Wadati-Benioff zone


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Wadati-Benioff zone

[¦wä¦dä·tē ′ben·ē‚ȯf ‚zōn]
(geophysics)
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References in periodicals archive ?
Stress Field in the Ryukyu--Kyushu Wadati-Benioff Zone by Inversion of Earthquake Focal Mechanisms, Tectonophysics, 384: 1-4, 175-189.
Space distribution ofthe contemporary stress field in the Izu-Bonin Wadati-Benioff zone by inversion of earthquake focal mechanisms, Journal of Geodynamics, 39: 413-428.
Contemporary Stress Field in the Wadati-Benioff Zone at the Japan-Kurile arc-arc junction (North Honshu, the Hokkaido corner and Hokkaido Island) by Inversion of Earthquake Focal Mechanisms".
Stress field in the Vanuatu (New Hebrides) Wadati-Benioff zone inferred by inversion of earthquake focal mechanisms: evidence for systematic lateral and vertical variations of principal stresses.
Depth distribution of stresses in the Hokkaido Wadati-Benioff zone as deduced by inversion of earthquake focal mechanisms.
Morphology of the Wadati-Benioff zone in the Hellenic arc.
Studies on the present-day geodynamics in worldwide Wadati-Benioff zones (WBZ) are carried out to examine their contemporary geodynamics.
The studied Wadati-Benioff zones are as follows: the Aegean (Christova and Nikolova, 1998; Vanek et al.
High resolution determination of the Wadati-Benioff zone geometry in central Peru, Revista Brasilera de Geofisica, 9, 141-159.