Results 221 to 230 of about 16,196 (284)
The Mantle Fe<sup>3+</sup>/ΣFe Ratio Has Doubled Since the Early Archean. [PDF]
Zhu XX +4 more
europepmc +1 more source
Intense Ground Magnetic Perturbations During the 2024 May and October Geomagnetic Storms
Abstract The May and October 2024 geomagnetic storms represent two of the most intense space weather events of Solar Cycle 25. While differing in global intensity, both storms produced extreme ionospheric disturbances, including equatorward auroral expansion to mid‐latitudes and rapid geomagnetic variations (dH/dt $\text{dH}/\text{dt}$).
P. De Michelis +3 more
wiley +1 more source
Water Versus Land on Temperate Rocky Planets. [PDF]
Guimond CM +8 more
europepmc +1 more source
Mechanical behavior of rocks and lithosphere dynamics in convergence zones
Solenn Hertgen
openalex +1 more source
Abstract The southeastern Tibetan Plateau (SETP) plays a pivotal role in accommodating intra‐continental deformation driven by the ongoing India‐Eurasia convergence. However, its contemporary surface vertical motions and the underlying geodynamic processes remain highly debated.
Lei Liu +8 more
wiley +1 more source
Delineating the Central Anatolia Transition Zone (CATZ): Constraints from Integrated Geodetic (GNSS/InSAR) and Seismic Data. [PDF]
Kutoğlu ŞH, Akgün E, Softa M.
europepmc +1 more source
Abstract As spherical shell mantle convection models become increasingly commonplace, understanding how plates are generated has raised the issue of how to recognize whether rigid plates are present in model output. Tectonocists have long recognized that intraplate regions are not rigid without exception.
P. Javaheri, J. P. Lowman
wiley +1 more source
Rift linkage and inheritance determine collisional mountain belt evolution. [PDF]
Wolf SG, Huismans RS, Muñoz JA, May DA.
europepmc +1 more source
Modeling the Deformation Response to Mt. Etna Sliding Flank
Abstract The southeastern flank of Mt. Etna volcano slides into the Ionian Sea at rates of centimeters per year. While gravitational spreading and tectonic forces can cause volcanic flank collapse, their effects intrinsically trade off with magmatic forcing. There is still strong uncertainty regarding the processes underlying the sliding.
Michelle Bensing +3 more
wiley +1 more source

