TY - JOUR
T1 - Dehydration and earthquakes in the subducting slab
T2 - Empirical link in intermediate and deep seismic zones
AU - Omori, S.
AU - Komabayashi, T.
AU - Maruyama, S.
PY - 2004/8/16
Y1 - 2004/8/16
N2 - In this study, a close link between the depth-distribution of subduction-zone earthquakes and dehydration events in the hydrated slab-peridotite is established. A phase diagram up to 27 GPa in the MgO-AlO-SiO-HO (MASH) system was constructed using a combination of thermodynamic calculation and Schreinemakers analysis on previous experimental data. At intermediate-depths (
AB - In this study, a close link between the depth-distribution of subduction-zone earthquakes and dehydration events in the hydrated slab-peridotite is established. A phase diagram up to 27 GPa in the MgO-AlO-SiO-HO (MASH) system was constructed using a combination of thermodynamic calculation and Schreinemakers analysis on previous experimental data. At intermediate-depths (
UR - http://www.scopus.com/inward/record.url?eid=2-s2.0-2542486322&partnerID=8YFLogxK
U2 - 10.1016/j.pepi.2003.08.014
DO - 10.1016/j.pepi.2003.08.014
M3 - Article
AN - SCOPUS:2542486322
SN - 0031-9201
VL - 146
SP - 297
EP - 311
JO - Physics of the Earth and Planetary Interiors
JF - Physics of the Earth and Planetary Interiors
IS - 1-2
ER -