Results 231 to 240 of about 24,812 (309)

Seismic Imaging of the Reykjanes Peninsula, Iceland: Crustal‐Scale Context of Geothermal Areas and Ongoing Volcano‐Tectonic Unrest

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 4, April 2025.
Abstract Volcanic and seismic unrest on the Reykjanes Peninsula in SW Iceland that started in late 2019 after ∼800 years of quiescence has drawn wide interest to this on‐land extension of the Mid‐Atlantic spreading ridge. Here, we use seismic data collected across the larger Peninsula region, covering six volcanic systems and associated high ...
J. Jenkins   +13 more
wiley   +1 more source

Local patterns of genetic sharing between neuropsychiatric and insulin resistance-related conditions. [PDF]

open access: yesTransl Psychiatry
Fanelli G   +27 more
europepmc   +1 more source

Seismic Stratigraphy of Valdivia Bank, South Atlantic and Implications for Oceanic Plateau Evolution, Sedimentation, and Thermal Rejuvenation

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 4, April 2025.
Abstract Valdivia Bank (VB) is an oceanic plateau in the South Atlantic that formed from hotspot‐ridge volcanism during the Late Cretaceous at the Mid‐Atlantic Ridge (MAR). It is part of Walvis Ridge (WR), a quasi‐linear seamount chain extending from offshore Namibia to Tristan da Cunha and Gough Islands.
E. Contreras   +5 more
wiley   +1 more source

Quantification of low-temperature gas emissions reveals CO<sub>2</sub> flux underestimates at Soufrière Hills volcano, Montserrat. [PDF]

open access: yesSci Adv
Riddell A   +9 more
europepmc   +1 more source

Quantitative Microstructural Analysis of Exhumed Epidote‐Amphibolites and Plate Interface Rheology in Warm Subduction Zones

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 4, April 2025.
Abstract Epidote‐amphibolites form along the plate interface during subduction infancy and are stable in warm, mature subduction zones that generate slow earthquakes. Epidote‐amphibolite rheology therefore likely influences plate‐scale processes during plate boundary formation and grain‐scale processes that give rise to slip transients.
Laurens H. Kleijbeuker   +3 more
wiley   +1 more source

Home - About - Disclaimer - Privacy