Thermal state and evolving geodynamic regimes of the Meso- to Neoarchean North China Craton

Constraining the thermal state of the lithosphere is crucial to understanding geodynamic regime in early Earth. Here the authors reconstruct ~2.9–2.5 Ga thermal structure of continental lithosphere of the North China Craton using TTG and propose a systematic Archean geodynamic evolution process.

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Autores principales: Guozheng Sun, Shuwen Liu, Peter A. Cawood, Ming Tang, Jeroen van Hunen, Lei Gao, Yalu Hu, Fangyang Hu
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/832dd3c7d0e54372be6138c6394da17b
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Sumario:Constraining the thermal state of the lithosphere is crucial to understanding geodynamic regime in early Earth. Here the authors reconstruct ~2.9–2.5 Ga thermal structure of continental lithosphere of the North China Craton using TTG and propose a systematic Archean geodynamic evolution process.