Schematic models of accretionary wedges in forearc basins. (A) Single‐wedge model with asymmetrical doubly vergent (singly vergent) uplift. (B) Two‐wedge model with symmetrical doubly vergent uplift. (C) Strike‐slip model.
Atsushi Noda, Ayumu Miyakawa
CC BY 3.0
Deposition and Deformation of Modern Accretionary-Type Forearc Basins: Linking Basin Formation and Accretionary Wedge Growth, Evolutionary Models of Convergent Margins - Origin of Their Diversity, Yasuto Itoh, IntechOpen, 2017, DOI: 10.5772/67559. Available from: <a rel="nofollow" class="external free" href="https://www.intechopen.com/books/evolutionary-models-of-convergent-margins-origin-of-their-diversity/deposition-and-deformation-of-modern-accretionary-type-forearc-basins-linking-basin-formation-and-ac">https://www.intechopen.com/books/evolutionary-models-of-convergent-margins-origin-of-their-diversity/deposition-and-deformation-of-modern-accretionary-type-forearc-basins-linking-basin-formation-and-ac</a>