Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Nicholas M. Beeler"'
Autor:
Andrew J Barbour, Nicholas M Beeler
Publikováno v:
Earth and Planetary Physics, Vol 5, Iss 6, Pp 547-558 (2021)
Connecting earthquake nucleation in basement rock to fluid injection in basal, sedimentary reservoirs, depends heavily on choices related to the poroelastic properties of the fluid-rock system, thermo-chemical effects notwithstanding. Direct constrai
Externí odkaz:
https://doaj.org/article/d460291d3aa14fb6a2f8373a99dcf16e
Autor:
Nicholas M. Beeler
Publikováno v:
Open-File Report.
Publikováno v:
Journal of Geophysical Research: Solid Earth. 123:457-475
The central section of the San Andreas Fault hosts tectonic tremor and low-frequency earthquakes (LFEs) similar to subduction zone environments. LFEs are often interpreted as persistent regions that repeatedly fail during the aseismic shear of the su
Publikováno v:
Journal of Geophysical Research: Solid Earth. 122:7042-7075
This study is to determine the detailed response of shear strength and other fault properties to changes in normal stress at room temperature using dry initial bare rock surfaces of granite at normal stresses between 5 and 7 MPa. Rapid normal stress
Publikováno v:
Journal of Geophysical Research: Solid Earth. 122:6389-6430
The popular constitutive formulations of rate-and-state friction offer two end member views on whether friction evolves only with slip (Slip law) or with time even without slip (Aging law). While rate stepping experiments show support for the Slip la
Publikováno v:
Bulletin of the Seismological Society of America, 2016, Vol.106(6), pp.2764-2776 [Peer Reviewed Journal]
Di Toro, G, Beeler, N M & Nielsen, S 2016, ' Earthquake source properties from pseudotachylite ', Bulletin of the Seismological Society of America . https://doi.org/10.1785/0120150344
Di Toro, G, Beeler, N M & Nielsen, S 2016, ' Earthquake source properties from pseudotachylite ', Bulletin of the Seismological Society of America . https://doi.org/10.1785/0120150344
Earthquake‐radiated motions contain information that can be interpreted as source displacement and therefore related to stress drop. Except in a few notable cases, these displacements cannot be easily related to the absolute stress level or the fau
Publikováno v:
Geophysical Research Letters. 42:7039-7045
We describe observations of dynamic rupture events that spontaneously arise on meter-scale laboratory earthquake experiments. While low-frequency slip of the granite sample occurs in a relatively uniform and crack-like manner, instruments capable of
Autor:
Nicholas M. Beeler, Stephen H. Hickman
Publikováno v:
Journal of Geophysical Research: Solid Earth. 120:3599-3616
Earthquake recurrence requires interseismic fault restrengthening which results from solid-state deformation in room temperature friction and indentation experiments. In contrast, exhumed fault zones show solution-transport processes such as pressure
Autor:
Greg Hirth, Nicholas M. Beeler
Publikováno v:
Geology. 43:223-226
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
Publikováno v:
Journal of Geophysical Research: Solid Earth. 119:8770-8791
In this study, rock friction “stick-slip” experiments are used to develop constraints on models of earthquake recurrence. Constant rate loading of bare rock surfaces in high-quality experiments produces stick-slip recurrence that is periodic at l