Tetsuro Hirono
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View article: Effect of Surface Hardness of Wooden Baseball Bat on Restitution Performance
Effect of Surface Hardness of Wooden Baseball Bat on Restitution Performance Open
View article: Enhanced solar modulation performance of VO2-based smart windows with insertion of ultrathin TiOx layer
Enhanced solar modulation performance of VO2-based smart windows with insertion of ultrathin TiOx layer Open
View article: Geochemical signals of high-temperature fluid–rock interactions in a mélange unit, Japan: Implications for geochemical reactions along major subduction-related faults
Geochemical signals of high-temperature fluid–rock interactions in a mélange unit, Japan: Implications for geochemical reactions along major subduction-related faults Open
To understand the slip behavior and characteristics of major faults within subduction-related mélange units, we performed microscopic observations and mineralogical and chemical analyses of a primary slip zone and its surrounding host rock…
View article: How Friction and Pore-Fluid Pressure Conditions Controlled by Fault Mineral Composition Affect Earthquake Rupture Propagation
How Friction and Pore-Fluid Pressure Conditions Controlled by Fault Mineral Composition Affect Earthquake Rupture Propagation Open
Although direct recovery of frictional features of fault rocks through drilling projects and multiple experimental analyses, such as the Japan Trench Fast Drilling Project and the Nankai Trough Seismogenic Zone Experiment have been recentl…
View article: Characteristics of Fault Rocks Within the Aftershock Cloud of the 2014 Orkney Earthquake (M5.5) Beneath the Moab Khotsong Gold Mine, South Africa
Characteristics of Fault Rocks Within the Aftershock Cloud of the 2014 Orkney Earthquake (M5.5) Beneath the Moab Khotsong Gold Mine, South Africa Open
Cores recovered during the International Continental Scientific Drilling Program project “Drilling into Seismogenic zones of M2.0 to M5.5 earthquakes in deep South African Gold Mines” include fault breccia from within the aftershock cloud …
View article: Friction and Pore-Fluid Pressure Conditions in Faults Controlling Earthquake Rupture Dynamics
Friction and Pore-Fluid Pressure Conditions in Faults Controlling Earthquake Rupture Dynamics Open
Although direct recovery of frictional features of fault rocks through drilling projects and multiple experimental analyses such as the Japan Trench Fast Drilling Project (JFAST) and the Nankai Trough Seismogenic Zone Experiment (NanTroSEI…
View article: ODP Leg 185, Hole 801C - Well Logging Data
ODP Leg 185, Hole 801C - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: ODP Leg 185, Hole 1149B - Well Logging Data
ODP Leg 185, Hole 1149B - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: ODP Leg 185, Hole 1149B - Well Logging Data
ODP Leg 185, Hole 1149B - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: ODP Leg 185, Hole 801C - Well Logging Data
ODP Leg 185, Hole 801C - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0006B - Well Logging Data
IODP Expedition 314, Hole C0006B - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0006B - Well Logging Data
IODP Expedition 314, Hole C0006B - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: Experimental and numerical demonstrations for development of composite planar fabrics in fault zones
Experimental and numerical demonstrations for development of composite planar fabrics in fault zones Open
<p>Many experimental works have previously performed to understand frictional properties of various kinds of rocks and minerals by using friction apparatus at various orders of sliding velocities ranging from nm/s to m/s together wit…
View article: Generation of sintered fault rock and its implications for earthquake energetics and fault healing
Generation of sintered fault rock and its implications for earthquake energetics and fault healing Open
After an earthquake, faults can recover strength through fault healing, but the mechanisms responsible are not well understood. Seismic slip may induce sintering, a bonding process between solid particles in contact under high temperatures…
View article: IODP Expedition 314, Hole C0003A - Well Logging Data
IODP Expedition 314, Hole C0003A - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0002A - Well Logging Data
IODP Expedition 314, Hole C0002A - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0001D - Well Logging Data
IODP Expedition 314, Hole C0001D - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0001D - Well Logging Data
IODP Expedition 314, Hole C0001D - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0003A - Well Logging Data
IODP Expedition 314, Hole C0003A - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0004B - Well Logging Data
IODP Expedition 314, Hole C0004B - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0002A - Well Logging Data
IODP Expedition 314, Hole C0002A - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: IODP Expedition 314, Hole C0004B - Well Logging Data
IODP Expedition 314, Hole C0004B - Well Logging Data Open
Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, …
View article: Sintered fault rock from the Taiwan Chelungpu fault
Sintered fault rock from the Taiwan Chelungpu fault Open
Law data of TEM, XRD, TG-DSC, and chemical kinetic analyses
View article: Sintered fault rock from the Taiwan Chelungpu fault
Sintered fault rock from the Taiwan Chelungpu fault Open
Law data of TEM, XRD, TG-DSC, and chemical kinetic analyses
View article: The seismogenic zones of an M2.0-5.5 earthquakes successfully recovered in deep South African gold mines: the outcomes and the follow-up plan
The seismogenic zones of an M2.0-5.5 earthquakes successfully recovered in deep South African gold mines: the outcomes and the follow-up plan Open
<p>This paper reports on the outcomes of the ICDP drilling into seismogenic zones of M2.0-5.5 earthquakes in South African (SA) gold mines (DSeis; 2017-2018), the follow-up work in 2019, and planned post-drilling activity from 2020 o…
View article: Diagenetic and shear-induced transitions of frictional strength of carbon-bearing faults and their implications for earthquake rupture dynamics in subduction zones
Diagenetic and shear-induced transitions of frictional strength of carbon-bearing faults and their implications for earthquake rupture dynamics in subduction zones Open
Subduction-related diagenetic reactions affect fault strength and are thus important for understanding earthquake rupture dynamics in subduction zones. Carbonaceous material (CM) is found worldwide in active plate-boundary and intracontine…
View article: Role of Weak Materials in Earthquake Rupture Dynamics
Role of Weak Materials in Earthquake Rupture Dynamics Open
Weak materials in seismic slip zones are important in studies of earthquake mechanics. For instance, the exceptionally large slip during the 2011 Tohoku-Oki earthquake has been attributed to the presence of smectite in the fault zone. Howe…
View article: Kinetic effect of heating rate on the thermal maturity of carbonaceous material as an indicator of frictional heat during earthquakes
Kinetic effect of heating rate on the thermal maturity of carbonaceous material as an indicator of frictional heat during earthquakes Open
View article: Slip parameters on major thrusts at a convergent plate boundary: regional heterogeneity of potential slip distance at the shallow portion of the subducting plate
Slip parameters on major thrusts at a convergent plate boundary: regional heterogeneity of potential slip distance at the shallow portion of the subducting plate Open
View article: Mechanochemical Effect on Maturation of Carbonaceous Material: Implications for Thermal Maturity as a Proxy for Temperature in Estimation of Coseismic Slip Parameters
Mechanochemical Effect on Maturation of Carbonaceous Material: Implications for Thermal Maturity as a Proxy for Temperature in Estimation of Coseismic Slip Parameters Open
Because shear stress in a fault is directly related to the frictional heat generated during slip, the thermal maturity of carbonaceous material has been used as a proxy for fault‐rock temperature. We used infrared and Raman spectroscopic a…