Early Permian Sunidyouqi suprasubduction-zone ophiolites in the central Solonker suture zone (Inner Mongolia, China)

Different final closing ages have been proposed for the evolution of the Paleo-Asian Ocean (PAO), including Late Silurian, pre-Late Devonian, Early Permian, Late-Permian and Late Permian–Early Triassic. Ophiolites represent fragments of ancient oceanic crust and play an important role in identifying...

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Veröffentlicht in:	Di xue qian yuan. 2019-05, Vol.10 (3), p.1101-1111
Hauptverfasser:	Xu, Guo, Liu, Huichuan, Li, Yinglei, Xu, Zhan, Xie, Yan
Format:	Artikel
Sprache:	eng
Schlagworte:	Anomalies Geochemistry Geochronology Magma Niobium North China Craton Oceans Ophiolite Orogeny Paleo-Asian Ocean Solonker SSZ Subduction (geology) Tantalum Tectonics
Online-Zugang:	Volltext
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