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Plate kinematic of Nubia-Somalia using combined DORIS and GPS solution / Jean-Mathieu Nocquet in Journal of geodesy, vol 80 n° 8-11 (November 2006)
[article]
Titre : Plate kinematic of Nubia-Somalia using combined DORIS and GPS solution Type de document : Article/Communication Auteurs : Jean-Mathieu Nocquet , Auteur ; Pascal Willis , Auteur ; S. Garcia, Auteur Année de publication : 2006 Article en page(s) : pp 591 - 607 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] Afrique (géographie physique)
[Termes IGN] bruit blanc
[Termes IGN] bruit rose
[Termes IGN] champ de vitesse
[Termes IGN] géodynamique
[Termes IGN] International Terrestrial Reference Frame
[Termes IGN] Nubie
[Termes IGN] positionnement cinématique
[Termes IGN] positionnement par DORIS
[Termes IGN] positionnement par GPS
[Termes IGN] rift
[Termes IGN] série temporelle
[Termes IGN] Somalie
[Termes IGN] tectonique des plaquesRésumé : (Auteur) We have used up to 12 years of data to assess DORIS performance for geodynamics applications. We first examine the noise characteristics of the DORIS time-series of weekly station coordinates to derive realistic estimates of velocity uncertainties. We find that a combination of white and flicker noise best explains the DORIS time-series noise characteristics. Second, weekly solutions produced by the Institut Géographique National/Jet Propulsion Laboratory (IGN/JPL) DORIS Analysis Centre are combined to derive a global velocity field. This solution is combined with two independent GPS solutions, including 11 sites on Nubia and 5 on the Somalia plate. The combination indicates that DORIS horizontal velocities have an average accuracy of 3 mm/year, with best-determined sites having velocity accuracy better than 1 mm/year (one-sigma levels). Using our combined velocity field, we derive an updated plate kinematics model with a focus on the Nubia–Somalia area. Including DORIS data improves the precision of the angular velocity vector for Nubia by 15%. Our proposed model provides robust bounds on the maximum opening rates along the East African Rift (4.7–6.7 mm/year). It indicates opening rates 15 and 7% slower than values predicted by NUVEL-1A for the southern Atlantic Ocean and Indian Ocean, respectively. These differences are likely to arise from the fact that NUVEL-1A considered Africa as a single non-deforming plate, while here we use a more refined approach. Copyright Springer Numéro de notice : A2006-536 Affiliation des auteurs : IGN+Ext (1940-2011) Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-006-0078-0 En ligne : https://doi.org/10.1007/s00190-006-0078-0 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28259
in Journal of geodesy > vol 80 n° 8-11 (November 2006) . - pp 591 - 607[article]Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 266-06102 RAB Revue Centre de documentation En réserve L003 Disponible 266-06101 RAB Revue Centre de documentation En réserve L003 Disponible Plate Motion of India and Interseismic Strain in the Nepal Himalaya from GPS and DORIS Measurements / Pierre Bettinelli in Journal of geodesy, vol 80 n° 8-11 (November 2006)
[article]
Titre : Plate Motion of India and Interseismic Strain in the Nepal Himalaya from GPS and DORIS Measurements Type de document : Article/Communication Auteurs : Pierre Bettinelli, Auteur ; Jean-Philippe Avouac, Auteur ; Mireille Flouzat, Auteur ; F. Jouanne, Auteur ; Laurent Bollinger, Auteur ; Pascal Willis , Auteur ; Gyani Raja Chitrakar, Auteur Année de publication : 2006 Article en page(s) : pp 567 - 589 Note générale : bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] déformation de la croute terrestre
[Termes IGN] données DORIS
[Termes IGN] données GPS
[Termes IGN] Himalaya
