Nicholas (Nick) M Beeler
Nick Beeler is a scientist in the Earthquake Science Center.
Science and Products
Filter Total Items: 58
Earthquake source properties from instrumented laboratory stick-slip Earthquake source properties from instrumented laboratory stick-slip
Stick-slip experiments were performed to determine the influence of the testing apparatus on source properties, develop methods to relate stick-slip to natural earthquakes and examine the hypothesis of McGarr [2012] that the product of stiffness, k, and slip duration, Δt, is scale-independent and the same order as for earthquakes. The experiments use the double-direct shear geometry...
Authors
Brian D. Kilgore, Arthur F. McGarr, Nicholas M. Beeler, David A. Lockner
Earthquake source properties from pseudotachylite Earthquake source properties from pseudotachylite
The motions radiated from an earthquake contain information that can be interpreted as displacements within the source and therefore related to stress drop. Except in a few notable cases, the source displacements can neither be easily related to the absolute stress level or fault strength, nor attributed to a particular physical mechanism. In contrast paleo-earthquakes recorded by...
Authors
Nicholas M. Beeler, Giulio Di Toro, Stefan Nielsen
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
Effective stress, friction and deep crustal faulting Effective stress, friction and deep crustal faulting
Studies of crustal faulting and rock friction invariably assume the effective normal stress that determines fault shear resistance during frictional sliding is the applied normal stress minus the pore pressure. Here we propose an expression for the effective stress coefficient αf at temperatures and stresses near the brittle-ductile transition (BDT) that depends on the percentage of...
Authors
N.M. Beeler, Greg Hirth, Amanda M. Thomas, Roland Burgmann
The role of fluid pressure on frictional behavior at the base of the seismogenic zone The role of fluid pressure on frictional behavior at the base of the seismogenic zone
To characterize stress and deformation style at the base of the seismogenic zone, we investigate how the mechanical properties of fluid-rock systems respond to variations in temperature and strain rate. The role of fluids on the processes responsible for the brittle-ductile transition in quartz-rich rocks has not been explored at experimental conditions where the kinetic competition...
Authors
Greg Hirth, Nicholas M. Beeler
Earthquake forewarning in the Cascadia region Earthquake forewarning in the Cascadia region
This report, prepared for the National Earthquake Prediction Evaluation Council (NEPEC), is intended as a step toward improving communications about earthquake hazards between information providers and users who coordinate emergency-response activities in the Cascadia region of the Pacific Northwest. NEPEC charged a subcommittee of scientists with writing this report about forewarnings...
Authors
Joan S. Gomberg, Brian F. Atwater, Nicholas M. Beeler, Paul Bodin, Earl Davis, Arthur D. Frankel, Gavin P. Hayes, Laura McConnell, Tim Melbourne, David H. Oppenheimer, John G. Parrish, Evelyn A. Roeloffs, Gary D. Rogers, Brian Sherrod, John Vidale, Timothy J. Walsh, Craig S. Weaver, Paul M. Whitmore
Science and Products
Filter Total Items: 58
Earthquake source properties from instrumented laboratory stick-slip Earthquake source properties from instrumented laboratory stick-slip
Stick-slip experiments were performed to determine the influence of the testing apparatus on source properties, develop methods to relate stick-slip to natural earthquakes and examine the hypothesis of McGarr [2012] that the product of stiffness, k, and slip duration, Δt, is scale-independent and the same order as for earthquakes. The experiments use the double-direct shear geometry...
Authors
Brian D. Kilgore, Arthur F. McGarr, Nicholas M. Beeler, David A. Lockner
Earthquake source properties from pseudotachylite Earthquake source properties from pseudotachylite
The motions radiated from an earthquake contain information that can be interpreted as displacements within the source and therefore related to stress drop. Except in a few notable cases, the source displacements can neither be easily related to the absolute stress level or fault strength, nor attributed to a particular physical mechanism. In contrast paleo-earthquakes recorded by...
Authors
Nicholas M. Beeler, Giulio Di Toro, Stefan Nielsen
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
Effective stress, friction and deep crustal faulting Effective stress, friction and deep crustal faulting
Studies of crustal faulting and rock friction invariably assume the effective normal stress that determines fault shear resistance during frictional sliding is the applied normal stress minus the pore pressure. Here we propose an expression for the effective stress coefficient αf at temperatures and stresses near the brittle-ductile transition (BDT) that depends on the percentage of...
Authors
N.M. Beeler, Greg Hirth, Amanda M. Thomas, Roland Burgmann
The role of fluid pressure on frictional behavior at the base of the seismogenic zone The role of fluid pressure on frictional behavior at the base of the seismogenic zone
To characterize stress and deformation style at the base of the seismogenic zone, we investigate how the mechanical properties of fluid-rock systems respond to variations in temperature and strain rate. The role of fluids on the processes responsible for the brittle-ductile transition in quartz-rich rocks has not been explored at experimental conditions where the kinetic competition...
Authors
Greg Hirth, Nicholas M. Beeler
Earthquake forewarning in the Cascadia region Earthquake forewarning in the Cascadia region
This report, prepared for the National Earthquake Prediction Evaluation Council (NEPEC), is intended as a step toward improving communications about earthquake hazards between information providers and users who coordinate emergency-response activities in the Cascadia region of the Pacific Northwest. NEPEC charged a subcommittee of scientists with writing this report about forewarnings...
Authors
Joan S. Gomberg, Brian F. Atwater, Nicholas M. Beeler, Paul Bodin, Earl Davis, Arthur D. Frankel, Gavin P. Hayes, Laura McConnell, Tim Melbourne, David H. Oppenheimer, John G. Parrish, Evelyn A. Roeloffs, Gary D. Rogers, Brian Sherrod, John Vidale, Timothy J. Walsh, Craig S. Weaver, Paul M. Whitmore