Oblique convergence along strike-slip faults can lead to both distributed and localized
deformation. How focused transpressive deformation is both localized and maintained along …

Terrane accretion introduces irregular geometry and allochthonous material to obliquely
convergent margins, which create opportunities to quantify strike‐slip displacement along …

Helium and carbon isotopic data from 12 springs along a~ 400 km segment of the Denali
fault system (Alaska, USA), inform mantle-to-surface connections of this enigmatic structure …

Abstract The Wrangell Arc in Alaska (USA) and adjacent volcanic fields in the Yukon provide
a long-term record of interrelations between flat-slab subduction of the Yakutat microplate …

Topography along strike‐slip fault restraining bends is theoretically self‐limited by erosion,
block translation and the expected abandonment of fault bends. However, Denali (6,194 m) …

Upper plates of subduction zones commonly respond to flat slab subduction by structural
reactivation, magmatic arc disruption, and foreland basin inversion. However, the role of …

Rare bedrock exposures of the eastern Denali fault zone in southwestern Yukon allow for
the measurement, sampling, and analyses of brittle regime fault slip data and deformation …

Active strike‐slip fault systems commonly display along‐strike Quaternary slip rate gradients
associated with fault bends and splay faults, which generate surface uplift by dip‐slip …

Uplift and cooling along the intersecting Totschunda and Denali strike‐slip faults of southern
Alaska can be used to investigate when these faults were active. Activity on these faults is …

IN-SIMS (in-situ secondary ionization mass spectrometry) micro-zircon geochronology
resolves the age of the Chipman and Kazan mafic dike swarms exposed along the central …