GPS is accurately recording vertical motion of Earth's surface in elastic response to seasonal changes in surface water storage in California. California's mountains subside up to 12 mm …
Abstract The Global Positioning System (GPS) measures elastic ground loading deformation in response to hydrological mass variations on or near Earth's surface. We present a time …
Abstract The Monviso ophiolite Lago Superiore Unit (LSU; Western Alps) constitutes a well- preserved, largely coherent fragment of eclogitic upper oceanic lithosphere subducted to c …
An increasing number of seismological studies report transient seismicity clusters in the mantle wedge several kilometers above the subduction interface. Their physical significance …
R Takagi, N Uchida, K Obara - Journal of Geophysical …, 2019 - Wiley Online Library
We detected 24 long‐term slow slip events (SSEs) in the western Nankai subduction zone, Japan, from 1996 to 2017 using a newly developed method: grid‐based determination of …
S Angiboust, J Kirsch, O Oncken… - Geochemistry …, 2015 - Wiley Online Library
The transition zone at the downdip end of seismic coupling along subduction interfaces is often the site of megathrust earthquake nucleation and concentrated postseismic afterslip …
Å Fagereng, A Beall - Philosophical Transactions of the …, 2021 - royalsocietypublishing.org
Fault slip speeds range from steady plate boundary creep through to earthquake slip. Geological descriptions of faults range from localized displacement on one or more discrete …
Abstract Deep Slow Slip and Tremors (SSTs) are a combination of transient clusters of tectonic tremors and slow slip associated with extremely elevated fluid pressures. SSTs are …