Wallace, L M; Araki, Eiichiro; Saffer, Demian M; Wang, Xiaoming; Rösner, Alexander; Kopf, Achim J; Nakanishi, A; Power, William L; Kobayashi, R; Kinoshita, Chihiro; Toczko, Sean; Kimura, Toshinori; Machida, Shiki; Carr, Stephanie A (2016): Pressure and temperature from the borehole observatory of IODP Hole 332-C0010A. PANGAEA, https://doi.org/10.1594/PANGAEA.874291, Supplement to: Wallace, LM et al. (2016): Near-field observations of an offshore Mw 6.0 earthquake from an integrated seafloor and subseafloor monitoring network at the Nankai Trough, southwest Japan. Journal of Geophysical Research: Solid Earth, 121(11), 8338-8351, https://doi.org/10.1002/2016JB013417
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An Mw 6.0 earthquake struck ~50 km offshore the Kii Peninsula of southwest Honshu, Japan on 1 April 2016. This earthquake occurred directly beneath a cabled offshore monitoring network at the Nankai Trough subduction zone and within 25-35 km of two borehole observatories installed as part of the International Ocean Discovery Program's NanTroSEIZE project. The earthquake's location close to the seafloor and subseafloor network offers a unique opportunity to evaluate dense seafloor geodetic and seismological data in the near field of a moderate-sized offshore earthquake. We use the offshore seismic network to locate the main shock and aftershocks, seafloor pressure sensors, and borehole observatory data to determine the detailed distribution of seafloor and subseafloor deformation, and seafloor pressure observations to model the resulting tsunami. Contractional strain estimated from formation pore pressure records in the borehole observatories (equivalent to 0.37 to 0.15 µstrain) provides a key to narrowing the possible range of fault plane solutions. Together, these data show that the rupture occurred on a landward dipping thrust fault at 9-10 km below the seafloor, most likely on the plate interface. Pore pressure changes recorded in one of the observatories also provide evidence for significant afterslip for at least a few days following the main shock. The earthquake and its aftershocks are located within the coseismic slip region of the 1944 Tonankai earthquake (Mw ~8.0), and immediately downdip of swarms of very low frequency earthquakes in this region, illustrating the complex distribution of megathrust slip behavior at a dominantly locked seismogenic zone.
Latitude: 32.209968 * Longitude: 136.686540
Date/Time Start: 2016-03-31T00:00:00 * Date/Time End: 2016-04-01T08:38:00
Minimum Elevation: -2552.0 m * Maximum Elevation: -2552.0 m
|#||Name||Short Name||Unit||Principal Investigator||Method/Device||Comment|
|2||Temperature, technical||T tech||°C||Rösner, Alexander||Platinumchip|
|3||Temperature, technical||T tech||°C||Rösner, Alexander||Absolute pressure gauges (APG)||Hydrostatic APG|
|4||In-situ pressure||Sigma||kPa||Rösner, Alexander||Formation|
|5||In-situ pressure||Sigma||kPa||Rösner, Alexander||Hydrostatic|
15668 data points