The general lack of a correlation between earthquakes and surface faulting in the interior of
the western US cordillera has motivated our efforts to evaluate the geometry, structural style …

We present a methodology for conducting a site-specific probabilistic analysis of fault
displacement hazard. Two approaches are outlined. The first relates the occurrence of fault …

Large normal fault zones are characterized by intense fracturing and hydrothermal
alteration. Displacement is localized in a slip zone of cataclasite, breccia and phyllonite …

A broad zone of dominantly subaerial silicic volcanism associated with regional extensional
faulting developed in southern South America during the Middle Jurassic …

Abstract The Saint Elias orogen of southern Alaska and adjacent Canada is a complex belt
of mountains formed by collision and accretion of the Yakutat terrane into the transition zone …

Outcrop mapping and fault-rock characterization of the Stillwater normal fault zone in Dixie
Valley, Nevada are used to document and interpret ancient hydrothermal fluid flow and its …

Oblique convergence in the St. Elias orogen of southern Alaska and northwestern Canada
has constructed the world's highest coastal mountain range and is the principal driver …

We consider the problem of defining the fracture permeability tensor for each grid block in a
rock mass from maps of natural fractures. For this purpose we implement a statistical model …

The Stillwater seismogenic normal fault in Dixie Valley, Nevada has been historically active
and is located in an area of high heat flow and hydrothermal activity. Three primary structural …

Abstract Rocks on South Georgia Island at the eastern end of the North Scotia Ridge are no
older than late Mesozoic. The Cumberland Bay and Sandebugten graywacke and mudstone …