@ALomaxNet @JudithGeology @otreborilisab @seismo_steve The general point was to constrain the slab in aseismic regions (essentially 200/250 km to 500 km depth). The precise weightings for hypocenter vs tomography used to calculate Slab2 can be found in an
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@widjokongko @SjofjanCh @infoBMKG @BNPB_Indonesia @infomitigasi @infobencana @aw3126 here is the open source paper by @gph_seismo https://t.co/bZycPxnUbK gis service https://t.co/DG0zEEtkO8 and the data https://t.co/44QzVBLmO1
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USGS Pub https://t.co/jftUKbcRBN via @USGS_Pubs WHAT!
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An interesting approach to (finally!) quantifying where subducting oceanic plates may be from tomography: Incorporating teleseismic tomography data into models of upper mantle slab geometry | Geophysical Journal International | Oxford Academic https://t.c