期刊
GEOPHYSICAL RESEARCH LETTERS
卷 46, 期 4, 页码 2025-2036出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2018GL080025
关键词
Japan and North Izu; double seismic zone; adjoint tomography; intermediate-depth and deep earthquakes; seismogenesis; fluid-related embrittlement
资金
- NSF [ACI-1053575, 1802247]
- Romanian MNESR-STAR grant [513]
- JST-JICA SATREPS grant [1554361]
- Directorate For Geosciences
- Division Of Earth Sciences [1802247] Funding Source: National Science Foundation
The distribution of intermediate-depth and deep intraslab earthquakes with respect to subducting slabs offers a unique insight into seismogenesis at high pressures and temperatures that should inhibit brittle failure. This study constrains the surface of the subducting Pacific Plate beneath Japan at depths between 100 and 380 km based on a previous continental-scale adjoint tomography model. Earthquake distributions relative to the slab surface reveal double seismic zones located within the top 60 km of the Pacific Plate. Thermal modeling suggests that the lower-plane seismicity corresponds to temperatures between 400 and 900 degrees C. The seismogenic pressure and temperature conditions correlate approximately with the conditions of dehydration reactions of several hydrous minerals, that is, antigorite (serpentine) and chlorite at depths between 100 and 200 km and phase A at greater depths between 200 and 380 km. These correlations indicate that at these depths water released from dehydration processes may facilitate triggering slab mantle earthquakes.
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