2023
DOI: 10.1016/j.geogeo.2023.100178
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Detrital zircon U–Pb geochronology and fluvial basin evolution of the Liuqu Conglomerate within the Yarlung Zangbo Suture Zone: A critical geochronometer for the collision tectonics of the Tibetan-Himalayan Orogenic Belt

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Cited by 3 publications
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“…Conversely, in the Eastern Asian section of the Tethyan Orogenic Belt (i.e. Tibetan sector), an Andean-type orogeny along the southern margin of Eurasia from the Early Jurassic to the Early Cretaceous has been proposed to explain deformation and sedimentation patterns in the southern Tibetan Plateau (Kapp et al, 2007;Zhang et al, 2012;Xie and Dilek, 2023). This process was punctuated by Toarcian-Aalenian back-arc rifting event resulting from retreat of the subducting Neo-Tethyan seafloor (Hou et al, 2015;Wei et al, 2017).…”
Section: Introductionmentioning
confidence: 99%
“…Conversely, in the Eastern Asian section of the Tethyan Orogenic Belt (i.e. Tibetan sector), an Andean-type orogeny along the southern margin of Eurasia from the Early Jurassic to the Early Cretaceous has been proposed to explain deformation and sedimentation patterns in the southern Tibetan Plateau (Kapp et al, 2007;Zhang et al, 2012;Xie and Dilek, 2023). This process was punctuated by Toarcian-Aalenian back-arc rifting event resulting from retreat of the subducting Neo-Tethyan seafloor (Hou et al, 2015;Wei et al, 2017).…”
Section: Introductionmentioning
confidence: 99%