Hiroki Sone
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Mineralogy Controls on Injection‐Induced Fault Slip Open
Fault rocks vary in mineralogy but understanding the role of mineralogy in injection‐induced fault slip behavior remains challenging. We conduct laboratory fluid injection experiments on representative faults with distinct surface mineralo…
View article: Potential for Continental Scientific Drilling to Inform Fault Mechanics and Earthquake Science
Potential for Continental Scientific Drilling to Inform Fault Mechanics and Earthquake Science Open
Our understanding of fault mechanics and earthquake processes remains limited, largely due to minimal direct observations near active faults at seismogenic depths. This lack of data restricts our ability to accurately assess and mitigate b…
Mechanical properties of Indonesian organic-rich shales from the Central Sumatra and North Sumatra Basin, and comparison with US shales Open
Mechanical characterization of shales is a fundamental requirement in optimizing shale resource development and transferring development strategies between shale plays. Here we report the laboratory-based mechanical properties of Indonesia…
Time‐Dependent Deformation in the Damage Zone of the Chelungpu Fault System and Potential Stress Relaxation Open
High fracture density in fault damage zones not only reduces the elastic stiffness of rocks but may also promote time‐dependent bulk deformation through the sliding of fracture and thus alter the stress in fault zones. On comparing the dam…
Enhanced Microseismicity During Production Pumping Cessation at the San Emidio Geothermal Field (Nevada, USA) in December 2016 Open
Tectonic activity, geothermal fluids, and microseismic events (MSEs) tend to occur in similar locations as a result of spatiotemporal changes in the subsurface stress state. To quantify this association, we analyze data from a dense seismi…
Evidence of stress relaxation caused by time-dependent deformation in the damage zone of the Chelungpu fault system Open
High fracture density in fault damage zones not only reduces the elastic stiffness of rocks but may also promote time-dependent bulk deformation through the sliding of fracture surfaces and thus impact the stress evolution in fault zones. …
Lithology and Fault‐Related Stress Variations Along the TCDP Boreholes: The Stress State Before and After the 1999 Chi‐Chi Earthquake Open
Understanding the stress state before and after an earthquake is essential to study how stress on faults evolves during the seismic cycle. This study integrates wellbore failure analysis, laboratory experiments, and edge dislocation model …
Strength data for article titled "Lithology and fault related stress variations along the TCDP borehole: the stress state before and after the Chi-Chi earthquake. Journal of Geophysical Research: Solid Earth" Open
Understanding the stress state before and after an earthquake is essential to study how stress on faults evolve during the seismic cycle. This study integrates wellbore failure analysis, laboratory experiments, and edge dislocation model t…
Hydraulic fracturing experiments at 1500 m depth in a deep mine: Highlights from the kISMET project Open
In support of the U.S. DOE SubTER Crosscut initiative, we established a field test facility in a deep mine and designed and carried out in situ hydraulic fracturing experiments relevant to enhanced geothermal systems (EGS) in crystalline r…
Comparison of Biotite Elastic Properties Recovered by Spherical Nanoindentations and Atomistic Simulations — Influence of Nano‐Scale Defects in Phyllosilicates Open
Phyllosilicate minerals, due to their sheets structure and morphology, are known to cause anisotropy in bulk rock properties and make the bulk rock more compliant. Accurately characterizing the micromechanical behavior of phyllosilicate mi…
Nanoindentation dataset of paper submitted to Journal of Geophysical Research: Solid Earths entitled "Comparison of biotite elastic properties recovered by spherical nanoindentations and atomistic simulations - influence of nano-scale defects in phyllosilicates" Open
Phyllosilicate minerals, due to their sheets structure and morphology, are known to cause anisotropy in bulk rock properties and make the bulk rock more compliant. Accurately characterizing the micromechanical behavior of phyllosilicate mi…
View article: IODP Expedition 358, Hole C0002Q - Well Logging Data
IODP Expedition 358, Hole C0002Q - 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 358, Hole C0002T - Well Logging Data
IODP Expedition 358, Hole C0002T - 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 358, Hole C0024A - Well Logging Data
IODP Expedition 358, Hole C0024A - 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 358, Hole C0002S - Well Logging Data
IODP Expedition 358, Hole C0002S - 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 358, Hole C0024A - Well Logging Data
IODP Expedition 358, Hole C0024A - 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 358, Hole C0002R - Well Logging Data
IODP Expedition 358, Hole C0002R - 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 358, Hole C0002R - Well Logging Data
IODP Expedition 358, Hole C0002R - 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 358, Hole C0002S - Well Logging Data
IODP Expedition 358, Hole C0002S - 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 358, Hole C0002Q - Well Logging Data
IODP Expedition 358, Hole C0002Q - 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 358, Hole C0002T - Well Logging Data
IODP Expedition 358, Hole C0002T - 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, …