Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Seismic velocity structure of the subducting Pacific plate in the Izu-Bonin region

Journal Article · · Journal of Geophysical Research; (United States)
DOI:https://doi.org/10.1029/92JB01336· OSTI ID:6994606
Observed travel time residual data from a spatially dense seismic network above deep earthquakes in the Izu-Bonin region are compared with 3D ray tracing calculations. The data are inconsistent with a homogeneous slab model and consistent with a heterogenous slab model with regional velocity variations. The residual data can be explained by a model that has a velocity gradient within the slab. In the subducting Pacific plate, the velocity near the center of the slab is faster than that near the upper boundary, and gradually decreases toward the bottom of the plate. A model with a velocity decrease of 3 percent, as predicted by a thermal profile, explains the observed data. 52 refs.
OSTI ID:
6994606
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 97; ISSN JGREA2; ISSN 0148-0227
Country of Publication:
United States
Language:
English

Similar Records

Origin of Izu-Bonin forearc submarine canyons
Conference · Fri Jun 01 00:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA) · OSTI ID:6317117

Results of ODP Leg 125 drilling in the Mariana/Izu-Bonin forearcs
Conference · Fri Jun 01 00:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA) · OSTI ID:6317127

Multiple plates subducting beneath Colombia, as illuminated by seismicity and velocity from the joint inversion of seismic and gravity data
Journal Article · Mon Apr 11 20:00:00 EDT 2016 · Earth and Planetary Science Letters · OSTI ID:1255155