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Red GPS Topo-Iberia: Resultados obtenidos en el Centro de Analisis de la UJA
Author(s)
De Lacy Perez de los Cobos, M. C.
Universidad de Jaen
Armenteros, J. A.
Universidad de Jaen
Ruiz Armenteros, A. M.
Universidad de Jaen
Gil Cruz, A. J.
Universidad de Jaen
Language
English
Obiettivo Specifico
1IT. Reti di monitoraggio e Osservazioni
Status
Published
JCR Journal
N/A or not JCR
Peer review journal
Yes
Title of the book
Issue/vol(year)
/76 (2014)
ISSN
0214-4557
Publisher
Servicio de Publicaciones, Universidad Complutense de Madrid
Pages (printed)
25-33
Issued date
2014
Alternative Location
Abstract
The project ”Geosciences in Iberia: Integrated stud
ies of topography and 4-D evolution Topo-Iberia”
(Ref.CSD2006-00041) is supported by the Spanish Min
istry for the Economy and Competitiveness. Its
objective is to understand the interactions in the
Iberian Peninsula (SW Europe) between deep, shallow
and atmospheric processes, through a multidisciplin
ary approach linking Geology, geophysics and
Geodesy. As part of this project a network of 26 CG
PS (continuous GPS) stations, covering the
Spanish part of the Iberian Peninsula (22 stations)
and Morocco (4 stations) was established in 2008 t
o
complement other GPS networks already deployed by d
ifferent Institutions, EPN (EUREF Permanent
Network), IGS (InternationalGNSS Service) and regio
nal governmental agencies to monitor crustal deformation due to Nubia and Eurasian tectonic plat
es. Data analysis is performed at three different
analysis centres: Real Instituto y Observatorio de
la Armada (ROA), University of Barcelona (UB) and
University of Jaen (UJA). The coordinate time serie
s and the velocity field from 2008-2013 computed
at UJA analysis centre are presented in this paper.
The estimated velocities show the southeast of the
Iberian Peninsula is a boundary area between two pl
ates accommodating the relative movements
between the Eurasian and Nubia plates.
ies of topography and 4-D evolution Topo-Iberia”
(Ref.CSD2006-00041) is supported by the Spanish Min
istry for the Economy and Competitiveness. Its
objective is to understand the interactions in the
Iberian Peninsula (SW Europe) between deep, shallow
and atmospheric processes, through a multidisciplin
ary approach linking Geology, geophysics and
Geodesy. As part of this project a network of 26 CG
PS (continuous GPS) stations, covering the
Spanish part of the Iberian Peninsula (22 stations)
and Morocco (4 stations) was established in 2008 t
o
complement other GPS networks already deployed by d
ifferent Institutions, EPN (EUREF Permanent
Network), IGS (InternationalGNSS Service) and regio
nal governmental agencies to monitor crustal deformation due to Nubia and Eurasian tectonic plat
es. Data analysis is performed at three different
analysis centres: Real Instituto y Observatorio de
la Armada (ROA), University of Barcelona (UB) and
University of Jaen (UJA). The coordinate time serie
s and the velocity field from 2008-2013 computed
at UJA analysis centre are presented in this paper.
The estimated velocities show the southeast of the
Iberian Peninsula is a boundary area between two pl
ates accommodating the relative movements
between the Eurasian and Nubia plates.
References
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frame.
J Geod
85:457–473
AVALLONE A, SELVAGGI G, D’ANASTASIO E et al (2010).
The RING
network: improvement of a GPS velocity field in the
central Mediterranean.
Ann
Geophys
53:39–54.
BIANCO, G., DEVOTI, R., LUCERI, V. (2003). Combinat
ion of loosely
constrained solutions.
IERS Tech. Note
30, 107–109.
DACH, R., U. HUGENTOBLER, P. FRIDEZ, AND M. MEINDL,
Eds. (2007).
Bernese GPS Software, Version 5.0, User Manual, Ast
ronomical Institute,
University of Bern. Bern. Switzerland.