[Termes IGN] tectonique des plaquesRésumé : (auteur) We analyse geodetically estimated deformation across the Nepal Himalaya in order to determine the geodetic rate of shortening between Southern Tibet and India, previously proposed to range from 12 to 21 mm yr−1. The dataset includes spirit-levelling data along a road going from the Indian to the Tibetan border across Central Nepal, data from the DORIS station on Everest, which has been analysed since 1993, GPS campaign measurements from surveys carried on between 1995 and 2001, as well as data from continuous GPS stations along a transect at the logitude of Kathmandu operated continuously since 1997. The GPS data were processed in International Terrestrial Reference Frame 2000 (ITRF2000), together with the data from 20 International GNSS Service (IGS) stations and then combined using quasi- observation combination analysis (QOCA). Finally, spatially complementary velocities at stations in Southern Tibet, initially determined in ITRF97, were expressed in ITRF2000. After analysing previous studies by different authors, we determined the pole of rotation of the Indian tectonic plate to be located in ITRF2000 at 51.409±1.560° N and −10.915±5.556°E, with an angular velocity of 0.483±0.015°. Myr−1. Internal deformation of India is found to be small, corresponding to less than about 2 mm yr−1 of baseline change between Southern India and the Himalayan piedmont. Based on an elastic dislocation model of interseismic strain and taking into account the uncertainty on India plate motion, the mean convergence rate across Central and Eastern Nepal is estimated to 19±2.5 mm yr−1, (at the 67% confidence level). The main himalayan thrust (MHT) fault was found to be locked from the surface to a depth of about 20 km over a width of about 115 km. In these regions, the model parameters are well constrained, thanks to the long and continuous time-series from the permanent GPS as well as DORIS data. Further west, a convergence rate of 13.4±5 mm yr−1, as well as a fault zone, locked over 150 km, are proposed. The slight discrepancy between the geologically estimated deformation rate of 21±1.5 mm yr−1 and the 19±2.5 mm yr−1 geodetic rate in Central and Eastern Nepal, as well as the lower geodetic rate in Western Nepal compared to Eastern Nepal, places bounds on possible temporal variations of the pattern and rate of strain in the period between large earthquakes in this region. Numéro de notice : A2006-673 Affiliation des auteurs : IGN+Ext (1940-2011) Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-006-0030-3 Date de publication en ligne : 08/03/2006 En ligne : https://doi.org/10.1007/s00190-006-0030-3 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=102742
in Journal of geodesy > vol 80 n° 8-11 (November 2006) . - pp 567 - 589[article]Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 266-06102 RAB Revue Centre de documentation En réserve L003 Disponible 266-06101 RAB Revue Centre de documentation En réserve L003 Disponible Twenty years of evolution for the DORIS permanent network: from its initial deployment to its renovation / Hervé Fagard in Journal of geodesy, vol 80 n° 8-11 (November 2006)
[article]
Titre : Twenty years of evolution for the DORIS permanent network: from its initial deployment to its renovation Type de document : Article/Communication Auteurs : Hervé Fagard, Auteur Année de publication : 2006 Article en page(s) : pp 429 - 456 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géodésie spatiale
[Termes IGN] altimétrie
[Termes IGN] DORIS
[Termes IGN] historique
[Termes IGN] Institut géographique national (France)
[Termes IGN] International Terrestrial Reference Frame
[Termes IGN] orbitographie
[Termes IGN] positionnement par DORIS
[Termes IGN] précision centimétrique
[Termes IGN] précision décimétrique
[Termes IGN] réseau Doris
[Termes IGN] secteur terrien
[Termes IGN] tectonique des plaquesRésumé : (Auteur) The ground network is one of the major components of the DORIS system. Its deployment, managed by the French national mapping agency [Institut Géographique National, (IGN)], started in 1986 at a sustained pace that allowed it to reach 32 stations upon the launch of the first DORIS-equipped satellite (SPOT-2) in 1990. For the first generation of transmitting antennas, the installation procedures were adapted to the decimetre performance objective for the DORIS system. During the second era of the deployment of an even denser network, the antenna support layouts