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Okinawa trough backarc basin: Early tectonic and magmatic evolution
ArticleAbstract: The Okinawa Trough, lying between Japan and Taiwan, is a backarc basin formed by extension within thPalabras claves:Autores:Angelier J., Deffontaines B., Dominguez S., Fournier M., Hsu S.K., Jean Yves Collot, Lallernand S., Le Formal J.P., Liu C.S., Lu C.Y., Malavielle J., Schnürle P., Sibuet J.C., Thareau N., Wang C.Fuentes:scopusTrench-parallel stretching and folding of forearc basins and lateral migration of the accretionary wedge in the southern Ryukyus: A case of strain partition caused by oblique convergence
ArticleAbstract: Detailed seafloor mapping in the area east of Taiwan revealed trench-parallel stretching and foldingPalabras claves:Autores:Angelier J., Deffontaines B., Dominguez S., Fournier M., Hsu S.K., Jean Yves Collot, Lallemand S.E., Le Formal J.P., Liu C.S., Liu S.Y., Lu C.Y., Malavielle J., Schnürle P., Sibuet J.C., Thareau N., Wang F.Fuentes:scopus