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Combination of solutions for geodetic and geodynamic applications of the Global Positioning System (GPS) / Elmar Brockmann (1996)
Titre : Combination of solutions for geodetic and geodynamic applications of the Global Positioning System (GPS) Type de document : Monographie Auteurs : Elmar Brockmann, Auteur Editeur : Zurich : Schweizerischen Geodatischen Kommission / Commission Géodésique Suisse Année de publication : 1996 Collection : Geodätisch-Geophysikalische Arbeiten in der Schweiz, ISSN 0257-1722 num. 55 Importance : 211 p. Format : 21 x 30 cm Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géodésie spatiale
[Termes IGN] compensation par moindres carrés
[Termes IGN] compensation séquentielle
[Termes IGN] convolution (signal)
[Termes IGN] données GPS
[Termes IGN] orbitographie
[Termes IGN] série temporelle
[Termes IGN] traitement de données GNSS
[Termes IGN] vitesseIndex. décimale : 30.61 Systèmes de Positionnement par Satellites du GNSS Numéro de notice : 55997 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Monographie En ligne : https://www.sgc.ethz.ch/sgc-volumes/sgk-55.pdf Format de la ressource électronique : URL Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=59954 Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 55997-01 30.61 Livre Centre de documentation Géodésie Disponible 55997-02 30.61 Livre Centre de documentation Géodésie Disponible Crustal deformation of the Yellowstone volcanic field from precise measurements of temporal gravity changes and supplementary leveling and GPS data / Felix Karl Arnet (1996)
Titre : Crustal deformation of the Yellowstone volcanic field from precise measurements of temporal gravity changes and supplementary leveling and GPS data Type de document : Thèse/HDR Auteurs : Felix Karl Arnet, Auteur Editeur : Zurich : Institut für Geodäsie und Photogrammetrie IGP - ETH Année de publication : 1996 Collection : IGP Mitteilungen, ISSN 0252-9335 num. 056 Importance : 125 p. Format : 21 x 30 cm ISBN/ISSN/EAN : 978-3-906513-79-9 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] champ de pesanteur local
[Termes IGN] déformation de la croute terrestre
[Termes IGN] données GPS
[Termes IGN] géophysique interne
[Termes IGN] levé gravimétrique
[Termes IGN] nivellement direct
[Termes IGN] volcan
[Termes IGN] Wyoming (Etats-Unis)Index. décimale : 30.82 Applications géophysiques de géodésie spatiale Résumé : (Auteur) The Yellowstone caldera in northwest of Wyoming, U.S.A, shows high rates of height and gravity changes. The height changes were monitored by precise leveling, which was first conducted in 1923 and remeasured every few years since 1975. Gravity measurements were first carried out in 1977 and repeated almost annually since 1983. Both measuring types were concentrated on a line crossing the northern part of the caldera. A GPS network was installed additionally in 1987. It covers the whole national park region and was remeasured every second year. The measurements showed, that the Caldera experienced an uplift of up to 0.8 m from 1923 to 1984. Since 1984, the trend reversed and the heights decreased up to 14 em. The gravity values along the same line changed up to 60 ± 12 µgal ( 1 µgal = 10 8 m S2 ) from 1977 to 1986. Until 1993, the gravity increased again up to +60 ± 12 µgal. The GPS results showed within the bounds of accuracy the same height changes as the precision leveling. In addition, horizontal displacements of up to 3 em towards the middle of the caldera were observed. Furthermore, it showed that the area of downshift expands partly considerably over the borders of the Yellowstone caldera. The factor between the height and gravity changes is a value that can be used to detect mass changes at depth. This value varies strongly from year to year. Over longer time spans, it converges towards the freeair gravity gradient of 0.3 mgal/m, where no mass changes occur. Finite element modeling shows, that the earth's crust in the Yellowstone National Park does not behave like an ideal elastic material. The horizontal displacements are significantly smaller than expected from the height changes. This is explained by the geology heavily disturbed by a lot of fault zones. Numéro de notice : 45614 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère DOI : 10.3929/ethz-a-001549641 En ligne : http://dx.doi.org/10.3929/ethz-a-001549641 Format de la ressource électronique : URL Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=58404 Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 45614-01 30.82 Livre Centre de documentation Géodésie Disponible 45614-02 30.82 Livre Centre de documentation Géodésie Disponible Ein hybrides System in der Geodäsie. Einsatz des NAVSTAR GPS mit dem Strapdown-Inertial-Navigations- system LASERNAV II für kinematische Punktbestimmung und Orientierung / Wolfgang Söhne (1996)
