Abstract
Abstract Internal structure and recent tectonics of the geologically complex Banda Arc region (latitude 1–9°S, longitude 124–135°E) have been studied by means of the analysis of global seismological data. Relocated hypocentral determinations of the International Seismological Center (EHB data) and fault plane solutions of the Global Centroid Moment Tensor Project have been used together with previously published information on regional geology and dynamics. The analysis considered earthquakes in the lithospheric wedges above subducting slabs and earthquakes in the uppermost portions of the Wadati–Benioff zones (focal depth
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