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
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