Titre : Ein hybrides System in der Geodäsie. Einsatz des NAVSTAR GPS mit dem Strapdown-Inertial-Navigations- system LASERNAV II für kinematische Punktbestimmung und Orientierung Titre original : [Un système hybride dans le recours géodésique au GPS avec un système inertiel de navigation à composants liés LASERNAV 2 pour la détermination de points et l'orientation] Type de document : Thèse/HDR Auteurs : Wolfgang Söhne, Auteur Editeur : Munich : Bayerische Akademie der Wissenschaften Année de publication : 1996 Collection : DGK - C Sous-collection : Dissertationen num. 463 Importance : 88 p. Format : 21 x 30 cm ISBN/ISSN/EAN : 978-3-7696-9504-5 Note générale : Bibliographie Langues : Allemand (ger) Descripteur : [Vedettes matières IGN] Géodésie spatiale
[Termes IGN] ambiguïté entière
[Termes IGN] données GPS
[Termes IGN] filtre de Kalman
[Termes IGN] GPS-INS
[Termes IGN] phase GPS
[Termes IGN] positionnement cinématique
[Termes IGN] résolution d'ambiguïtéIndex. décimale : 30.64 GPS et centrales inertielles Résumé : (Auteur) The combination of a medium accuracy strapdown inertial navigation system with GPS as an example for an integrated geodetic useable system is presented. First the GPS observables used within this paper are descri-bed and the mean problems concerning with kinematic use of GPS like ambiguity resolution, cycle slips and multipath are pointed out. To adjust the ambiguities in a fast and efficient way a Kalman filter algorithm is presented. The results of the integrated system using different types of vehicles are described. Finally it is shown that by using the observations of all available antennas the accuracy for attitude calculation is the highest one. Numéro de notice : 28030 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=63377 Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 28030-01 30.64 Livre Centre de documentation Géodésie Disponible 28030-02 30.64 Livre Centre de documentation Géodésie Disponible Geometrische Modellierung innerer und äußerer Deformationen der Erdoberfläche mit Anwendungen an der Nord-anatolischen Verwerfung und in der Westtürkei / Y. Altiner (1996)
Titre : Geometrische Modellierung innerer und äußerer Deformationen der Erdoberfläche mit Anwendungen an der Nord-anatolischen Verwerfung und in der Westtürkei Titre original : [Modélisation géométrique des déformations internes et externes de la superficie terrestre avec application sur le plissement en Anatolie nord et dans l'ouest de la Turquie] Type de document : Thèse/HDR Auteurs : Y. Altiner, Auteur Editeur : Munich : Bayerische Akademie der Wissenschaften Année de publication : 1996 Collection : DGK - C Sous-collection : Dissertationen num. 462 Importance : 84 p. Format : 21 x 30 cm Note générale : Bibliographie Langues : Allemand (ger) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] collocation
[Termes IGN] déformation de la croute terrestre
[Termes IGN] données GPS
[Termes IGN] interpolation polynomiale
[Termes IGN] modèle mathématique
[Termes IGN] TurquieIndex. décimale : 30.82 Applications géophysiques de géodésie spatiale Numéro de notice : 28031 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=63378 Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 28031-01 30.82 Livre Centre de documentation Géodésie Disponible Recent crustal deformation and strain accumulation in the Marmara sea region, NW Anatolia, inferred from GPS measurements / Christian Straub (1996)
Titre : Recent crustal deformation and strain accumulation in the Marmara sea region, NW Anatolia, inferred from GPS measurements Type de document : Thèse/HDR Auteurs : Christian Straub, Auteur Editeur : Zurich : Institut für Geodäsie und Photogrammetrie IGP - ETH Année de publication : 1996 Collection : IGP Mitteilungen, ISSN 0252-9335 num. 058 Importance : 150 p. Format : 21 x 30 cm ISBN/ISSN/EAN : 978-3-906513-82-9 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de géodésie spatiale
[Termes IGN] analyse comparative
[Termes IGN] campagne GPS
[Termes IGN] déformation de la croute terrestre
[Termes IGN] données GPS
[Termes IGN] Marmara, mer de
[Termes IGN] positionnement par GPS
[Termes IGN] risque naturel
[Termes IGN] séismeIndex. décimale : 30.82 Applications géophysiques de géodésie spatiale Résumé : (auteur) This work analyzes recent crustal deformation in the Marmara Sea region, NW Anatolia, based on data derived from repeated GPS measurements. It is the geodetic part of the MARMARA poly-project of the Swiss Federal Institute of Technology (ETHZ). The overall goal of the Marmara poly-project is to examine the active tectonics and their interaction with groundwater circulation, heat flow and seismicity in northwestern Anatolia. In 1990, the Geodesy and Geodynamics Lab. (GGL) of the ETHZ established 52 GPS sites at the western end of the single strand North Anatolian Fault Zone (NAFZ) and its splaying into a complex fault system. This complexity is caused by the transition from the east-west oriented motion of the Anatolian block to the extensional regime of the Aegean Sea directing north-south. The GPS sites were occupied during three major GPS campaigns in 1990, 1992, and 1994. The GPS data were analyzed using the Bernese GPS Software. As a result of the combination of these campaigns a detailed velocity field of the transition zone between the westward motion of Anatolia and the extending Aegean