%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Widiyantoro, S.
%A Ramdhan, M.
%A Métaxian, Jean-Philippe
%A Cummins, P. R.
%A Martel, C.
%A Erdmann, S.
%A Nugraha, A. D.
%A Budi-Santoso, A.
%A Laurin, Antoine
%A Fahmi, A. A.
%T Seismic imaging and petrology explain highly explosive eruptions of Merapi Volcano, Indonesia
%D 2018
%L fdi:010074033
%G ENG
%J Scientific Reports - Nature
%@ 2045-2322
%K INDONESIE
%K MERAPI VOLCAN
%M ISI:000444374900007
%P art. 13656 [7]
%R 10.1038/s41598-018-31293-w
%U https://www.documentation.ird.fr/hor/fdi:010074033
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers18-09/010074033.pdf
%V 8
%W Horizon (IRD)
%X Our seismic tomographic images characterize, for the first time, spatial and volumetric details of the subvertical magma plumbing system of Merapi Volcano. We present P-and S-wave arrival time data, which were collected in a dense seismic network, known as DOMERAPI, installed around the volcano for 18 months. The P-and S-wave arrival time data with similar path coverage reveal a high Vp/Vs structure extending from a depth of >= 20 km below mean sea level (MSL) up to the summit of the volcano. Combined with results of petrological studies, our seismic tomography data allow us to propose: (1) the existence of a shallow zone of intense fluid percolation, directly below the summit of the volcano; (2) a main, pre-eruptive magma reservoir at >= 10 to 20 km below MSL that is orders of magnitude larger than erupted magma volumes; (3) a deep magma reservoir at MOHO depth which supplies the main reservoir; and (4) an extensive, subvertical fluid-magma-transfer zone from the mantle to the surface. Such high-resolution spatial constraints on the volcano plumbing system as shown are an important advance in our ability to forecast and to mitigate the hazard potential of Merapi's future eruptions.
%$ 066 ; 064