Results 151 to 160 of about 497,770 (261)
Abstract Crustal thickness (or Moho depth) is a key parameter for many geological and geophysical models. Despite this we have a limited number of measurements, typically from seismic receiver functions, to constrain variations in crustal thickness.
Alice Blackwell +3 more
wiley +1 more source
Testing the geologically testable hypothesis on subduction initiation [PDF]
openaire +2 more sources
Abstract We propose a method to infer detailed spatiotemporal variations in interplate coupling by integrating geodetic and seismic data. It examines whether focal mechanisms of intraplate earthquakes occurring near the plate interface align with the stressing rates caused by a geodetically derived slip‐deficit rate model, evaluating deviations from a ...
Kazutoshi Imanishi, Akemi Noda
wiley +1 more source
Abstract Chlorite is thought to be one of the major water‐carrying phases in subduction zones, both within the slab and in the mantle wedge. Its presence has previously been linked to common seismological observations at subduction zones, including P and S wave anisotropy as well as high VP/VS ratios (>1.8) in the mantle wedge.
Nicholas Backhouse +8 more
wiley +1 more source
Modulation of intra-oceanic trench bending and along-trench thermochemical transport by mantle toroidal flow. [PDF]
Liu L +7 more
europepmc +1 more source
Imaging the Alpine Collision With Seismic Radial Anisotropy
Abstract The Alpine region and the adjacent Northern Apennines (NA) and Northern Dinarides record the complex tectonic evolution associated with the collision between the Eurasian and Adriatic plates. We combine Rayleigh and Love surface waves from ambient noise and earthquake data recorded at over 3,300 seismic stations to construct a high‐resolution ...
Henrique Berger Roisenberg +6 more
wiley +1 more source
Contrasting slab decarbonation patterns control deep carbon cycling efficiency in hot vs. cold subduction zones. [PDF]
Zhang H +9 more
europepmc +1 more source
Inception and Plate Evolution of the Lau Back‐Arc Basin From Plate Boundary Refinements
Abstract Back‐arc basins are important settings for crustal growth that form in response to both near and far‐field tectonic influences. To better understand the processes that control back‐arc basin initiation and evolution, we present a refined model of the kinematics of opening of the Lau Basin, embedded in a global plate model.
Alan T. Baxter +5 more
wiley +1 more source
Late Cretaceous to recent tectonic evolution of the Ulukisla Basin (Southern Central Anatolia) [PDF]
Gürer, Derya +9 more
core +1 more source
Abstract The anatomy of orogens is difficult to decipher as structural information is usually limited to surface and seismic data. Seismic properties are directionally dependent on anisotropic minerals, especially phyllosilicates. Due to tectonic complexity, the effect of anisotropy in seismic data is difficult to determine.
D. Lang +4 more
wiley +1 more source

