Apatite fission track thermochronology (AFTT) on granitic samples collected in the central
Alaska Range in conjunction with geologic constraints from basins to the north (Nenana …

In the tectonically active Circum-Pacific Belt, thick transgressive sequences are not
uncommon, in contrast with their rarity in the Cretaceous of the Western Interior. Thick …

Arc-trench systems of the circum-Pacific orogenic belt contain voluminous sandstones within
fore-arc terranes that include complexly deformed subduction complexes and relatively …

Southcentral Alaska is a complex tectonic region that transitions from subduction of Pacific
crust to flat slab subduction—and collision—of overthickened Yakutat crust. Because much …

Local geologic relationships in the western Chugach Mountains, together with regional
considerations, suggest that in the Early Cretaceous a subduction zone was formed along …

The Border Ranges fault system (BRFS) locally separates supracrustal Upper Cretaceous‐
Tertiary rocks of the Cook Inlet/Matanuska Valley forearc basin on the Peninsular terrane …

Topographic development inboard of the continental margin is a predicted response to ridge
subduction. New thermochronology results from the western Alaska Range document ridge …

Forearc systems evolve through the interplay of numerous processes, but aside from lateral
movements much of the observed variability in morphology can be related to evolution of …

I present the results of an extensive data mining effort integrating 197 permanent and
temporary seismic stations into a Rayleigh wave ambient noise study across southern …

Subduction zones are common tectonic features central to large-scale crustal and elemental
cycling, and they are accompanied by basins often with thick sedimentary fill and structures …