Abstract
Compressional wave velocity and the preferred orientation of olivine of Hidaka Horoman dunite (sample name HD 20 A) were measured. Fabrics of compressional wave velocity of the dunite and preferred orientation of olivine in the dunite are shown. These fabrics are closely related to each other. Olivine crystallographic “a” axis concentrated about the tectonic X axis. Maximum compressional velocity is 8.8km/s and minimum one is 7.9km/s.
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More From: Zisin (Journal of the Seismological Society of Japan. 2nd ser.)
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