David A Lockner
David Lockner is a geophysicist in the Earthquake Science Center.
Science and Products
Filter Total Items: 14
No Result Found
Filter Total Items: 115
Gallery of melt textures developed in Westerly Granite during high-pressure triaxial friction experiments Gallery of melt textures developed in Westerly Granite during high-pressure triaxial friction experiments
Introduction Melting occurred during stick-slip faulting of granite blocks sheared at room-dry, room-temperature conditions in a triaxial apparatus at 200–400 megapascals (MPa) confining pressure. Petrographic examinations of melt textures focused largely on the 400-MPa run products. This report presents an overview of the petrographic data collected on those samples, followed by brief...
Authors
Diane E. Moore, David A. Lockner, Brian D. Kilgore, Nicholas M. Beeler
Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study
We performed flow-through laboratory experiments on five cylindrically cored samples of ultramafic rocks, in which we generated a well-mated through-going tensile fracture, to investigate evolution of fracture permeability during serpentinization. The samples were tested in a triaxial loading machine at a confining pressure of 50 MPa, pore pressure of 20 MPa, and temperature of 260°C...
Authors
Aida Farough, Diane E. Moore, David A. Lockner, R.P. Lowell
Pseudotachylyte increases the post-slip strength of faults Pseudotachylyte increases the post-slip strength of faults
Solidified frictional melts, or pseudotachylytes, are observed in exhumed faults from across the seismogenic zone. These unique fault rocks, and many experimental studies, suggest that frictional melting can be an important process during earthquakes. However, it remains unknown how melting affects the post-slip strength of the fault and why many exhumed faults do not contain...
Authors
Brooks P. Proctor, David A. Lockner
Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD
The San Andreas Fault Observatory at Depth (SAFOD) scientific drillhole near Parkfield, California crosses the San Andreas Fault at a depth of 2.7 km. Downhole measurements and analysis of core retrieved from Phase 3 drilling reveal two narrow, actively deforming zones of smectite-clay gouge within a roughly 200 m-wide fault damage zone of sandstones, siltstones and mudstones. Here we...
Authors
Carolyn A. Morrow, David A. Lockner, Stephen H. Hickman
A robust calibration technique for acoustic emission systems based on momentum transfer from a ball drop A robust calibration technique for acoustic emission systems based on momentum transfer from a ball drop
We describe a technique to estimate the seismic moment of acoustic emissions and other extremely small seismic events. Unlike previous calibration techniques, it does not require modeling of the wave propagation, sensor response, or signal conditioning. Rather, this technique calibrates the recording system as a whole and uses a ball impact as a reference source or empirical Green’s...
Authors
Gregory C. McLaskey, David A. Lockner, Brian D. Kilgore, Nicholas M. Beeler
Preslip and cascade processes initiating laboratory stick slip Preslip and cascade processes initiating laboratory stick slip
Recent modeling studies have explored whether earthquakes begin with a large aseismic nucleation process or initiate dynamically from the rapid growth of a smaller instability in a “cascade-up” process. To explore such a case in the laboratory, we study the initiation of dynamic rupture (stick slip) of a smooth saw-cut fault in a 76mm diameter cylindrical granite laboratory sample at 40...
Authors
Gregory C. McLaskey, David A. Lockner
Science and Products
Filter Total Items: 14
No Result Found
Filter Total Items: 115
Gallery of melt textures developed in Westerly Granite during high-pressure triaxial friction experiments Gallery of melt textures developed in Westerly Granite during high-pressure triaxial friction experiments
Introduction Melting occurred during stick-slip faulting of granite blocks sheared at room-dry, room-temperature conditions in a triaxial apparatus at 200–400 megapascals (MPa) confining pressure. Petrographic examinations of melt textures focused largely on the 400-MPa run products. This report presents an overview of the petrographic data collected on those samples, followed by brief...
Authors
Diane E. Moore, David A. Lockner, Brian D. Kilgore, Nicholas M. Beeler
Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study
We performed flow-through laboratory experiments on five cylindrically cored samples of ultramafic rocks, in which we generated a well-mated through-going tensile fracture, to investigate evolution of fracture permeability during serpentinization. The samples were tested in a triaxial loading machine at a confining pressure of 50 MPa, pore pressure of 20 MPa, and temperature of 260°C...
Authors
Aida Farough, Diane E. Moore, David A. Lockner, R.P. Lowell
Pseudotachylyte increases the post-slip strength of faults Pseudotachylyte increases the post-slip strength of faults
Solidified frictional melts, or pseudotachylytes, are observed in exhumed faults from across the seismogenic zone. These unique fault rocks, and many experimental studies, suggest that frictional melting can be an important process during earthquakes. However, it remains unknown how melting affects the post-slip strength of the fault and why many exhumed faults do not contain...
Authors
Brooks P. Proctor, David A. Lockner
Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD
The San Andreas Fault Observatory at Depth (SAFOD) scientific drillhole near Parkfield, California crosses the San Andreas Fault at a depth of 2.7 km. Downhole measurements and analysis of core retrieved from Phase 3 drilling reveal two narrow, actively deforming zones of smectite-clay gouge within a roughly 200 m-wide fault damage zone of sandstones, siltstones and mudstones. Here we...
Authors
Carolyn A. Morrow, David A. Lockner, Stephen H. Hickman
A robust calibration technique for acoustic emission systems based on momentum transfer from a ball drop A robust calibration technique for acoustic emission systems based on momentum transfer from a ball drop
We describe a technique to estimate the seismic moment of acoustic emissions and other extremely small seismic events. Unlike previous calibration techniques, it does not require modeling of the wave propagation, sensor response, or signal conditioning. Rather, this technique calibrates the recording system as a whole and uses a ball impact as a reference source or empirical Green’s...
Authors
Gregory C. McLaskey, David A. Lockner, Brian D. Kilgore, Nicholas M. Beeler
Preslip and cascade processes initiating laboratory stick slip Preslip and cascade processes initiating laboratory stick slip
Recent modeling studies have explored whether earthquakes begin with a large aseismic nucleation process or initiate dynamically from the rapid growth of a smaller instability in a “cascade-up” process. To explore such a case in the laboratory, we study the initiation of dynamic rupture (stick slip) of a smooth saw-cut fault in a 76mm diameter cylindrical granite laboratory sample at 40...
Authors
Gregory C. McLaskey, David A. Lockner