Results 21 to 30 of about 72,159 (349)
Lithospheric folding in Iberia [PDF]
Integration of stress indicator data, gravity data, crustal kinematics data, and analysis of topography and recent vertical motions demonstrates the occurrence of consistently oriented spatial patterns of large‐scale Alpine to recent intraplate deformation in Iberia. The inferred upper crustal and lithospheric deformation patterns and the timing of the
Cloetingh, Sierd+7 more
openaire +5 more sources
Smart Speed Imaging in Digital Image Correlation: Application to Seismotectonic Scale Modeling
Analog models of earthquakes and seismic cycles are characterized by strong variations in strain rate: from slow interseismic loading to fast coseismic release of elastic energy.
Michael Rudolf+6 more
doaj +1 more source
Insolation driven variations of Mercury’s lithospheric strength [PDF]
Mercury's coupled 3:2 spin-orbit resonance in conjunction with its relatively high eccentricity of ~0.2 and near-zero obliquity results in both a latitudinal and longitudinal variation in annual average solar insolation and thus equatorial hot and cold ...
Aharonson, Oded+4 more
core +5 more sources
We used the moisture recycling framework to quantify the precipitation regulation services of ecosystems of the Tibetan Plateau (TP) for their contribution to precipitation. TP ecosystems contributed substantially to local and downwind precipitation, with a contribution declining from TP and neighboring areas to eastern China and other surrounding ...
Yan Li+10 more
wiley +1 more source
Evidence of Segmentation in the Iberia–Africa Plate Boundary: A Jurassic Heritage?
The present structure of the Iberia−Africa plate boundary between the Gorringe Bank and the Algerian Basin is characterized by a highly segmented geometry and diffused seismicity. Filtered Bouguer gravity data show conspicuous highs coinciding with
Manel Fernàndez+4 more
doaj +1 more source
The present-day tectonic setting of the Western Mediterranean region, from the Pyrénées to the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution involving the interactions between the Africa, Eurasia and Iberia plates
Jolivet Laurent+11 more
doaj +1 more source
Coupling Between Lithosphere Removal and Mantle Flow in the Central Andes
The central Andes is part of a Cordilleran orogen formed through continent‐ocean convergence. In contrast to the thickened crust, the mantle lithosphere below much of the orogen is anomalously thin.
Huilin Wang+2 more
doaj +1 more source
GEODYNAMICS OF URANIUM ORE FIELDS IN THE WESTERN PART OF THE INHUL MEGABLOK OF THE UKRAINIAN SHIELD
The Ingul megablock of the Ukrainian Shield contains a number of endogenous deposits of the sodium-uranium formation, which have been developed for more than 55-60 years.
V. Verkhovsev,+5 more
doaj +1 more source
In the last decade, the real time ground–based geomagnetic observations realized in correlation with the Vrancea seismicity in Romania, together with supplementary studies related to some earthquakes (Mw9.0 Tohoku, Japan on 11 March 2011 and Mw8.3 ...
Dragoș Armand Stănică+1 more
doaj +1 more source
Tidal controls on the lithospheric thickness and topography of Io from magmatic segregation and volcanism modelling [PDF]
Tidal heating is expected to impart significant, non-spherically-symmetric structure to Jupiter's volcanic moon Io. A signature of spatially variable tidal heating is generally sought in observations of surface heat fluxes or volcanic activity, an exploration complicated by the transient nature of volcanic events.
arxiv +1 more source