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大兴安岭哈多河地区早石炭世侵入岩成因及其地质意义

梁天意 谢园宏 董洋 韩学智 姜兆元 杨拓 陈方浦 李文龙

地质论评2025,Vol.71Issue(4):1159-1176,18.
地质论评2025,Vol.71Issue(4):1159-1176,18.DOI:10.16509/j.georeview.2024.10.025

大兴安岭哈多河地区早石炭世侵入岩成因及其地质意义

Genesis and geological significance of Early Carboniferous intrusive rocks in Haduohe area of the Great Hinggan Mountains

梁天意 1谢园宏 1董洋 2韩学智 1姜兆元 1杨拓 1陈方浦 1李文龙1

作者信息

  • 1. 辽宁省化工地质勘查院有限责任公司,辽宁锦州,121000
  • 2. 鞍山师范学院,辽宁鞍山,114056
  • 折叠

摘要

Abstract

Haduohe area is located in the middle of the Great Hinggan Mountains,the Erlian-Hegenshan-Heihe tectonic belt lies on its south side,this area is an ideal place to study the tectonic evolution of the ancient Asian Ocean,it can further reveal the collision-splicing process of Xingan block and Songnen block in the Late Paleozoic and provide new evidence of the demise of the ancient Asian Ocean.Based on the field work,through the microscope observation,the whole rock chemical analysis and LA-ICP-MS U-Pb zircon dating of the late Paleozoic intrusive rocks in Haduohe area.According to the test analysis results,the weighted average ages of Two stage intrusive rocks are respectively(352.1±1.7)Ma and(339.1±4.2)Ma,the ages belongs to the early Carboniferous.The average SiO2 content of medium coarse monzogranite is 73.11%,the average Al2O3 content is 13.47%,the average total alkali(ALK)content is 8.74%,the average Na2O/K2O is 1.13,which belongs to the metatretic substance.The average SiO2 content of medium-fine monzogranite is 71.98%,the average Al2O3 content is 13.82%,the average total alkali(ALK)content is 8.94%,the average Na2O/K2O is 1.15,which belongs to the metatretic substance,both of them are high potassium calc-alkaline series rocks.Two stage intrusive rocks are enriched in light rare earth and deficient in heavy rare earth,the distribution pattern of rare earth is right-leaning,which Enrichment of LILE(Rb、K、U)and Loss of HFSE(Nb、Zr、P、Ti),also have obvious Eu negative anomaly,which shows the characteristics of I-type granite.Combined with previous research results,the early Carboniferous intrusive rocks in Haduohe area were formed by magmatic tectonic events under island arc background,it indicates that Xingan block and Songnen block were still in the collision and merging process in the Early Carboniferous,the ancient Asian ocean is closing up and dying.

关键词

大兴安岭/早石炭世/侵入岩/年代学/地球化学/构造环境

Key words

the Great Hinggan Mountains/Early Carboniferous/intrusive rocks/chronology/geochemical/tectonic environment

引用本文复制引用

梁天意,谢园宏,董洋,韩学智,姜兆元,杨拓,陈方浦,李文龙..大兴安岭哈多河地区早石炭世侵入岩成因及其地质意义[J].地质论评,2025,71(4):1159-1176,18.

基金项目

本文为中国地质调查局"内蒙古1∶5万钓鱼台等四幅区域地质调查"项目(编号:DD20160201-07)的成果. This study was supported by"Inner Mongolia 1∶50000 Diaoyutai and Other Three Regional Geological Survey"of China Geological Survey(No.DD20160201-07) (编号:DD20160201-07)

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