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Accretionary growth and crust formation in the Central Asian Orogenic Belt and comparison with the Arabian-Nubian shield
Conference ObjectAbstract: The Central Asian Orogenic Belt is one of the largest accretionary terrains on Earth and records a cPalabras claves:Accretion, Arabian-Nubian Shield, Central Asia, Kazakhstan, Mongolia, Zircon geochronologyAutores:Alfred Kron̈er, Badarch G., Demoux A., Gruschka S., Hegner E., Jahn B.m., Khain E.V., Tomurtogoo O., Windley B.F., Wingate M.T.D.Fuentes:scopusAccretionary orogens through Earth history
ArticleAbstract: Accretionary orogens form at intraoceanic and continental margin convergent plate boundaries. They iPalabras claves:Autores:Alfred Kron̈er, Cawood P.A., Collins W.J., Kusky T.M., Mooney W.D., Windley B.F.Fuentes:scopusEvolution of a Permian intraoceanic arc-trench system in the Solonker suture zone, Central Asian Orogenic Belt, China and Mongolia
ArticleAbstract: The identification of a fossil arc-trench system from the ophiolite-decorated Solonker suture zone iPalabras claves:CAOB, Forearc mélange, Ophiolite, Plate convergence, Proto-arc crust, zircon datingAutores:Alfred Kron̈er, Jian P., Liu D.Y., Miao L., Shi Y., Tomurhuu D., Windley B.F., Zhang F., Zhang L., Zhang W.Fuentes:scopusUnderstanding and study perspectives on tectonic evolution and crustal structure of the Paleozoic Chinese Tianshan
ReviewAbstract: The Chinese Tianshan Belt is one of the key regions for the understanding of tectonics of the CentraPalabras claves:Autores:Alfred Kron̈er, Charvet J., Chen Y., Choulet F., Faure M., Gao J., Glen R., Jian P., Li J., Lin W., Ma H., Natal'in B., Plag H.P., Quinn C., Seltmann R., Shang Q., Shu L., Wan B., Wang B., Wang Q., WILDE S.A., Windley B.F., Xiao W., Yamirka Rojas-Agramonte, Zhang W.Fuentes:scopusSubduction-Accretion History of the Central Asian Orogenic Belt: Constraints from Mongolia
ArticleAbstract:Palabras claves:Autores:Alfred Kron̈er, Badarch G., Buchan A.C., Cunningham W.D., Salnikova E.B., Tomurtogoo O., Windley B.F.Fuentes:scopusTectonic models for accretion of the Central Asian Orogenic Belt
ReviewAbstract: The Central Asian Orogenic Belt (c. 1000-250 Ma) formed by accretion of island arcs, ophiolites, ocePalabras claves:Autores:Alexeiev D.V., Alfred Kron̈er, Badarch G., Windley B.F., Xiao W.Fuentes:scopusThe Tectonic Architecture of Central Madagascar: Implication on the Evolution of the East African Orogeny
ArticleAbstract:Palabras claves:Autores:Alfred Kron̈er, Collins A.S., Fitzsimons I., Hulscher B., Windley B.F.Fuentes:scopusThe tectonic framework of Mongolia and contiguous regions in the context of the crustal evolution of the Central Asian Orogenic Belt
ArticleAbstract:Palabras claves:Autores:Alfred Kron̈er, Badarch G., Cunningham W.D., Tomurtogoo O., Windley B.F., Xiao W.Fuentes:scopus