Sedimentary Evolution and Provenance of the late Permian‐middle Triassic Raggyorcaka Deposits in North Qiangtang (Tibet, Western China): Evidence for a Forearc Basin of the Longmu Co‐Shuanghu Tethys Ocean

The tectonic origin of the >500‐km‐long E‐W trending Central Qiangtang metamorphic belt (CQMB), which separates the North Qiangtang block (NQB) and South Qiangtang block (SQB), remains controversial. Moreover, the coeval geological evolution of the southern NQB has been poorly investigated, parti...

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Veröffentlicht in:	Tectonics (Washington, D.C.) D.C.), 2020-01, Vol.39 (1), p.n/a
Hauptverfasser:	Liang, Xiao, Sun, Xihui, Wang, Genhou, Gao, Jinhan, An, Xingyu
Format:	Artikel
Sprache:	eng
Schlagworte:	Carboniferous Central Qiangtang metamorphic belt Continental margins detrital zircon Evolution forearc basin Forearc basins Geological time Isotopes Oceans Paleoceanography Paleozoic Permian Sandstone Sedimentary rocks sedimentation Sequencing Subduction tectonics Tethys Ocean Triassic Zircon
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