Effects of Alteration and Cracks on the Seismic Velocity Structure of Oceanic Lithosphere Inferred From Ultrasonic Measurements of Mafic and Ultramafic Samples Collected by the Oman Drilling Project-Reference-Cited by-同舟云学术

Effects of Alteration and Cracks on the Seismic Velocity Structure of Oceanic Lithosphere Inferred From Ultrasonic Measurements of Mafic and Ultramafic Samples Collected by the Oman Drilling Project

Published:2021-11 Issue:11 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Hatakeyama Kohei¹²^ORCID,Katayama Ikuo¹^ORCID,Abe Natsue³⁴^ORCID,Okazaki Keishi⁵^ORCID,Michibayashi Katsuyoshi⁶⁷,

Affiliation:

1. Department of Earth and Planetary Systems Science Hiroshima University Hiroshima Japan

2. Now at Department of Education Meisei University Tokyo Japan

3. Mantle Drilling Promotion Office MarE3 JAMSTEC Yokohama Japan

4. Division of Natural System, Graduate School of Natural Science & Technology Kanazawa University Kanazawa Japan

5. Kochi Institute for Core Sample Research X‐star JAMSTEC Kochi Japan

6. Department of Earth and Planetary Sciences Graduate School of Environmental Studies Nagoya University Nagoya Japan

7. Research Institute for Marine Geodynamics JAMSTEC Yokosuka Japan

Funder

Japan Science Society

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB021923

Reference69 articles.

1. Atomistic calculations of structural and elastic properties of serpentine minerals: the case of lizardite

2. Relationship between seismic P-wave velocity and the composition of anhydrous igneous and meta-igneous rocks

3. Serpentine Mineral Replacements of Natural Olivine and their Seismic Implications: Oceanic Lizardite versus Subduction-Related Antigorite

4. Influence of fluids on VP/VS ratio: increase or decrease?

5. Elastic moduli of a cracked solid

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