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Zircon ages for a felsic volcanic rock and arc-related early Palaeozoic sediments on the margin of the Baydrag microcontinent, central Asian orogenic belt, Mongolia
ArticleAbstract: Magmatic zircons from the basal part of an arc terrane in the accretionary complex NE of the BaydragPalabras claves:Central Asian Orogenic Belt, Detrital zircon age, MongoliaAutores:Alfred Kron̈er, Barth M., Demoux A., Jian P., Tomurhuu D., Yamirka Rojas-Agramonte, Zack T.Fuentes:scopusZircon ages from the baydrag block and the bayankhongor ophiolite zone: Time constraints on late neoproterozoic to cambrian subduction- and accretion-related magmatism in central Mongolia
ArticleAbstract: Central Mongolia represents a heterogeneous crustal domain of the Central Asian Orogenic Belt and isPalabras claves:Appendix, Color figureAutores:Alfred Kron̈er, Badarch G., Demoux A., Jian P., Tomurhuu D., Wingate M.T.D.Fuentes:scopusZircon ages of the Bayankhongor ophiolite mélange and associated rocks: Time constraints on Neoproterozoic to Cambrian accretionary and collisional orogenesis in Central Mongolia
ArticleAbstract: Central Mongolia is geologically characterized by close juxtaposition of an accreted oceanic terranePalabras claves:Accretion-collision, Central Asian Orogenic Belt, Mongolia, Ophiolite, Syenite porphyry, zirconAutores:Alfred Kron̈er, Jian P., Liu D.Y., Miao L., Shi Y., Tomurhuu D., Windley B.F., Zhang F., Zhang W.Fuentes:scopus