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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: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:lastName>Huang</md:lastName>
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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">
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<md:name>International Research Institute of Disaster Science, Tohoku University</md:name>
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<md:name>National Institute of Advanced Industrial Science and Technology</md:name>
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<md:name>Faculty of Science and Engineering, Waseda University</md:name>
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<md:lastName>Johnson</md:lastName>
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<md:name>Department of Earth Sciences University of New Hampshire, USA</md:name>
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<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:affiliation id="dataset.author109692.inst21952">
<md:name>Department of Earth Resources Engineering Kyushu University Japan</md:name>
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<md:firstName>Min</md:firstName>
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<md:orcid>0000-0002-2856-3951</md:orcid>
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<md:name>College of Marine Sciences Shanghai Ocean University China</md:name>
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<md:name>Institute for Geosciences University of Bonn Germany</md:name>
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<md:name>School of Earth and Environmental Sciences Queens College</md:name>
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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:orcid>0000-0001-6899-8995</md:orcid>
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<md:name>National Centre for Polar and Ocean Research, Ministry of Earth Sciences</md:name>
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<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: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: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:name>Lamont-Doherty Earth Observatory of Columbia University, New York</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:author id="dataset.author59306">
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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 (fall cone) from IODP Hole 386-M0090C</md:title>
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<md:URI>https://doi.org/10.1594/PANGAEA.975447</md:URI>
<md:dateTime>2025-02-26T10:31:30</md:dateTime>
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<md:abstract>Undrained shear strength data from fall cone testing 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 at an interval of approx. 1 meter using an ELE International fall cone penetrometer (STANDARD BS1377) with the following cone specifications: 35 mm cone, 30 degrees angle, around 30 g, stainless steel, 3.25 (+/-0.05) mm rod diameter. The fall cone penetrometer measures the penetration of a cone as it free falls and embeds itself in the sediment. During testing, the cone (pointing downward) was lowered, so that it just touched the surface of the split core before it was locked in place with the dial gauge reading noted. Undrained shear strength was determined using the empirical formula determined by Hansbo (1957, http://urn.kb.se/resolve?urn=urn:nbn:se:swedgeo:diva-356). The formula of Hansbo (1957) may be inadequate for silty sediment (present in some Expedition 386 cores); therefore, fall cone measurements were obtained preferably in clay-dominated intervals. In three cases (386-M0081B-1H-21,25.5; 386-M0088D-1H-7,25.5; 386-M0091B-1H-10,25.5), data collection was not successful for different reasons (IT problems, human failure). For the sake of completeness, however, the "Sample labels" were nevertheless noted and results left empty.
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:author id="ref131047.author36007">
<md:lastName>Strasser</md:lastName>
<md:firstName>Michael</md:firstName>
<md:eMail>michael.strasser@uibk.ac.at</md:eMail>
<md:orcid>0000-0003-3991-2405</md:orcid>
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<md:author id="ref131047.author30530">
<md:lastName>Ikehara</md:lastName>
<md:firstName>Ken</md:firstName>
<md:eMail>k-ikehara@aist.go.jp</md:eMail>
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<md:author id="ref131047.author68403">
<md:lastName>Everest</md:lastName>
<md:firstName>Jeremy D</md:firstName>
<md:eMail>dev@bgs.ac.uk</md:eMail>
<md:orcid>0000-0002-3455-7494</md:orcid>
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<md:author id="ref131047.author108945">
<md:lastName>IODP Expedition 386 Scientists</md:lastName>
</md:author>
<md:year>2023</md:year>
<md:title>Japan Trench Paleoseismology</md:title>
<md:type id="ref131047.reftype14">book</md:type>
<md:source>Proceedings of the International Ocean Discovery Program, International Ocean Discovery Program</md:source>
<md:volume>386</md:volume>
<md:URI>https://doi.org/10.14379/iodp.proc.386.2023</md:URI>
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<md:extent>
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<md:northBoundLatitude>38.29531667</md:northBoundLatitude>
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<md:meanLatitude>38.29531667</md:meanLatitude>
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<md:elevation geocodeId="geocode1" name="DEPTH, sediment/rock" unit="m">
<md:min>0.255</md:min>
<md:max>0.255</md:max>
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<md:label>IODP</md:label>
<md:name>Integrated Ocean Drilling Program / International Ocean Discovery Program</md:name>
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<md:dateTime>2021-05-28T00:00:00</md:dateTime>
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<md:chiefScientist>Strasser, Michael</md:chiefScientist>
<md:chiefScientist>Ikehara, Ken</md:chiefScientist>
<md:start>2021-04-13</md:start>
<md:end>2021-06-01</md:end>
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<md:name>Kaimei</md:name>
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<md:comment>IGSN: IBCR0386EHZ6001. Comment: 1.5 m. Location: applied ship's position due to malfunctioning GPC transponder.</md:comment>
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<md:size unit="data points">3</md:size>
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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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<md:history datetime="2026-02-10T13:34:39">"Penetration depth" were corrected by dividing them by a factor of ten.</md:history>
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