Fine structure beneath the Tohoku district, northeastern Japan arc, as derived by an inversion of P-wave arrival times from local earthquakes
- 1 February 1984
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 101 (3-4), 245-265
- https://doi.org/10.1016/0040-1951(84)90116-1
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Observations of shear-wave velocity polarization anisotropy beneath Honshu,Japan: Two masses with different polarizations in the upper mantle.Journal of Physics of the Earth, 1982
- Two-dimensional depth structure of the crust beneath the Tohoku District,the northeastern Japan arc Part II. Moho discontinuity and P-wave velocity.Journal of Physics of the Earth, 1982
- Three-dimensional velocity structure beneath the Kanto district, Japan.Journal of Physics of the Earth, 1982
- Three-dimensional shear velocity structure beneath the Japan islands and its tectonic implications.Journal of Physics of the Earth, 1980
- Deep structure under Yellowstone National Park U.S.A.: A continental “hot spot”Tectonophysics, 1979
- Velocity structure of the crust beneath the northeastern part of Honshu, Japan, as derived from local earthquake data.Journal of Physics of the Earth, 1979
- A large-scale three-dimensional seismic structure under the Japan Islands and the sea of Japan.Journal of Physics of the Earth, 1977
- Magma Beneath Yellowstone National ParkScience, 1975
- The upper mantle beneath Japan inferred from P traveltime anomalies by means of three dimensional ray tracing. I.Journal of Physics of the Earth, 1973
- Partial melting and the low-velocity zonePhysics of the Earth and Planetary Interiors, 1970