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The cessation of igneous activity and uplift when an actively spreading ridge is subducted beneath an island arc
Authors:Soichi  Osozawa
Affiliation:Institute of Geology and Paleontology, Faculty of Science, Tohoku University, Sendai 980, Japan
Abstract:Abstract Ridge subduction and the resulting formation of a slab window interrupts volcanic arc-type igneous activity and causes uplift of the arc system. These implied diachronous relationships are examined by comparison of the temporal and spatial positions of ancient migrated trench-trench-ridge triple junctions and the distribution of subduction-related igneous and metamorphic rocks in Japan.
Keywords:arc magmatism    diachronous    metamorphism    ridge subduction    slab window    triple junction    uplift
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