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Convergent margin key elements and systematics
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           Distal back-arc:                                 Magmatic arc:                 Accretionary wedge: cold, inherent
           transition to                              hot, igneous-dominated              strong syn-
           intraplate                                                                     sedimentary shortening
                              Back-arc basin:                                             deformation, amagmatic

                              hot, syn-sediment                                           (thickening crust)
                              magmatism, extension                                                         Intraplate: cold,

                              weak/strong deformation                                                      undeformed,
                                                                                                           amagmatic































                           (Stern, 2002)






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