Radiogenic Heating as the Thermal Driver of Himalayan Crustal Heating During Prolonged Thickening

Abstract The thermal evolution of the crust during continental collision evolves from cold to hot with time, which impacts crustal reworking and differentiation. However, it remains elusive as to the mechanism driving the crust to be hot during the protracted collision. Here, we describe crust therm...

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Prif Awduron:	Shuaiqi Liu, Guibin Zhang, Lifei Zhang, Shuzhen Wang, Feng Chang
Fformat:	Artigo
Iaith:	Inglês
Cyhoeddwyd:	Wiley 2025-11-01
Cyfres:	Geochemistry, Geophysics, Geosystems
Pynciau:	metamorphism thermal evolution Himalayan orogen geochronology phase equilibria modeling partial melting
Mynediad Ar-lein:	https://doi.org/10.1029/2025GC012590
Tagiau:	Ychwanegu Tag Dim Tagiau, Byddwch y cyntaf i dagio'r cofnod hwn!