Magma is transported and stored in the crust mostly through networks of planar structures
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …

Growing evidence supports the notion that plutons are constructed incrementally, commonly
over long periods of time, yet field evidence for the multiple injections that seem to be …

Episodes of spreading ridge subduction occurred during late Oligocene to early Miocene
time along western California and during late Paleocene to early Eocene time along …

We have carried a structural study across Kodiak accretionary complex in Alaska, USA, in
order to describe its thermal structure and decipher the processes of exhumation. The …

Active faults slip at different rates over the course of the seismic cycle: earthquake slip (c. 1
ms− 1), interseismic creep (c. 10–100 mm year− 1) and intermediate rate transients (eg …

Abstract The Sanak-Baranof belt includes a series of near-trench plutons that intrude the
outboard Chugach–Prince William terrane over~ 2200 km along the southern Alaskan …

Abstract The Kamchatka and Aleutian (KAT) arc-trench systems meet orthogonally at Cape
Kamchatka Peninsula. The KAT connection is the intersection of the NE-striking Kamchatka …

A variety of methods have been employed to decipher magmatic systems, including
geophysical, petrological, textural and geochemical approaches, and these elucidate a …

The Uganik Thrust is a fossil out‐of‐sequence thrust fault which was active over a period
of∼ 3 Ma during the early Tertiary until activity ceased with the subduction of the Kula …

Large granitoid batholiths contain key information about the formation and evolution of the
continental crust, but their growth mechanism and compositional diversity are still not clear …