Late Cretaceous Intraplate Mafic Dyke Swarms in the East Kunlun Orogen, Northern Tibetan Plateau: Implications for Lithospheric Reactivation and Early Surface Uplift

The Cretaceous represents a key period in the geodynamic evolution of the Tibetan Plateau and the initial development of its paleotopography. While widespread orogenesis and magmatism associated with the Lhasa–Qiangtang collision are well documented in southern Tibet, coeval magmatic records in nort...

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Príomhchruthaitheoirí:	Denghui Chen, Hao Wu, Wei Wang, Yujie Zhao, Huajun Wen, Dongming Jiang, Xiaotong Sun, Fuhao Xiong
Formáid:	Artigo
Teanga:	Inglês
Foilsithe / Cruthaithe:	MDPI AG 2026-05-01
Sraith:	Geosciences
Ábhair:	Cretaceous magmatism mafic dyke swarms lithospheric reactivation intraplate extension Northern Tibetan Plateau
Rochtain ar líne:	https://www.mdpi.com/2076-3263/16/5/201
Clibeanna:	Cuir clib leis Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!