DEVOTI, R., RIGUZZI, F., CUFFARO, M., DOGLIONI, C.
(2008). New GPS
constraints on the kinematics of the Apennine subdu
ction.
Earth and Planetary
Science Letters,
273 (1–2), 163–174.
DEVOTI R, ESPOSITO A, PIETRANTONIO G et al. (2011).
Evidence of large
scale deformation patterns from GPS data in the Ita
lian subduction boundary.
Earth Planet Sci Lett
311:230–241. DOW, J.M.; NEILAN, R.E.; GENDT, G. (2005). The Inte
rnational GPS Service
(IGS): Celebrating the 10th Anniversary and Looking
to the Next Decade,
Adv.
Space Res.,
36, 320-326.
FADIL A, VERNANT P, MCCLUSKY S et al. (2006). Activ
e tectonics of the
western Mediterranean: geodetic evidence for rollba
ck of a delaminated
subcontinental lithospheric slab beneath the Rif Mo
untains, Morocco.
Geology
34:529–532
MCCLUSKY S, REILINGER R, MAHMOUD S et al. (2003). G
PS constraints on
Africa (Nubia) and Arabia plate motions.
Geophys J Int
155:126–138.
MARÍN-LECHADO C, GALINDO-ZALDÍVAR J, GIL AJ et al.
(2010). Levelling
profiles and a GPS network to monitor the active fo
lding and faulting
deformation in the Campo de Dalias (Betic Cordiller
a, Southeastern Spain).
Sensors 10:3504–3518.
WESSEL, P. AND W. H. F. SMITH (1998). New improved
version of the Generic
Mapping Tools released,
EOS Trans.
AGU
, 79, 579.
08: an improved
solution of the international terrestrial reference
frame.
J Geod
85:457–473
AVALLONE A, SELVAGGI G, D’ANASTASIO E et al (2010).
The RING
network: improvement of a GPS velocity field in the
central Mediterranean.
Ann
Geophys
53:39–54.
BIANCO, G., DEVOTI, R., LUCERI, V. (2003). Combinat
ion of loosely
constrained solutions.
IERS Tech. Note
30, 107–109.
DACH, R., U. HUGENTOBLER, P. FRIDEZ, AND M. MEINDL,
Eds. (2007).
Bernese GPS Software, Version 5.0, User Manual, Ast
ronomical Institute,
University of Bern. Bern. Switzerland.
DEVOTI, R., RIGUZZI, F., CUFFARO, M., DOGLIONI, C.
(2008). New GPS
constraints on the kinematics of the Apennine subdu
ction.
Earth and Planetary
Science Letters,
273 (1–2), 163–174.
DEVOTI R, ESPOSITO A, PIETRANTONIO G et al. (2011).
Evidence of large
scale deformation patterns from GPS data in the Ita
lian subduction boundary.
Earth Planet Sci Lett
311:230–241. DOW, J.M.; NEILAN, R.E.; GENDT, G. (2005). The Inte
rnational GPS Service
(IGS): Celebrating the 10th Anniversary and Looking
to the Next Decade,
Adv.
Space Res.,
36, 320-326.
FADIL A, VERNANT P, MCCLUSKY S et al. (2006). Activ
e tectonics of the
western Mediterranean: geodetic evidence for rollba
ck of a delaminated
subcontinental lithospheric slab beneath the Rif Mo
untains, Morocco.
Geology
34:529–532
MCCLUSKY S, REILINGER R, MAHMOUD S et al. (2003). G
PS constraints on
Africa (Nubia) and Arabia plate motions.
Geophys J Int
155:126–138.
MARÍN-LECHADO C, GALINDO-ZALDÍVAR J, GIL AJ et al.
(2010). Levelling
profiles and a GPS network to monitor the active fo
lding and faulting
deformation in the Campo de Dalias (Betic Cordiller
a, Southeastern Spain).
Sensors 10:3504–3518.
WESSEL, P. AND W. H. F. SMITH (1998). New improved
version of the Generic
Mapping Tools released,
EOS Trans.
AGU
, 79, 579.
Type
article
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