建造,沉积构造环境为活动大陆边缘的弧内盆地,与区域上二连—贺根山蛇绿—增生杂岩带晚石炭世—早二叠世时期的构造环境一致.

Abstract

The Baoligaomiao Formation,located in the Arshan area of the Da Hinggan Ling(Mts.),compri-ses a continental sedimentary-volcanic rock series,predominantly formed of sedimentary clastic rocks and andes-ites,which have undergone regional metamorphism and have been converted into the low greenschist facies.This study focuses on the zircon U-Pb dating and geochemical analysis of the low-grade metamorphic rocks of Baoligao-miaoFormation.By integrating lithologic petrographosed and metamorphic deformation characteristics,the research aims to reconstruct the protolith structure and explore the sedimentary setting.The results indicate that the LA-ICP-MS zircon U-Pb age of the metamorphic andesites in the Arshan area is approximately(312.1±1.2)Ma,belonging to the Late Carboniferous and Early Permian periods,and it is identified as part of Baoligaomiao Forma-tion.The protolith assemblage of Baoligaomiao Formation in the Arshan area is a typical terrigenous intermediate-acidic volcano-sedimentary lacustrine facies.The sedimentary tectonic environment is the intra-arc basin of the ac-tive continental margin,which is consistent with the tectonic environment of the Late Carboniferous-Early Permian in Erlian-Hegenshan ophiolite-accretionary complex.

关键词

宝力高庙组/锆石U-Pb定年/原岩建造/弧内盆地/阿尔山地区

Key words

Baoligaomiao Formation/zircon U-Pb dating/protolith formation/intra-arc basin/Aershan area

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基金项目

&&(202001)

出版年

2024
世界地质
吉林大学 东北亚国际地学研究与教学中心

世界地质

CSTPCD
影响因子:0.769
ISSN:1004-5589
被引量1
参考文献量31
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