Eastward Growth of the Tibetan Plateau Linked to Cenozoic Orogenic Wedge Deformation and Fluctuating Melt Sources

Abstract The India–Asia collision continuously loads the Tibetan Plateau (TP), driving its Cenozoic eastward growth. This process has caused extensive crustal deformation and a diverse magmatic response. Here, we report on newly identified 35−6.5 Ma granitoids from Kangding area in southeastern (SE)...

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Бібліографічні деталі
Автори:	Quan Ou, Jia‐Jing Mei, Derek A. Wyman, Jian‐Qing Lai, Feng Zi, Kun Wang, Jing‐Yi Liu, Jia Liao, Zhiwu Li
Формат:	Artigo
Мова:	Inglês
Опубліковано:	Wiley 2026-06-01
Серія:	Geochemistry, Geophysics, Geosystems
Предмети:	silicon isotope Kangding Cenozoic granitoid metasedimentary materials contribution secularly fluctuating melt source stress overload zone eastward growth of Tibetan Plateau
Онлайн доступ:	https://doi.org/10.1029/2025GC012820
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Eastward Growth of the Tibetan Plateau Linked to Cenozoic Orogenic Wedge Deformation and Fluctuating Melt Sources

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