Results 171 to 180 of about 29,724 (300)

Time Evolution of Dehydration‐Induced Stick‐Slip Behaviors of Simulated Bassanite Gouges

open access: yesGeophysical Research Letters, Volume 52, Issue 9, 16 May 2025.
Abstract Pore pressure by dehydrating hydrous minerals can trigger deep and intermediate‐depth earthquakes. We performed friction experiments on simulated bassanite gouges under various confining pressures and temperatures. At room temperature (RT), stress drops and recurrence intervals of stick‐slip events varied with confining pressures.
M. Kawabata   +5 more
wiley   +1 more source

Heavy boron isotopes in intraplate basalts reveal recycled carbonate in the mantle. [PDF]

open access: yesSci Adv
Xu R   +11 more
europepmc   +1 more source

Geochemical and Isotopic Evidence for Fluid Flow in the Western Nankai Subduction Zone, Japan

open access: bronze, 1993
Miriam Kastner   +4 more
openalex   +1 more source

Unlocking the Style and Timing of Submarine Landslides: Insights From the Tuaheni North Slide, Hikurangi Margin

open access: yesGeophysical Research Letters, Volume 52, Issue 9, 16 May 2025.
Abstract We investigate the morphology and timing of Tuaheni North, a large submarine landslide within the Tuaheni Landslide Complex on Aotearoa New Zealand's Hikurangi Margin. We show a clear correlation between two major source volumes from Tuaheni North and two downslope mass transport deposits (MTDs), suggesting there were two distinct events ...
Alexey Portnov   +5 more
wiley   +1 more source

Advancements in the GRACE and GRACE‐FO Gradiometer Mode

open access: yesEarth and Space Science, Volume 12, Issue 5, May 2025.
Abstract The global gravitational gradient field has not been observed since the decommission of GOCE in 2013. Based on the foundational work of Peidou and Pagiatakis (2019, https://doi.org/10.1029/2018jb016382), we advance the concept of GRACE gradiometer mode (GM) for the purpose of using GRACE, GRACE‐FO and future gravity space missions as ...
Nikeet Pandit, Spiros Pagiatakis
wiley   +1 more source

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