Modelo de deformación horizontal GPS de la región sur de la Península Ibérica y norte de Africa (SPIMA)

  1. Belén Rosado Moscoso
  2. Alberto Fernández-Ros
  3. Andrés Jiménez Jiménez
  4. Manuel Berrocoso Domínguez
Journal:
Boletín geológico y minero

ISSN: 0366-0176

Year of publication: 2017

Volume: 128

Issue: 1

Pages: 141-156

Type: Article

DOI: 10.21701/BOLGEOMIN.128.1.008 DIALNET GOOGLE SCHOLAR

More publications in: Boletín geológico y minero

Abstract

Global Navigation Satellite System (GNSS), and in particular Global Positioning System (GPS) technology provides a powerful tool for studying geodynamic processes. As a consequence of GPS studies, it is now possible to analyze the interaction between tectonic plates in order to evaluate and establish the characteristics of their boundaries. In this study, our main interest is to focus on the time series analysis obtained from observations of GNSS-GPS satellites. Each GPS observation session provides topocentric geodetic coordinates (east, north, elevation) of the permanent stations that constitute the geodetic network established for this purpose. This paper shows a detailed topocentric coordinate time-series study for sites belonging to what we call the SPINA network, which stands for south of the Iberian Peninsula, north of Africa region. The series under study are processed by techniques of relative positioning with respect to the IGS (International GNSS Service) reference station located in Villafranca. These times series have been analyzed using filter processes, harmonic adjustments and wavelets. A surface velocity field is derived from the time series of daily solutions for each station, whose observations span 8 years or longer. This allows us to obtain a horizontal displacement model to show the regional geodynamic main characteristics.