Displacement of GNSS permanent stations depending on the distance to the epicentre due to Japan’s earthquake on 11 March 2011

Garrido-Villén, Natalia; Berné-Valero, José Luis; Antón-Merino, A; Huang, Ching-Yao

doi:10.1179/1752270612y.0000000025

Cited by 2 publications

(1 citation statement)

References 21 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Therefore, after a Tsunami, it is necessary to re-establish the property lines again, using Global Positioning System (GPS) normally, as was the case in Indonesia [14]. From a geodesic point of view, it is well known that the definitive displacement of the zones near the epicentre is the results of earthquakes [15], e.g., the postseismic deformation after 2008 Wencham earthquake in China [16], or postseismic changes in Thai geodetic network owing to the Sumatra-Andaman mega-thrust earthquake in 2004 [17] and the Nias earthquake in 2005 [18].…”

Section: Introductionmentioning

confidence: 99%

Applied Engineering Using Schumann Resonance for Earthquakes Monitoring

et al. 2017

View full text Add to dashboard Cite

For populations that may be affected, the risks of earthquakes and tsunamis are a major concern worldwide. Therefore, early detection of an event of this type in good time is of the highest priority. The observatories that are capable of detecting Extremely Low Frequency (ELF) waves (<300 Hz) today represent a breakthrough in the early detection and study of such phenomena. In this work, all earthquakes with tsunami associated in history and all existing ELF wave observatories currently located worldwide are represented. It was also noticed how the southern hemisphere lacks coverage in this matter. In this work, the most suitable locations are proposed to cover these geographical areas. Also, ELF data processed obtained from the observatory of the University of Almeria in Calar Alto, Spain are shown. This is a contribution to help protect against natural disasters such as those caused by earthquakes and tsunamis.

show abstract

Section: Introductionmentioning

confidence: 99%

Applied Engineering Using Schumann Resonance for Earthquakes Monitoring

et al. 2017

View full text Add to dashboard Cite

show abstract

A non-uniform dip slip formula to calculate the coseismic deformation: Case study of Tohoku Mw9.0 Earthquake

Zhang¹,

Wang²,

Duan³

et al. 2019

Open Geosciences

View full text Add to dashboard Cite

The distribution of slip faults along the fault plane plays a special role in the kinetic pattern of tectonic deformation. To better understand the coseismic deformation and geodynamics of the earthquake, this paper applied the pile-up theory and derived an analytical formula to describe the non-uniform slip distribution along the fault width. To validate the new formula, it was tested with the coseismic displacements at the global positioning system (GPS) stations for the Tohoku earthquake in 11 March, 2011. Then, the computed horizontal and vertical displacements calculated using NDSM were compared to back-slip model (BSM) using GPS data obtained from the Jet Propulsion Laboratory (JPL). Finally, the theoretical analysis revealed that the analytical formulas derived here can be perceived as the expansion and perfection of the uniform dislocation model. Meanwhile, our results showed that the characteristics of the spatial distribution deformation from NDSM are similar to those derived by GPS measurements. Furthermore, the near-field RMS errors indicated that the horizontal displacements estimated using NDSM is 27.5%, and 35.6% for the vertical components. Our new formulas and findings could assist better portray the crustal deformation in some region and geodynamics in specific earthquake.

show abstract

Displacement of GNSS permanent stations depending on the distance to the epicentre due to Japan’s earthquake on 11 March 2011

Cited by 2 publications

References 21 publications

Applied Engineering Using Schumann Resonance for Earthquakes Monitoring

Applied Engineering Using Schumann Resonance for Earthquakes Monitoring

A non-uniform dip slip formula to calculate the coseismic deformation: Case study of Tohoku Mw9.0 Earthquake

Contact Info

Product

Resources

About