Laboratory measurements of ‘porosity-free’ intrinsicVpandVsin an olivine gabbro of the Oman ophiolite: Implication for interpretation of the seismic structure of lower oceanic crust-Reference-Cited by-同舟云学术

Laboratory measurements of ‘porosity-free’ intrinsicVpandVsin an olivine gabbro of the Oman ophiolite: Implication for interpretation of the seismic structure of lower oceanic crust

Published:2015-05-28 Issue:2 Volume:24 Page:131-144
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Saito Satoshi¹²,Ishikawa Masahiro³,Arima Makoto³,Tatsumi Yoshiyuki¹⁴

Affiliation:

1. Institute for Research on Earth Evolution; Japan Agency for Marine-Earth Science and Technology; 2-15 Natsushima-cho Yokosuka Kanagawa 237-0061 Japan

2. Department of Earth Sciences, Graduate School of Science and Engineering; Ehime University; 2-5 Bunkyo-cho Matsuyama Ehime 790-8577 Japan

3. Graduate School of Environment and Information Sciences; Yokohama National University; Tokiwadai Hodogaya-ku Yokohama Kanagawa 240-8501 Japan

4. Department of Earth and Planetary Sciences, Faculty of Science; Kobe University; Nada-ku Kobe Hyogo 657-8501 Japan

Funder

Japan Society for the Promotion of Science

Publisher

Wiley

Subject

Geology

Reference38 articles.

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3. Magma chambers in the Oman ophiolite: Fed from the top and the bottom;Boudier;Earth and Planetary Science Letters,1996

4. How crack porosity and shape control seismic velocities in the upper oceanic crust: Modeling downhole logs from Holes 504B and 1256D;Carlson;Geochemistry Geophysics Geosystems,2010

5. The influence of porosity and crack morphology on seismic velocity and permeability in the upper oceanic crust;Carlson;Geochemistry Geophysics Geosystems,2014

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