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Fault surface geometry plays a critical role in fault and earthquake mechanics. We have quantified...
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Reverse-drag folds are often used to infer subsurface fault geometry in extended terrains, yet details...
The stratal geometry of the Permian Capitan Reef Complex has been influenced by syn-sedimentary deformation...
Although the Permian Capitan depositional system is perhaps one of the best-exposed and most thoroughly...
Research in Earth and Environmental Sciences is becoming increasingly quantitative and process-based. This trend is...
Rollover or reverse-drag folds are a common element of extended terrains and have been documented...
The Arkitsa fault is a high angle normal fault within the Gulf of Evvia rift...
Stratal geometries of folded rocks can provide constraints for the prediction of fracture distribution and...
The western Grand Canyon is a natural laboratory for investigating processes of continental extension due...
We integrate high-precision aftershock locations with geodetic inverse modeling to create a more complete kinematic...
The increasing quality of geodetic data (synthetic aperture radar interferometry [INSAR] dense Global Positioning System...
The Laramie Peak shear system (LPSS) is a 10 km-thick zone of heterogeneous general shear...
Griswold Point is an east-west trending sand spit located in Old Lyme, Connecticut, USA, just...
The Modeling Structural Processes Working Group of the recent NAGT Workshop: "Teaching Structural Geology in...
Models are useful for teaching about the scientific process and the complex phenomena we investigate....
Many studies of earthquake triggering and fault interaction have relied on highly-idealized fault geometries and...
In the western Grand Canyon, the Colorado River cuts through a series of moderate offset...
Poly3D, a fast 3D boundary element numerical code and Poly3DGUI a graphical user interface, facilitate...
We present a new 3D slip-inversion method based on the analytical solution of an angular...
The May 13, 1995 Kozani-Grevena earthquake (Mw=6.5) is a natural laboratory for studying crustal normal...
Recent advances in geologic mapping, aftershock location, and reflection seismology allow geoscientists to image surface...
In this paper, we show that deformation can be dated by combining mesoscopic and microscopic...