GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Publisher
Language
Years
  • 1
    Publication Date: 2023-10-26
    Description: In this paper, we study the spatial distribution and temporal evolution of the postseismic deformation of the 2010–2011 Rigan earthquake sequence which occurred at the southern termination of the East Lut fault system, southeast Iran. One-year GPS measurements after the Rigan earthquake sequence reveals right-lateral postseismic displacement along the East Chahqanbar fault and left-lateral postseismic displacement along the South Chahqanbar fault. To investigate the deformation variations in time and space, InSAR time-series of COSMO-SkyMed images is applied using the Small Baseline Subset algorithm. The results confirm a clear cumulative postseismic signal increasing to 8 mm during the first five months following the first mainshock in the direction of the coseismic displacement. The cumulative postseismic displacements are well correlated with the cumulative number of the aftershocks and their associated moment release. Considering this correlation and the observation of a sharp discontinuity along the coseismic fault in the displacement map, it is concluded that the after-slip mechanism is responsible for the observed postseismic deformation in the study region. This study is the first observation of a short-term postseismic motion in eastern Iran through geodetic data in contrast with long-lasting postseismic displacements following the earthquakes that occurred around Lut block. Modeling of the postseismic displacement results in a distributed slip pattern with a maximum slip of 0.8 m on the fault plane responsible for the 2010 Rigan coseismic deformation. This indicates that the postseismic deformation on barriers remained unbroken during the mainshock.
    Description: Published
    Description: 228630
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Rigan earthquake ; Postseismic deformation ; InSAR ; Lut block Southeastern Iran
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-06-19
    Description: The masses in the Earth’s atmosphere and surface cause the crust to deform. Part of these mass movements are periodic, e.g. tides in the oceans and in the atmosphere, but there are also non-periodic movements. Periodic (tidal) phenomena are quite well understood and modelled, whereas the non-periodic (non-tidal) phenomena are harder to model due to non-repeating patterns in the mass changes. Understanding the tidal and non-tidal loading improves the quality of the geodetic time series and thus, improves the stability of the reference frames. The tidal corrections to geodetic time series are done routinely, following recommendations and guidelines of the IERS Conventions. We investigated the 3D deformations in Fennoscandia induced by non-tidal atmospheric loading (NTAL) through GNSS time series modeling using GAMIT/GLOBK software. We have used 5 months of data from continuous GNSS stations belonging to FinnRef (Finnish Permanent GNSS Network) and EPN (EUREF Permanent GNSS Network) from year 2015. Two coordinate time series solutions were generated: first (reference) solution was estimated without applying loading model, while for the second solution a gridded loading model was used. We also downloaded loading correction time series from an openly available server and created the third time series by subtracting the loading correction from the reference time series. We compared the variance of three time series to see which method produces the most stable time series. The effect of NTAL correction is quite small, but not insignificant and the implementation trough the software is the most straightforward way of doing it.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-08-09
    Description: The Earth’s surface is continuously deforming at various temporal and spatial scales. The deformation is caused by the changing mass distribution of atmospheric, oceanic, hydrological masses, glaciers and ice sheets as well as earthquakes and/or human activities. Some of the mass changes are periodic and rather well known (e.g., ocean and solid Earth tides), whereas the non-periodic mass changes are not that well known or easy to model. The latter part is often referred to as non-tidal loading (NTL) and is the focus of the study. A deeper understanding of the NTL in geodetic time series, particularly in regional and/or local scales, will result in insights in modelling and removing the effect from the time series, thus improving the stability of the geodetic time series. Examining the impacts of different loading products in our region is critical for accurately removing the loading signal. Currently, there are several open sources for loading products. In this study, we compared the performance of these loading products and investigated their impact on the scatter of GNSS time series in the permanent GNSS stations in Finland (FinnRef). We studied five different hydrological loading models, six different non-tidal atmospheric loading models, and three different non-tidal oceanic loading models to see how various loading configurations operate and how they affect the noise characteristics of GNSS 3D time series, and ultimately figure out which models is most realistic in Finland.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...