Auflistung Scientific Technical Report / Deutsches Geoforschungszentrum Potsdam nach Titel
Anzeige der Dokumente 117-129 von 129
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The changing geomagnetic field from the ionosphere to the core-mantle boundary
(GFZ, Potsdam[Bibliothek des Wiss.-Parks Albert Einstein] [Vertrieb], [Potsdam], 2008) -
The effect of the geocentric gravitational constant on scale - (submitted to journal of geodesy)
(Scientific Technical Report / Geoforschungszentrum Potsdam; 2001, 12) -
The paleostress history of the Central European Basin System
(GFZ, Helmholtz-Zentrum, Potsdam, 2009)The Central European Basin System (CEBS) is a complex intracontinental system of sedimentary basins that have evolved through several geodynamic phases since Late Carboniferous times. The basin system is framed by the ... -
Theory of elastic waves
Müller, Gerhard;
(Scientific Technical Report / Geoforschungszentrum Potsdam; 2007, 03)
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Thermal properties of gas hydrate bearing sediments and effects of phase transitions on the transport of heat deduced from temperature logging at Mallik, NWT, Canada
(GFZ, Helmholtz-Zentrum, 2005)
Detailed knowledge about the thermal properties of rocks containing gas hydrate is required in order to quantify processes involving the formation and decomposition of gas hydrate in nature. This work investigates the ... -
Thermomechanical polythermal ice-sheet model
(GFZ, Helmholtz-Zentrum[Bibliothek des Wissenschaftsparks Albert Einstein] [Vertrieb], [Potsdam], 2006) -
Vertical crustal motion at tide gauges derived by analyzing GPS time series
(Scientific Technical Report / Deutsches Geoforschungszentrum Potsdam GFZ; 2008, 03) -
Wavelet-Analysen ozeanischer Drehimpulszeitreihen
(GFZ, Helmholtz-Zentrum, 2003)This report presents the results of a wavelet analysis of Ocean Angular Momentum (OAM) time series, that were generated by the OMCT-Model (Ocean Model for Circulation and Tides). The findings from this analysis were then ... -
Zeitliche Schwereänderungen und glazio-isostatische Ausgleichsprozesse am Vatnajökull, Südostisland
(GFZ, Helmholtz-Zentrum, 2002)Der glazio-isostatische Ausgleich in Island als Folge des Abschmelzens der größten europäischen Eiskappe, dem Vatnajökull, verursacht zeitliche Änderungen der Schwere und Landhebung. Nach Auswertung der Schweredaten zeigt ... -
Zur Bestimmung des cm-Geoids und dessen zeitlicher Variationen mit GRACE
(GFZ, Helmholtz-Zentrum, 2007) -
Zur Theorie der Multipole und ihre Anwendung bei der Schwerefeldberechnung
(Scientific Technical Report / Geoforschungszentrum Potsdam; 2004, 14)
