Results 41 to 50 of about 6,202 (287)
Triggering of the 2014 M(w)7.3 Papanoa earthquake by a slow slip event in Guerrero, Mexico [PDF]
Since their discovery two decades ago(1,2), slow slip events have been shown to play an important role in accommodating strain in subduction zones.
N. Cotte +22 more
core +1 more source
We use a prestack depth migration reflection image and magnetic anomaly data across the northern Hikurangi subduction zone, New Zealand, to constrain plate boundary structure and geometry of a subducting seamount in a region of shallow slow slip and ...
Daniel H. N. Barker +6 more
doaj +1 more source
We stacked daily Global Navigation Satellite System (GNSS) displacement increments in southwest Japan to detect the cumulative crustal deformation accompanying non-volcanic low-frequency tremors from April 1, 2004 to December 31, 2009, which are ...
Megumi Fujita +2 more
doaj +1 more source
Slow slip event measurements of IODP Hole 343-C0019
Slow slip event measurements of IODP Hole 343 ...
Ikari, Matt J +7 more
core +1 more source
Slow slip on the northern Hikurangi subduction interface, New Zealand
In October 2002, a surface displacement episode of 20–30 mm magnitude was observed over a ∼10 day period on two continuous Global Positioning System (GPS) instruments near Gisborne, North Island, New Zealand. We interpret this to result from slow slip on
Townend, J. +3 more
core +2 more sources
Long-term slow slip events along the Nankai trough delayed by the 2016 Kumamoto earthquake, Japan
The Global Navigation Satellite System network in Japan detected transient crustal deformation along the Nankai trough, Japan, from June 2018. Time-dependent inversion analysis shows that a long-term slow slip event in northern Hyuga-nada Sea along the ...
Shinzaburo Ozawa +3 more
doaj +1 more source
Fast and slow intraplate ruptures during the 19 October 2020 magnitude 7.6 Shumagin earthquake
Strong tsunami excitation from slow rupture of shallow subduction zone faults is recognized as a key concern for tsunami hazard assessment. Three months after the 22 July 2020 magnitude 7.8 thrust earthquake struck the plate boundary below the Shumagin ...
Yefei Bai +4 more
doaj +1 more source
Characteristics of Slow Slip Event in March 2020 Revealed From Borehole and DONET Observatories
We have detected an event of pore pressure change (hereafter, we refer it to “pore pressure event”) from borehole stations in real time in March 2020, owing to the network developed by connecting three borehole stations to the Dense Oceanfloor Network ...
Keisuke Ariyoshi +13 more
doaj +1 more source
The silent earthquake of 2002 in the Guerrero seismic gap, Mexico (Mw=7.6): Inversion of slip on the plate interface and some implications [PDF]
We invert GPS position data to map the slip on the plate interface during an aseismic, slow-slip event, which occurred in 2002 in the Guerrero seismic gap of the Mexican subduction zone, lasted for ~4 months, and was detected by 7 continuous GPS ...
S. I. Franco-Sánchez +6 more
doaj
Interseismic Coupling and Slow Slip Events on the Cascadia Megathrust [PDF]
In this study, we model geodetic strain accumulation along the Cascadia subduction zone between 2007.0 and 2017.632 using position time series from 352 continuous GPS stations. First, we use the secular linear motion to determine interseismic locking along the megathrust.
Sylvain Michel +2 more
openaire +2 more sources

