Results 221 to 230 of about 181,228 (320)
Earthquake frequency-magnitude distribution at Mount Etna sheds light on magma ascent in the volcano's plumbing system. [PDF]
Firetto Carlino M +7 more
europepmc +1 more source
The Effects of Deformation on the Early Crystallization Kinetics of Basaltic Magmas
Barbara Tripoli +3 more
openalex +1 more source
Magnetic Evolution of Super‐Earth Exoplanets With a Basal Magma Ocean
Abstract Habitability of super‐Earths likely requires self‐sustained magnetic fields to shield their atmospheres from stellar forcing. Extreme pressures and temperatures probably produce a long‐lived basal magma ocean (BMO), a potential source for these fields.
Victor Lherm +2 more
wiley +1 more source
A computed tomography observation of the Unzen lava reveals the frequent existence of vesicles and crystals in proximity. [PDF]
Saito K, Hoshino M, Goto A, Namiki A.
europepmc +1 more source
Abstract The study of terrestrial lava tubes is essential for understanding geological processes occurring during volcanic activity on other planetary bodies, such as Mars. These processes lead to the formation of minerals analogous to those found on other planets.
F. Alberquilla +10 more
wiley +1 more source
Abstract In the Afghan Hindu Kush, the 223–209 Ma (≤800°C) Salang batholith is part of the Silk‐Road magmatic arc that was built on ∼40‐km‐thick Turan‐Karakum block continental crust. The batholith constitutes the hanging wall of the Herat‐Panjshir‐Badakhshan—the Paleo‐Tethys—suture zone, vestige of the subducted Paleozoic‐early Mesozoic Paleo‐Tethys ...
Lothar Ratschbacher +8 more
wiley +1 more source
A cross-tissue transcriptome-wide association study identifies novel candidate genes associated with brain glymphatic system function. [PDF]
Zhu X +6 more
europepmc +1 more source
Fluid flux melting generated postcollisional high Sr/Y copper ore–forming water-rich magmas in Tibet
Yongjun Lu +4 more
openalex +2 more sources
Electrical and thermal conductivity of Earth's iron-enriched basal magma ocean. [PDF]
Dragulet F, Stixrude L.
europepmc +1 more source
Detrital zircon unmixing identifies three sediment sources for the Oligocene–Miocene Nyalau Formation, including a previously unrecognised syn‐depositional component characterised by Oligocene–Miocene volcanic zircons and Neoproterozoic populations absent from established sources.
Ekundayo J. Adepehin +3 more
wiley +1 more source

