Fate of Forearc lithosphere at arc‐continent collision zones: Evidence from local earthquake tomography of the Sunda‐Banda Arc Transition, Indonesia.

Fate of Forearc lithosphere at arc‐continent collision zones: Evidence from local earthquake tomography of the Sunda‐Banda Arc Transition, Indonesia.

Supendi, P., Nugraha, A.D., Widiyantoro, S., Abdullah, C.I., Rawlinson, N., Cummins, P.R., Harris, C.W., Roosmawati, N. and Miller, M.S.,

Geophysical Research Letters, (Q1)
47(6), p.e2019GL086472.
2020.

A new 3‐D seismic P wave velocity model of the Sunda‐Banda Arc Transition from local earthquake tomography reveals (i) northward subduction of oceanic lithosphere, associated with the convergence of Australia and Sundaland, as a high‐velocity zone extending down to ~200 km depth; (ii) two distinct low‐velocity zones, one immediately above the slab, which is likely a zone of partial melt, and one in the 0–40 km depth range, which is probably a magma chamber associated with active volcanoes above; and (iii) a northerly dipping high‐velocity zone that bisects the two low‐velocity anomalies, which we interpret as an underthrust forearc sliver of continental origin. Based on He3/He4 measurements from volcanic outflows, it is possible that the magma supply is contaminated by interaction with this forearc sliver as it ascends from the melt region below.

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