The crustal structure in south‐central Alaska has been influenced by terrane accretion, flat
slab subduction, and a modern strike‐slip fault system. Within the active subduction system …

We investigated the co‐evolution of melt, shape, and crystallographic preferred orientations
(MPOs, SPOs, and CPOs) in experimentally deformed partially molten rocks, from which we …

We compare viscoelastic models to obtain the seismic properties of a partially molten rock
as a function of temperature, pressure and tectonic stress. Invoking the correspondence …

Research on the SSI effect on flat sites has yielded many valuable conclusions. However,
current research on the impacts of various special local terrains on structural dynamics …

Partial melts can form as a result of crustal thickening due to orogenesis. Even small melt
fractions weaken the crust, so that partially molten volumes should accumulate significant …

Shear attenuation provides insights into the physical and chemical state of the upper mantle.
Yet, observations of attenuation are infrequent in the oceans, despite recent proliferation of …

Partial melt in the deforming mid-or lower continental crust causes a strength decrease and
drives formation of lithological heterogeneities. However, mechanisms of formation of syn …

As seismic data from the lower crust becomes more readily available, it is important to link
seismic properties to the ongoing processes within lower crustal evolution. This includes …

Seismic velocity and anisotropy are mainly controlled by the elastic components of rock
microstructure. Here we present a MATLAB program, GassDem (Gassmann Differential …

Conceptual models of magma storage and transport under calderas favor a connected
system of sills and dikes. These features are individually below the resolution of standard …