2022
DOI: 10.1002/gj.4490
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Eogene to Neogene north‐eastward expansion of the arcuate tectonic belt in north‐east Tibetan Plateau: Constraints from detrital zircon geochronology and heavy minerals

Abstract: The north‐eastward extrusion of the Tibetan Plateau has always been under debate. The arcuate tectonic belt is located at the north‐east margin of the Tibetan Plateau and bears crucial information about the tectonic and geomorphic evolution of north‐east Tibetan Plateau. Combined with sedimentary sequence, detrital zircon U–Pb geochronology, and heavy mineral combinations, significant provenance transformation can be determined both in the south‐west and north‐east of the arcuate tectonic belt during the Eocen… Show more

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