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Structural constraints on the evolution of the Central Asian Orogenic Belt in SW Mongolia
ArticleAbstract: We provide a detailed description of the structures along a 300 km long and 50 km wide transect acroPalabras claves:40 39 Ar/ Ar geochronology, Building of the Central Asian Orogenic Belt, Mongolia, Oroclinal bending, Structural geologyAutores:Alfred Kron̈er, Corsini M., Lehmann J., Lexa O., Otgonbator D., Schulmann K., Štípská P., Tomurhuu D.Fuentes:scopusTiming of accretion and collisional deformation in the Central Asian Orogenic Belt: Implications of granite geochronology in the Bayankhongor Ophiolite Zone
ArticleAbstract: Growing evidence suggests that the mechanism of Palaeozoic continental growth in Central Asia was byPalabras claves:Central Asian Orogenic Belt, Mongolia, Ophiolites, Zircon geochronologyAutores:Alfred Kron̈er, Brewer T.S., Buchan C., Cunningham W.D., Pfander J., Tomurhuu D., Tomurtogoo O., Windley B.F.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