Dispersion of regional body waves at 100–150 km depth beneath Alaska: In situ constraints on metamorphism of subducted crust
- 15 May 1996
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 23 (10) , 1171-1174
- https://doi.org/10.1029/96gl00974
Abstract
No abstract availableThis publication has 19 references indexed in Scilit:
- A program for seismic wavefield modeling using finite-difference techniquesComputers & Geosciences, 1996
- H2O transport and release in subduction zones: Experimental constraints on basaltic and andesitic systemsJournal of Geophysical Research, 1995
- Interslab earthquakes and phase changes in subducting lithosphereReviews of Geophysics, 1995
- Tomographic imaging of the Alaska subduction zoneJournal of Geophysical Research, 1995
- Deep structure of Japan subduction zone as derived from local, regional, and teleseismic eventsJournal of Geophysical Research, 1994
- Three‐dimensional inversion of regional P and S arrival times in the East Aleutians and sources of subduction zone gravity highsJournal of Geophysical Research, 1994
- Seismological constraints on the gabbro-eclogite transition in subducted oceanic crustEarth and Planetary Science Letters, 1994
- P-wave velocity structure inside the subducting Pacific plate beneath the Japan regionPhysics of the Earth and Planetary Interiors, 1991
- Deep-Focus Earthquakes and Recycling of Water into the Earth's MantleScience, 1991
- Gabbro‐eclogite reaction rate and its geophysical significanceReviews of Geophysics, 1975