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<md:name>National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan</md:name>
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<md:affiliation id="dataset.author75976.inst20476">
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<md:lastName>Grant</md:lastName>
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<md:name>British Geological Survey, The Lyell Centre</md:name>
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<md:name>Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan</md:name>
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<md:name>Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan</md:name>
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<md:lastName>Bellanova</md:lastName>
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<md:name>Neotectonics and Natural Hazards Group, RWTH Aachen University</md:name>
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<md:lastName>Brunet</md:lastName>
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<md:name>CNRS, Geoscience Department, University of Rennes 1</md:name>
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<md:lastName>Cai</md:lastName>
<md:firstName>Zhirong</md:firstName>
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<md:name>Division of Earth and Planetary Sciences, Kyoto University</md:name>
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<md:name>Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan</md:name>
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<md:author id="dataset.author75465">
<md:lastName>Huang</md:lastName>
<md:firstName>Jyh-Jaan Steven</md:firstName>
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<md:affiliation id="dataset.author75465.inst21940">
<md:name>Department of Geology, University of Innsbruck</md:name>
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<md:author id="dataset.author109689">
<md:lastName>Ishizawa</md:lastName>
<md:firstName>Tahashi</md:firstName>
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<md:name>International Research Institute of Disaster Science, Tohoku University</md:name>
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<md:lastName>Itaki</md:lastName>
<md:firstName>Takuya</md:firstName>
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<md:orcid>0000-0001-5232-0055</md:orcid>
<md:affiliation id="dataset.author39883.inst21948">
<md:name>National Institute of Advanced Industrial Science and Technology</md:name>
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<md:firstName>Kana</md:firstName>
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<md:name>Faculty of Science and Engineering, Waseda University</md:name>
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<md:author id="dataset.author83420">
<md:lastName>Johnson</md:lastName>
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<md:orcid>0000-0002-5671-7209</md:orcid>
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<md:name>Department of Earth Sciences University of New Hampshire, USA</md:name>
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<md:lastName>Kanamatsu</md:lastName>
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<md:name>Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan</md:name>
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<md:lastName>Keep</md:lastName>
<md:firstName>Myra</md:firstName>
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<md:name>School of Earth Sciences University of Western Australia Australia</md:name>
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<md:firstName>Arata</md:firstName>
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<md:affiliation id="dataset.author109692.inst21952">
<md:name>Department of Earth Resources Engineering Kyushu University Japan</md:name>
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<md:firstName>Martin</md:firstName>
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<md:lastName>Luo</md:lastName>
<md:firstName>Min</md:firstName>
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<md:orcid>0000-0002-2856-3951</md:orcid>
<md:affiliation id="dataset.author75072.inst21953">
<md:name>College of Marine Sciences Shanghai Ocean University China</md:name>
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<md:URI>http://sites.google.com/site/thediljemer/</md:URI>
<md:affiliation id="dataset.author32299.inst21954">
<md:name>Institute for Geosciences University of Bonn Germany</md:name>
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<md:lastName>McHugh</md:lastName>
<md:firstName>Cecilia M G</md:firstName>
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<md:name>School of Earth and Environmental Sciences Queens College</md:name>
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<md:lastName>Micallef</md:lastName>
<md:firstName>Aaron</md:firstName>
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<md:name>GEOMAR - Helmholtz Centre for Ocean Research Kiel</md:name>
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<md:name>Faculty of Symbiotic Systems Science Fukushima University Japan</md:name>
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<md:lastName>Pandey</md:lastName>
<md:firstName>Dhananjai K</md:firstName>
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<md:orcid>0000-0001-6899-8995</md:orcid>
<md:affiliation id="dataset.author60001.inst21167">
<md:name>National Centre for Polar and Ocean Research, Ministry of Earth Sciences</md:name>
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<md:orcid>0000-0003-4701-0372</md:orcid>
<md:affiliation id="dataset.author34988.inst2974">
<md:name>CNRS, Geoscience Department, University of Rennes 1</md:name>
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<md:name>Marine Sciences Research Center, Stony Brook University</md:name>
<md:URI>http://www.msrc.sunysb.edu/</md:URI>
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<md:name>Boone Pickens School of Geology, Oklahoma State University</md:name>
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<md:orcid>0000-0002-2485-8015</md:orcid>
<md:affiliation id="dataset.author83558.inst21958">
<md:name>Lake Biwa Museum</md:name>
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<md:affiliation id="dataset.author109694.inst21959">
<md:name>School of Earth Sciences, The Ohio State University</md:name>
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<md:firstName>Chloé</md:firstName>
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<md:affiliation id="dataset.author60272.inst24">
<md:name>Lamont-Doherty Earth Observatory of Columbia University, New York</md:name>
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<md:firstName>Maxwell</md:firstName>
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<md:affiliation id="dataset.author109695.inst21960">
<md:name>Colorado School of Mines</md:name>
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<md:firstName>Susanne M</md:firstName>
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<md:affiliation id="dataset.author463.inst24">
<md:name>Lamont-Doherty Earth Observatory of Columbia University, New York</md:name>
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<md:name>Geological Survey of Finland</md:name>
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<md:firstName>Yong Hong</md:firstName>
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<md:affiliation id="dataset.author109696.inst21961">
<md:name>College of Marine Geosciences, Ocean University of China</md:name>
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<md:firstName>Ting-Wei</md:firstName>
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<md:affiliation id="dataset.author59306.inst1093">
<md:name>Norwegian Geotechnical Institute</md:name>
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<md:affiliation id="dataset.author59306.inst277">
<md:name>MARUM - Center for Marine Environmental Sciences, University Bremen</md:name>
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<md:lastName>Zellers</md:lastName>
<md:firstName>Sarah D</md:firstName>
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<md:affiliation id="dataset.author28941.inst21962">
<md:name>Department of Physical Sciences, University of Central Missouri</md:name>
<md:ROR>https://ror.org/02c63wv67</md:ROR>
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<md:year>2025</md:year>
<md:title>Shear strength (shear vane) from IODP Hole 386-M0089C</md:title>
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<md:URI>https://doi.org/10.1594/PANGAEA.975377</md:URI>
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<md:abstract>Shear strength from automated shear vane (AVS) of the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). This dataset was obtained at the end of the core processing workflow during the third phase (Personal Sampling Party, PSP) of expedition 386, which took place between 2022-11-15 – 2022-11-30 onboard D/V Chikyu. Measurements were performed on the work halves of core sections using a Wykeham-Farrance AVS. The apparatus consists of four vanes perpendicular to each other that are inserted in the sediment to their full length while attempting to minimize disturbance to the sediment. A motor loads a helical torsion spring and the bottom of the spring is united to the vane. Therefore, the bottom deflection of the spring records the angular displacement of the sediment, from which undrained shear strength has been calculated. Measurements were attempted approx. every 2 m throughout the core, though, some lithologies, especially in the upper few meters were too soft to obtain reasonable results. These core depths are blank in the Shear strength [kPa] column of the presented dataset.
For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023</md:abstract>
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<md:title>Japan Trench Paleoseismology</md:title>
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<md:source>Proceedings of the International Ocean Discovery Program, International Ocean Discovery Program</md:source>
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<md:comment>Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management  (https://www.ecord.org).</md:comment>
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