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Strasser, Michael; Ikehara, Ken; Everest, Jeremy D; Maeda, Lena; Hochmuth, Katharina; Grant, Hannah; Stewart, Margaret S; Sakurai, Noriaki; Yokoyama, Takahiro; Bao, Rui; Bellanova, Piero; Brunet, Morgane; Cai, Zhirong; Cattaneo, Antonio; Hsiung, Kan-Hsi; Huang, Jyh-Jaan Steven; Ishizawa, Tahashi; Itaki, Takuya; Jitsuno, Kana; Johnson, Joel E; Kanamatsu, Toshiya; Keep, Myra; Kioka, Arata; Kölling, Martin; Luo, Min; März, Christian; McHugh, Cecilia M G; Micallef, Aaron; Nagahashi, Yoshitaka; Pandey, Dhananjai K; Proust, Jean-Noël; Rasbury, Troy; Riedinger, Natascha; Satoguchi, Yasufumi; Sawyer, Derek E.; Seibert, Chloé; Silver, Maxwell; Straub, Susanne M; Virtasalo, Joonas J; Wang, Yong Hong; Wu, Ting-Wei; Zellers, Sarah D (2025): Natural remanent magnetization data from IODP Hole 386-M0092C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.979794

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Published: 2025-03-20 • DOI registered: 2025-04-19

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Abstract:
Natural remanent magnetization (NRM) data from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. Because the diameter of the split section (12.5 cm) is larger than the magnetometer entrance (8.1 cm), U-channel samples were taken from the center of each working half during the onshore phase. Measurements were conducted likewise during the onshore phase using the long-core superconducting rock magnetometer (2G Enterprises, model 760) installed on D/V Chikyu. Due to time constraints paleomagnetism measurements were limited to NRM with 5 mT demagnetization, with measurements typically made at 2 cm intervals. Because linearity is difficult to calculate for short cores, such as trigger cores, corrections of declination were not performed for these cores.
For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
Keyword(s):
International Ocean Discovery Program (IODP); IODP; Japan Trench; Paleomagnetic data
Related to:
Strasser, Michael; Ikehara, Ken; Everest, Jeremy D; IODP Expedition 386 Scientists (2023): Japan Trench Paleoseismology. Proceedings of the International Ocean Discovery Program, International Ocean Discovery Program, 386, https://doi.org/10.14379/iodp.proc.386.2023
Project(s):
Integrated Ocean Drilling Program / International Ocean Discovery Program (IODP)
Coverage:
Latitude: 36.911050 * Longitude: 143.423850
Date/Time Start: 2021-05-25T00:00:00 * Date/Time End: 2021-05-25T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.62 m
Event(s):
386-M0092C (JTPS-06B)  * Latitude: 36.911050 * Longitude: 143.423850 * Date/Time Start: 2021-05-25T00:00:00 * Date/Time End: 2021-05-25T00:00:00 * Elevation: -7700.0 m * Location: Japan Trench * Campaign: Exp386 * Basis: Kaimei * Method/Device: Trigger corer (TC) * Comment: IGSN: IBCR0386EH96001. Comment: 1.5 m. Location: applied ship'sposition due to malfunctioning GPC transponder.
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).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1 Event labelEvent
2 Sample code/labelSample labelDSDP/ODP/IODP sample designation
3 DEPTH, sediment/rockDepth sedmGeocode
4 InclinationIncldegSuperconducting Rock Magnetometer (SRM), 2G Enterprises, 760
5 DeclinationDecldegSuperconducting Rock Magnetometer (SRM), 2G Enterprises, 760
6 IntensityIntensityA/mSuperconducting Rock Magnetometer (SRM), 2G Enterprises, 760
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
128 data points

Data

Download dataset as tab-delimited text — use the following character encoding:

1 
Event		2 
Sample label		3 
Depth sed [m]		4 
Incl [deg]		5 
Decl [deg]		6 
Intensity [A/m]
386-M0092C 386-M0092C-1P-1,00.0062.12309.887.65E-06
386-M0092C386-M0092C-1P-1,20.0253.39263.871.54E-05
386-M0092C386-M0092C-1P-1,40.0446.74247.722.69E-05
386-M0092C386-M0092C-1P-1,60.0642.85240.263.97E-05
386-M0092C386-M0092C-1P-1,80.0840.59236.665.17E-05
386-M0092C386-M0092C-1P-1,100.1039.69235.626.13E-05
386-M0092C386-M0092C-1P-1,120.1239.58234.886.90E-05
386-M0092C386-M0092C-1P-1,140.1440.26234.317.45E-05
386-M0092C386-M0092C-1P-1,160.1641.38233.497.80E-05
386-M0092C386-M0092C-1P-1,180.1842.57233.077.99E-05
386-M0092C386-M0092C-1P-1,200.2043.78232.727.97E-05
386-M0092C386-M0092C-1P-1,220.2244.50232.857.82E-05
386-M0092C386-M0092C-1P-1,240.2444.87233.807.61E-05
386-M0092C386-M0092C-1P-1,260.2644.85235.437.42E-05
386-M0092C386-M0092C-1P-1,280.2844.66237.587.27E-05
386-M0092C386-M0092C-1P-1,300.3044.46239.657.09E-05
386-M0092C386-M0092C-1P-1,320.3244.73241.426.79E-05
386-M0092C386-M0092C-1P-1,340.3445.36242.346.39E-05
386-M0092C386-M0092C-1P-1,360.3648.22240.925.77E-05
386-M0092C386-M0092C-1P-1,380.3846.99243.325.58E-05
386-M0092C386-M0092C-1P-1,400.4047.01242.105.30E-05
386-M0092C386-M0092C-1P-1,420.4246.78239.475.07E-05
386-M0092C386-M0092C-1P-1,440.4446.49236.754.84E-05
386-M0092C386-M0092C-1P-1,460.4646.23234.744.58E-05
386-M0092C386-M0092C-1P-1,480.4846.13233.804.31E-05
386-M0092C386-M0092C-1P-1,500.5045.39233.114.11E-05
386-M0092C386-M0092C-1P-1,520.5243.40232.824.06E-05
386-M0092C386-M0092C-1P-1,540.5440.28232.704.18E-05
386-M0092C386-M0092C-1P-1,560.5637.23233.034.32E-05
386-M0092C386-M0092C-1P-1,580.5835.38233.414.20E-05
386-M0092C386-M0092C-1P-1,600.6035.54234.153.60E-05
386-M0092C386-M0092C-1P-1,620.6238.38233.562.60E-05