gradually evolved towards a better quality, thus improving the long-term stability of the antenna reference point, and a new antenna model allowed a more accurate survey. As the positioning accuracy of the DORIS system improved, it was necessary to review the antenna stability for the whole network. A first stability estimation, using criteria like antenna model and support design, was followed by a major renovation effort which started in 2000 and is now almost complete. In 6 years, through the renovation or installation of 43 stations and the implementation of new installation procedures to meet more stringent stability requirements, significant improvement in network quality was achieved. Later a more analytical approach, taking into account the characteristics of each element that support the antenna, has been taken to assess the potential stability of all DORIS occupations. IGN is also in charge of its operational maintenance, an intensive activity on account of the significant failure rate of the successive generations of equipment. Nevertheless, thanks to its unique density and homogeneity, DORIS has maintained a very good coverage rate of the satellite orbits. Through 38 well-distributed current co-locations with the Global Positioning System, Satellite Laser Ranging and Very Long Baseline Interferometry techniques in its current 56-station network, DORIS contributes significantly to the realisation of the International Terrestrial Reference System. DORIS stations in areas where no other space geodesy technique is available provide a significant contribution to the study of plate tectonics. Many stations co-located with tide gauges contribute to the monitoring of sea level changes. Although it has several advantages over similar techniques, there is still room for improvement in the DORIS network. Copyright Springer Numéro de notice : A2006-533 Affiliation des auteurs : IGN (1940-2011) Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-006-0084-2 En ligne : https://doi.org/10.1007/s00190-006-0084-2 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28256
in Journal of geodesy > vol 80 n° 8-11 (November 2006) . - pp 429 - 456[article]Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 266-06102 RAB Revue Centre de documentation En réserve L003 Disponible 266-06101 RAB Revue Centre de documentation En réserve L003 Disponible Kinematics of the North American–Caribbean-Cocos plates in Central America from new GPS measurements across the Polochic-Motagua fault system / H. Lyon-Caen in Geophysical research letters, vol 33 n° 19 (Octobre 2006)
[article]
Titre : Kinematics of the North American–Caribbean-Cocos plates in Central America from new GPS measurements across the Polochic-Motagua fault system Type de document : Article/Communication Auteurs : H. Lyon-Caen, Auteur ; E. Barrier, Auteur ; Cécile Lasserre, Auteur ; A. Franco, Auteur ; I. Arzu, Auteur ; L. Chiquin, Auteur ; M. Chiquin, Auteur ; Thierry Duquesnoy , Auteur ; O. Flores, Auteur ; O. Galicia, Auteur ; J. Luna, Auteur ; E. Molina, Auteur ; O. Porras, Auteur Année de publication : 2006 Article en page(s) : n° L19309 Note générale : bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géodésie physique
[Termes IGN] Amérique centrale
[Termes IGN] Amérique du nord
[Termes IGN] déformation de la croute terrestre
[Termes IGN] faille géologique
[Termes IGN] subduction
[Termes IGN] tectonique des plaquesRésumé : (auteur) The Polochic-Motagua strike-slip fault system in Guatemala marks the on-land plate boundary between the North American (NA) and the Caribbean (CA) plates. GPS observations in 1999 and 2003 show that the far-field velocity across the system (NA-CA relative velocity) is ∼20 mm/yr. This is significantly higher than the NUVEL-1A velocity but is consistent with the GPS based CA-NA velocity proposed by DeMets et al. (2000). The observations are modeled by a fault centered on the Motagua fault, locked at a depth of 20 km, with a slip-rate decreasing from eastern to central Guatemala from 20 to 12 mm/yr towards the NA-CA-Cocos triple junction. This decrease is accommodated by ∼8 mm/yr of E-W extension in the westernmost part of CA south of the Motagua fault. About 10 mm/yr of dextral slip is observed across the Mid-American Volcanic Arc. The NA-CA-Cocos triple junction is thus a complex, ∼400 km-wide wedge-shaped area. Numéro de notice : A2006-676 Affiliation des auteurs : IGN+Ext (1940-2011) Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1029/2006GL027694 Date de publication en ligne : 11/10/2006 En ligne : https://doi.org/10.1029/2006GL027694 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=102947