Sea was obtained. The average rate of motion of Anatolia relative to Eurasia is 20 mm/a in a W direction. West of longitude 27.5°, the average direction of motion turns from W to WSW. From north to south, a gradual rate increase from 0 to 20 mm/a was found. Comparisons with deformation rates derived from the summation of seismic moment tensors suggest that less than 60% of the GPS inferred rates are released by earthquakes. The deformation rates are evaluated by means of strain and stress analysis, by using the method of collocation, examination of residuals relative to rigid Eulerian rotations, as well as a Finite Element model of the Marmara Sea region. Most deformation occurs along the northern strand of the NAFZ that runs from Mudurnu through the Gulf of izmit, passing the Marmara Sea, re-enters the Eurasian mainland and continuing to the Gulf of Saros. The Yalova peninsula endures considerable deformation as well. No significant deformation was found on the Biga peninsula. Thus, the western part of the middle strand that crosses the Biga peninsula is either inactive or locked. The Gulf of Edremit and the areas south of it are occupied by extensional processes in NNE-SSW direction (max. extension: 0.3 ppm/a [= u.strain/a]). The average shear-strain rate in the Marmara Sea region is 0.1 ppm/a (maximum shear: 0.3 ppm/a). The highest annual accumulation of density of strain energy (4 mJ/m3) and maximum shear stress (16 kN/m2) is located along the northern strand. The projection of the strain on the main fault allows us to determine the kind and amount of faulting that can be expected at individual fault lines. The dextral strike along the northern strand reaches 0.1-0.3 ppm/a. The results obtained from repeated GPS measurements compare well with the pattern of horizontal direction of major extension derived from seismotectonic and neotectonic data. In the East, the major horizontal extension directs NE-SW. Further to the west it gradually changes to almost N-S. Comparisons with rigid pole rotations for the Eastern Mediterranean, postulated by other authors, show that the Marmara region cannot be regarded as part of a rigid Anatolian block. The analysis of residuals to a rigid pole rotation of the Anatolian sites of the MARMARA GPS network (33.9°N, 29.8°E, CD=1.36°/Ma) depicts the location and size of the area of the main deformation. Cross-sectors radial to the best fitting pole reveal a detailed pattern of increase of deformation rates over the different fault lines. The deformation zones in the eastern and western part is narrow (=45 km). The zone for the middle sector undergoes a more distributed deformation (up to 100 km). The investigation of the radial residuals illustrates the overall extension of the Marmara region directing NE-SW. Finite Element calculations (2D, elasto-static) confirm the findings of the strain and stress analysis. Furthermore, they suggest that the known neotectonic fault geometry is capable of absorbing a considerable accumulation of distortion. However, the Finite Element model also gives indications for additional fault structures at the western end of the Marmara Sea and in Thrace, north and south of the northern strand striking subparallel to it. Finally, the strain field of the Eastern Mediterranean region is derived from GPS measurements spanning the whole region. The deformation pattern confirm the strong dextral motion along the NAFZ (0.2 ppm/a) as well as the extensional regimes of Western Anatolia and the Aegean Sea. Residuals from a rotation for the Eastern Mediterranean reveal that the Anatolian/Aegean region does not behave like a single rigid plate. The rates along the NAFZ show that there is a zone with a width of up to 100 km that endures strong internal deformation. The southern Aegean, Western, and Southwestern Greece do not fit to a simple rigid polar rotation at all. Numéro de notice : 68913 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Thèse étrangère DOI : 10.3929/ethz-a-001624667 En ligne : http://dx.doi.org/10.3929/ethz-a-001624667 Format de la ressource électronique : URL Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=64059 Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité 68913-01 30.82 Livre Centre de documentation Géodésie Disponible PermalinkThe Geodetic Antarctic Project GAP95. German contributions to the SCAR 95 Epoch campaign / R. Dietrich (1996)PermalinkThe Global Positioning System and GIS / M. Kennedy (1996)PermalinkThe reprocessing of the code IGS data of 1995 (the RIGS data campaign) / Serge Botton (1996)PermalinkZur Bahndynamik niedrigfliegender Satelliten / M. Scheinert (1996)PermalinkGeodetic measurements of convergence across the New Hebrides Subduction Zone / Stéphane Calmant in Geophysical research letters, vol 22 n° 19 (octobre 1995)PermalinkAnalyse der GPS-Alpentraverse / M. Vogel (1995)PermalinkErweiterte Modellbildung zur Netzausgleichung für die Deformationsanalyse, dargestellt am Beispiel der Geo- traverse Venezolanische Anden / H. Saler (1995)PermalinkPermalinkGPS measurements at the Nuottavaara post glacial fault / Markku Poutanen (1995)Permalink