Continental Crust Rejuvenation Across the Paleo‐Mesoarchean Transition Resulted From Elevated Mantle Geotherms

Continental Crust Rejuvenation Across the Paleo‐Mesoarchean Transition Resulted From Elevated Mantle Geotherms

Abstract The increase in initial Hf isotopes identified in early Mesoarchean detrital zircon is commonly interpreted as a reflection of the geodynamic transition from stagnant‐lid to mobile‐lid tectonics. However, given the lack of petrogenetic context, interpreting detrital zircon may lead to spuri...

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Bibliographic Details
Main Authors: Gui‐Mei Lu, Yi‐Gang Xu, Wei Wang, Christopher J. Spencer, Guangyu Huang, Nick M. W. Roberts
Format: Article
Language:English
Published: Wiley 2024-04-01
Series:Geophysical Research Letters
Subjects:
continental crust rejuvenation
elevated mantle geotherms
Yangtze Block
Paleo‐Mesoarchean transition
Online Access:https://doi.org/10.1029/2024GL108715

Internet

https://doi.org/10.1029/2024GL108715

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