Results 261 to 270 of about 248,223 (333)
Crustal structure of La Palma Island inferred from 3D aeromagnetic modelling. [PDF]
Romero-Toribio MC +2 more
europepmc +1 more source
Abstract Salt's inherent weakness and capacity for ductile deformation create significant mechanical contrasts that locally perturb the stress field in surrounding rocks, often leading to deviations from regional tectonic stresses. Variations in local stress are a critical factor for wellbore stability, seal integrity, and fluid flow in subsurface ...
Lauren J. Reeher +3 more
wiley +1 more source
Temporary Seismic Array Installation in the Contursi Terme Hydrothermal System: A Step Toward Geothermal Assessment. [PDF]
Serlenga V +13 more
europepmc +1 more source
Effects of Improved Tidal Mixing in NEMO One‐Degree Global Ocean Model
Abstract Diapycnal mixing in the ocean interior has diverse numerical representations in current global ocean models. These representations affect the simulated transport and storage of oceanic tracers in ways that remain little studied. Here we present the impacts of three different tidal mixing representations in thousand‐year‐long simulations with ...
Casimir de Lavergne +7 more
wiley +1 more source
Development of a Transient Wellbore Heat Transfer Model Validated with Distributed Temperature Sensing Data. [PDF]
Nakamoto R, Leggett S.
europepmc +1 more source
Fission Track Age of Volcanoes in the Kuju Volcanic Region in Relation to Geothermal Activity
Koichiro Watanabe +2 more
openalex +2 more sources
Impact‐Generated Mixing, Melting and Vaporization of the Early Earth's Crust
Abstract Earth's primary accretion was followed by a protracted flux of interplanetary collisions by leftover planetesimals. The effects of the largest collisions—with bodies possibly exceeding 1,000 km diameter—would have been devastating for terrestrial near‐surface environments.
S. Marchi +3 more
wiley +1 more source
Impact Reactivation of a Hydrothermal System in Basalt in the Vargeão Dome Impact Structure, Brazil
Abstract As hydrous minerals have been observed in impact craters on Mars, impact‐generated hydrothermal systems (IGHSs) have been considered as potential habitats for life on that planet. The Vargeão Dome, a 12 km wide impact structure in southern Brazil, was formed in basalts with at least two hydrothermal alteration stages.
Jitse Alsemgeest +5 more
wiley +1 more source

