The following pages link to David A Lockner (Q54089):
Displayed 50 items.
- Physical properties of sidewall cores from Decatur, Illinois (Q57935) (← links)
- Dependence of frictional strength on compositional variations of Hayward fault rock gouges (Q63695) (← links)
- Physical properties of two core samples from Well 34-9RD2 at the Coso geothermal field, California (Q67896) (← links)
- High-pressure rock-physics laboratories investigate earthquake processes (Q70203) (← links)
- Hayward Fault rocks: porosity, density, and strength measurements (Q73172) (← links)
- How brucite may affect the frictional properties of serpentinite (Q73239) (← links)
- Proceedings of the International workshop on the Nojima Fault core and borehole data analysis (Q74554) (← links)
- Sample characterizations and strength measurements of serpentinite gouges (Q80118) (← links)
- High-temperature permeability studies; 1, Permeability of granite and novaculite at 300 degrees to 500 degrees C (Q82285) (← links)
- Laboratory measurements of velocity-dependent frictional strength (Q95467) (← links)
- A laboratory control system using the PDP 1103 microprocessor (Q110276) (← links)
- Premonitory slip and tidal triggering of earthquakes (Q144859) (← links)
- Conversion of wet glass to melt at lower seismogenic zone conditions: Implications for pseudotachylyte creep (Q145662) (← links)
- Evolution of fluid transmissivity and strength recovery of shear fractures under hydrothermal conditions (Q146368) (← links)
- Rapid acceleration leads to rapid weakening in earthquake-like laboratory experiments (Q147416) (← links)
- Fault weakening and earthquake instability by powder lubrication (Q148741) (← links)
- Constraints on the stress state of the San Andreas fault with analysis based on core and cuttings from SAFOD drilling phases 1 and 2 (Q149077) (← links)
- Data Report: Permeability, porosity, and frictional strength of core samples from IODP Expedition 366 in the Mariana forearc (Q149606) (← links)
- Observations of quasistatic fault growth from acoustic emissions (Q151811) (← links)
- An earthquake mechanism based on rapid sealing of faults (Q151903) (← links)
- Fault growth and acoustic emissions in confined granite (Q152014) (← links)
- Fracture in Westerly granite under AE feedback and constant strain rate loading: Nucleation, quasi-static propagation, and the transition to unstable fracture propagation (Q152178) (← links)
- An earthquake instability model based on faults containing high fluid-pressure compartments (Q152447) (← links)
- Pseudotachylyte increases the post-slip strength of faults (Q152720) (← links)
- Calibrated acoustic emission system records M -3.5 to M -8 events generated on a saw-cut granite sample (Q153146) (← links)
- Hydrothermal frictional strengths of rock and mineral samples relevant to the creeping section of the San Andreas Fault (Q153281) (← links)
- Anisotropic changes in P-wave velocity and attenuation during deformation and fluid infiltration of granite (Q154152) (← links)
- Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence (Q154277) (← links)
- Frictional properties of exhumed fault gouges in DFDP-1 cores, Alpine Fault, New Zealand (Q155069) (← links)
- COMPLEX RESISTIVITY OF FAULT GOUGE AND ITS SIGNIFICANCE FOR EARTHQUAKE LIGHTS AND INDUCED POLARIZATION. (Q155221) (← links)
- Preslip and cascade processes initiating laboratory stick slip (Q155811) (← links)
- Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study (Q155869) (← links)
- Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD (Q155912) (← links)
- Frictional strength of wet and dry montmorillonite (Q156062) (← links)
- Earthquake source properties from instrumented laboratory stick-slip (Q156321) (← links)
- A robust calibration technique for acoustic emission systems based on momentum transfer from a ball drop (Q234368) (← links)
- Evolution of wear and friction along experimental faults (Q236202) (← links)
- Deep permeability of the San Andreas Fault from San Andreas Fault Observatory at Depth (SAFOD) core samples (Q236569) (← links)
- Laboratory generated M -6 earthquakes (Q237221) (← links)
- Buried shallow fault slip from the South Napa earthquake revealed by near-field geodesy (Q239630) (← links)
- Comparative deformation behavior of minerals in serpentinized ultramafic rock: Application to the slab-mantle interface in subduction zones (Q242462) (← links)
- San Andreas Fault Zone mineralogy, geochemistry, and physical properties from SAFOD cuttings and core (Q242466) (← links)
- Chemical controls on fault behavior: weakening of serpentinite sheared against quartz-bearing rocks and its significance for fault creep in the San Andreas system (Q243290) (← links)
- Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties (Q247508) (← links)
- Oscillating load-induced acoustic emission in laboratory experiment (Q247878) (← links)
- The coefficient of friction of chrysotile gouge at seismogenic depths (Q249079) (← links)
- Earthquake rupture at focal depth, part II: mechanics of the 2004 M2.2 earthquake along the Pretorius Fault, TauTona Mine, South Africa (Q251227) (← links)
- The role of adsorbed water on the friction of a layer of submicron particles (Q251271) (← links)
- Low strength of deep San Andreas fault gouge from SAFOD core (Q251870) (← links)
- Talc friction in the temperature range 25°–400 °C: relevance for fault-zone weakening (Q252737) (← links)