User profiles for "author:D Saffer"
Demian SafferInstitute of Geophysics, Jackson School of Geosciences, University of Texas at Austin Verified email at ig.utexas.edu Cited by 12144 |
Hydrogeology and mechanics of subduction zone forearcs: Fluid flow and pore pressure
At subduction zones, fluid flow, pore pressure, and tectonic processes are tightly
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …
The frictional, hydrologic, metamorphic and thermal habitat of shallow slow earthquakes
DM Saffer, LM Wallace - Nature Geoscience, 2015 - nature.com
The recognition of a previously unknown spectrum of slow earthquake phenomena has
ignited one of the most dynamic fields in modern seismology and fault mechanics. These …
ignited one of the most dynamic fields in modern seismology and fault mechanics. These …
[BOOK][B] Designing for interaction: creating innovative applications and devices
D Saffer - 2010 - books.google.com
Building products and services that people interact with is the big challenge of the 21st
century. Dan Saffer has done an amazing job synthesizing the chaos into an …
century. Dan Saffer has done an amazing job synthesizing the chaos into an …
[BOOK][B] Designing gestural interfaces: Touchscreens and interactive devices
D Saffer - 2008 - books.google.com
If you want to get ahead in this new era of interaction design, this is the reference you need.
Nintendo's Wii and Apple's iPhone and iPod Touch have made gestural interfaces popular …
Nintendo's Wii and Apple's iPhone and iPod Touch have made gestural interfaces popular …
Comparison of smectite-and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts
Along plate boundary subduction thrusts, the transformation of smectite to illite within fault
gouge at temperatures of∼ 150° C is one of the key mineralogical changes thought to …
gouge at temperatures of∼ 150° C is one of the key mineralogical changes thought to …
Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing …
JC Moore, D Saffer - Geology, 2001 - pubs.geoscienceworld.org
Off southwest Japan the seaward limit of coseismic displacement (or updip limit of the
seismogenic zone) of the 1946 Mw 8.3 thrust earthquake reaches to 4 km depth and∼ 40 …
seismogenic zone) of the 1946 Mw 8.3 thrust earthquake reaches to 4 km depth and∼ 40 …
Frictional and hydrologic properties of clay‐rich fault gouge
The slip behavior of major faults depends largely on the frictional and hydrologic properties
of fault gouge. We report on laboratory experiments designed to measure the strength …
of fault gouge. We report on laboratory experiments designed to measure the strength …
The state of stress on the fault before, during, and after a major earthquake
EE Brodsky, JJ Mori, L Anderson… - Annual Review of …, 2020 - annualreviews.org
Earthquakes occur by overcoming fault friction; therefore, quantifying fault resistance is
central to earthquake physics. Values for both static and dynamic friction are required, and …
central to earthquake physics. Values for both static and dynamic friction are required, and …
[HTML][HTML] Laboratory observations of slow earthquakes and the spectrum of tectonic fault slip modes
Slow earthquakes represent an important conundrum in earthquake physics. While regular
earthquakes are catastrophic events with rupture velocities governed by elastic wave speed …
earthquakes are catastrophic events with rupture velocities governed by elastic wave speed …
On the relation between fault strength and frictional stability
A fundamental problem in fault mechanics is whether slip instability associated with
earthquake nucleation depends on absolute fault strength. We present laboratory …
earthquake nucleation depends on absolute fault strength. We present laboratory …