Paleozoic accretionary orogenic mechanism in the eastern part of Xing-Meng Orogenic Belt: Geological evolution evidence from Zhalantun island arc in the northern part of the Daxing'an Mountains

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Publication Details

Journal
Acta Petrologica Sinica
Published
2025-01-01
DOI
https://doi.org/10.18654/1000-0569/2025.08.17
Primary Topic
Geochemistry and Geochronology of Asian Mineral Deposits
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article
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article

Paleozoic accretionary orogenic mechanism in the eastern part of Xing-Meng Orogenic Belt: Geological evolution evidence from Zhalantun island arc in the northern part of the Daxing'an Mountains

Xiaoping Yang, Yanqing Zang, FU JunYu, Cheng Qian et al.
Acta Petrologica Sinica
Geochemistry and Geochronology of Asian Mineral Deposits
article

Paleozoic accretionary orogenic mechanism in the eastern part of Xing-Meng Orogenic Belt: Geological evolution evidence from Zhalantun island arc in the northern part of the Daxing'an Mountains

Xiaoping Yang, Yanqing Zang, FU JunYu, Cheng Qian, Tao Qin, Yujin Zhang, Yan Wang
article en

Abstract

No abstract available for this paper.
Acta Petrologica SinicaVol. 41(8)
Life below water
Openalex Percentile: Top 74%
Geochemistry and Geochronology of Asian Mineral Deposits
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Paleozoic accretionary orogenic mechanism in the eastern part of Xing-Meng Orogenic Belt: Geological evolution evidence from Zhalantun island arc in the northern part of the Daxing'an Mountains — Xiaoping Yang, Yanqing Zang, et al. · Acta Petrologica Sinica (2025) | TGRS Research Map | TGRS