in Geophysical research letters > vol 33 n° 19 (Octobre 2006) . - n° L19309[article]Determination of postglacial land uplift in Fennoscandia from leveling, tide-gauges and continuous GPS stations using least squares collocation / O. Vestol in Journal of geodesy, vol 80 n° 5 (August 2006)
[article]
Titre : Determination of postglacial land uplift in Fennoscandia from leveling, tide-gauges and continuous GPS stations using least squares collocation Type de document : Article/Communication Auteurs : O. Vestol, Auteur Année de publication : 2006 Article en page(s) : pp 248 - 258 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] altitude
[Termes IGN] collocation par moindres carrés
[Termes IGN] données altimétriques
[Termes IGN] données GPS
[Termes IGN] données marégraphiques
[Termes IGN] Fennoscandie
[Termes IGN] rebond post-glaciaire
[Termes IGN] réseau de nivellement
[Termes IGN] réseau géodésique local
[Termes IGN] réseau géodésique permanent
[Termes IGN] station permanente
[Termes IGN] tectonique des plaquesRésumé : (Auteur) Precise leveling, tide-gauge recordings and time series from continuous GPS stations are all sources of information about the ongoing postglacial land uplift in Fennoscandia. This article describes how to gather these three sources of data together in a least-squares collocation adjustment in order to calculate uplift rates, as well as new heights for the benchmarks in the leveling network. The estimated reliability of the resulting uplift model is in general better than 0.4 mm/year, decreasing in areas of fewer data. Copyright Springer Numéro de notice : A2006-367 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-006-0063-7 En ligne : https://doi.org/10.1007/s00190-006-0063-7 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28091
in Journal of geodesy > vol 80 n° 5 (August 2006) . - pp 248 - 258[article]Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 266-06071 RAB Revue Centre de documentation En réserve L003 Disponible 266-06072 RAB Revue Centre de documentation En réserve L003 Disponible Étude par télédétection radar du processus tectonique d'échappement : comparaison entre l'Anatolie et les Andes vénézuéliennes / D. Dhont in Photo interprétation, vol 42 n° 2 (Juin 2006)PermalinkMesure de la déformation de l'écorce terrestre par géodésie spatiale [diaporama] / Jérome Verdun (2006)PermalinkMesures GPS continues et tectonique des plaques / Christophe Vigny in Géochronique, n° 94 (juin - août 2005)PermalinkLa tectonique de la Méditerranée vue par GPS / Jean-Mathieu Nocquet in Géochronique, n° 94 (juin - août 2005)PermalinkUtilisation des données GPS pour la réalisation de la carte géodynamique de la Méditerranée / Nicolas Chamot-Rooke in Géochronique, n° 94 (juin - août 2005)PermalinkUtilisation du GPS dans l'étude des séismes et du cycle sismique / F. Rolandone in Géochronique, n° 94 (juin - août 2005)Permalink[Le réseau Teria] les scientifiques vont disposer d'un réseau beaucoup plus important / Pierre Briole in Géomètre, n° 2012 (février 2005)PermalinkApplication of wavelet analysis to the study of spatial pattern of morphological lineaments in digital terrain models: a case study / Gyozo Jordan in Remote sensing of environment, vol 94 n° 1 (15/01/2005)PermalinkCan tectonic processes be recovered from new gravity satellite data? / Valentin O. Mikhailov in Earth and planetary science letters, vol 228 n° 3-4 (15 December 2004)PermalinkIs the Amik Basin (SE Turkey) a triple-junction area? Analyses of SPOT XS imagery and seismicity / S. Over in International Journal of Remote Sensing IJRS, vol 25 n° 19 (October 2004)Permalink