Results 111 to 120 of about 2,926 (202)
Coseismic Deformation Field and Fault Slip Distribution Inversion of the 2020 Jiashi Ms 6.4 Earthquake: Considering the Atmospheric Effect with Sentinel-1 Data Interferometry. [PDF]
Zhang X, Li J, Liu X, Li Z, Adil N.
europepmc +1 more source
25‐Second Determination of 2019 Mw 7.1 Ridgecrest Earthquake Coseismic Deformation
We have developed a global earthquake monitoring system based on low‐latency measurements from more than 1000 existing Global Navigational Satellite System (GNSS) receivers, of which nine captured the 2019 Mw 6.4 Ridgecrest, California, foreshock and Mw ...
Santillan, Marcelo +3 more
core +1 more source
Intertidal foraminifera of the Avon-Heathcote Estuary; response to coseismic deformation and potential to record local historic events [PDF]
The Avon-Heathcote Estuary, located in Christchurch, New Zealand, experienced coseismic deformation as a result of the February 22nd 2011 Christchurch Earthquake.
Vettoretti, Gina Josephine
core +1 more source
We used continuous Global Positioning System (GPS) measurements to infer the fault geometry and the amount of coseismic slip associated to the August 24, 2016 Mw 6 Amatrice earthquake.
Daniele Cheloni +28 more
doaj +1 more source
Alternating seismic uplift and subsidence in the late Holocene at Madang, Papua New Guinea: Evidence from raised reefs [PDF]
Well-preserved mid-late Holocene coral reefs are exposed in low coastal cliffs in the vicinity of the Madang lagoon on the north coast of Papua New Guinea.
Tudhope, Alexander +18 more
core +1 more source
Coseismic and postseismic crustal deformations caused by earthquake episodes are important in understanding the mechanisms of these episodes as well as the fault rheology near an epicentral area.
Furuya, Masato +3 more
core +1 more source
Water vaporization promotes coseismic fluid pressurization and buffers temperature rise [PDF]
We investigated the frictional properties of carbonate-rich gouge layers at a slip rate of 1.3 m/s, under dry and water-saturated conditions, while monitoring temperature at different locations on one of the gouge-host rock interfaces.
Lu Yao +8 more
core +1 more source
The Mw 7.0 Dingri earthquake, the largest documented normal-faulting event in southern Tibet, struck within the NS-trending Dinggye-Xainza Rift system. Here we combine field observations, high resolution optical and synthetic aperture radar imagery and ...
Wenbin Xu +8 more
doaj +1 more source
Shallow geological structures triggered during the Mw 6.4 Meinong earthquake, southwestern Taiwan
The Meinong earthquake generated up to ~10 cm surface displacement located 10 - 35 km west of the epicenter and monitored by InSAR and GPS. In addition to coseismic deformation related to the deep earthquake source, InSAR revealed three sharp surface ...
Maryline Le Béon +10 more
doaj +1 more source
Three-dimensional coseismic surface deformation fields are important for quantifying the geometric and kinematic characteristics of earthquake rupture faults.
Nana Han +5 more
doaj +1 more source

