Geochemical anomaly in ancient subduction boundary fault: Trench-parallel heterogeneity in slip behavior caused by variation of mineral composition

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    W[2017AGUFM.H43G1721M]
    LA["Linked Authors (0)"]
    LI["Linked Institutions (6)"]
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ADS bibcode

2017AGUFM.H43G1721M

year

2017

Listed Authors

Macente, A.

Vanorio, T.

Miller, K. J.

Fusseis, F.

Ogawa, T.

Ishikawa, T.

Kaneki, S.

Hirono, T.

Listed Institutions

Stanford Earth Sciences, Stanford, CA, United States

Geophysics Department, SRPL - Stanford Rock Physics Laboratory, Stanford University, Stanford, CA, United States

Stanford University, Stanford, CA, United States

University of Edinburgh, Edinburgh, United Kingdom

Osaka University, Osaka, Japan

JAMSTEC, Nankoku, Kochi, Japan

Osaka University, Osaka, Japan

Osaka University, Osaka, Japan

Linked Authors [?]

Linked Institutions

• JAMSTEC, Kochi Institute for Core Sample Research
• Osaka University, Japan
• Stanford University, California
• Stanford University, Department of Geophysics
• Stanford University, School of Earth Sciences
• University of Edinburgh, UK