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  • 1
    Call number: ILP/M 06.0135
    In: Publication of the International Lithosphere Programme
    In: Tectonophysics
    Type of Medium: Monograph available for loan
    Pages: XI, 283 S. : Ill., graph. Darst.
    Series Statement: Publication of the International Lithosphere Programme 281a
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: ILP/M 06.0139
    In: Publication of the International Lithosphere Programme
    In: Tectonophysics
    Type of Medium: Monograph available for loan
    Pages: IX, 352 S. : Ill., graph. Darst., Kt.
    Series Statement: Publication of the International Lithosphere Programme 281b
    Location: Reading room
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  • 3
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 4/M 91.0338 ; M 92.0236
    Type of Medium: Monograph available for loan
    Pages: IX, 436 S.
    ISBN: 3540516093
    Series Statement: Exploration of the deep continental crust
    Language: English
    Location: Reading room
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 4
    Call number: 21/SR 90.0917(16-18) ; 21/SR 90.0917(16)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 16
    Type of Medium: Series available for loan
    Pages: 64 Seiten , Illustrationen , 30 cm
    Edition: Als Manuskript gedruckt
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 16
    Language: German , English
    Note: Enthält auch: Erkenntnisse der Gebirgsmechanik über.das mechanische Verhalten verschiedenartiger Gesteine / Höfer, K.-H. , Enthält auch: Zur Bedeutung der Crack-porosity bei Messungen unter hydrostatischem Druck / HURTIG, E.; u. a. , Enthält auch: Lateral inhomogeneities of the Earth's mantle and their petrological interpretation / FUCHS, K.; LIEBAU, F.; MAYER-ROSA, D. , Enthält auch: Velocity and density distributions in the upper mantle of Europe as derived from seismological observations / MAYER-ROSA, D.; MÜLLER, St. , Enthält auch: Die Druckabhängigkeit der CURIE-Temperatur von Titanomagnetiten / SCHULT, A. , Enthält auch: Die elektrische Leitfähigkeit von natürlichen Olivinen bei hohen Drücken und Temperaturen / SCHOBER, M.; SCHULT, A. , Enthält auch: Betrachtungen zum Näherungscharakter von Festkörpermodellen für das Erdinnere / STILLER, H. , Enthält auch: Influence of pore-fluid pressure in rocks on tensile cracking under high pressure / TEISSEYRE, R. , Enthält auch: Die Hochdrucktechnologie des Zentralinstituts Physik der Erde in Potsdam und die Zusammenarbeit mit dem Zentralinstitut Physik der Erde in Moskau auf dem Gebiet der Hochdruck-Hochtemperatur-Physik / VOLLSTÄDT, H.: WAGNER, F.C. , Enthält auch: Experimentelle Untersuchung der spezifischen Volumendeformation, der Kompressibilität und der Dichte von Gesteinen unter hohem Druck / LEBEDEV, T.S.; SAPOVAL, V.I. ; KORCIN, V.A. , Enthält auch: Der elektrische Widerstand von Mineralen und Gesteinen unter hohen Drücken und Temperaturen und der Bau der ·Erdkruste und des oberen Erdmantels / OESBERG, R.-P. , Enthält auch: On the possible density d.ecrease of the upper mantle in the saismic channel zone for Vs / TARKOV, A.P. , Enthält auch: Apparate und Methoden zur Untersuchung physikalischer Eigenschaften von Gesteinen unter hohen Drücken / VOLAROVIC, M.P.
    Location: Reading room
    Location: Reading room
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    Branch Library: GFZ Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: 4/M 92.1327/16 ; ILP/M 06.0119
    In: Geodynamics series
    In: Publication of the International Lithosphere Programme
    Type of Medium: Monograph available for loan
    Pages: xi, 327 S. : graph. Darst.
    ISBN: 0875905188
    Series Statement: Geodynamics series 16
    Classification:
    Geophysical Deep Sounding
    Language: English
    Location: Reading room
    Location: Reading room
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    Branch Library: GFZ Library
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  • 6
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: We introduce a new technique for rapidly heating (106 °C/s) thin films using an electrical thermal annealing (ETA) pulse technique. By applying a high-current dc electrical pulse to a conductive substrate-heater material (Si), joule heating occurs thus heating the thin film. This method was demonstrated by heating thin films of aluminum at rates ranging from 103 to 106 °C/s. The temperature of the system is measured by using the substrate heater as a thermistor and is found to be within ≈±10 °C during anneals at ≈105 °C/s. Phase transformations in the Ti-Si system were also observed using in situ resistivity measurements during ETA at ≈104 °C.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Exposed crystalline basement of the Serre Mountains in Calabria presents a tilted block of a nearly complete section of the Hercynian continental lower crust (HCLC). In addition to petrological and structural data from surface mapping, and petrophysical data from the laboratory, a seismic reflection-refraction experiment was conducted in May 1990. This consisted of a 40 km long N-S profile crossing the HCLC and of four short transverse profiles, each recorded using 3-component receivers with an 80 m spacing and explosive sources.The reflectivity of the outcropping lower crustal units is lower than theoretically predicted from the observed compositional layering. A low-velocity zone, outcropping in the north, and dipping to the south, marks the contact between the HCLC and the underlying Alpine metamorphic units. Below this zone, the deeper crust appears well-structured by strong and continuous, discrete reflections down to 6.5–8 s t.w.t. (presumably the crust-mantle boundary at 19–24 km depth) with a dominant dip toward the south.Analysis of refracted-wave velocities reveals values systematically lower by up to 30% than laboratory data on rock samples or calculated data from modal analysis. This discrepancy can only partly be explained by the effect of microcracks (10%), the underestimation of the amount of leucosomes (2–5%) and the effect of seismic anisotropy (0–5%). The remaining discrepancy must be attributed to large scale alteration of the rocks due to Apennine tectogenetic events.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 116 (2002), S. 7137-7144 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: Complex (dielectric) permittivity spectra of aqueous solutions of the monosaccharides D-Xylose, D-Galactose, D-Glucose, D-Fructose, Methyl-β-D-xylose, and Methyl-β-D-glucose, as well as the disaccharides D-Lactose, D-Maltose, and D-Sucrose have been measured. In order to avoid any systematic errors, various experimental setups, each matched to a particular measuring range, have been used to cover the frequency domain from 300 kHz to 40 GHz. In some characteristic details our spectra for maltose solutions deviate from those recently reported by Weingärtner et al. [J. Chem. Phys. 115, 1463 (2001)]. The monosaccharide spectra at c=1 mol/l and the disaccharide spectra at c≤0.5 mol/l reveal a rather homogeneous relaxation of the carbohydrate and water dipole moments, which can be well represented by a Cole–Cole relaxation time distribution. At higher solute concentration the dielectric spectra are favorably represented by two relaxation terms, though interpolation of the experimental data by the Cole–Cole spectral function is possible within the limits of errors. There are indications that these terms might be due to local fluctuations in the carbohydrate concentration, in conformity with previous ultrasonic spectra of monosaccharide solutions.© 2002 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 125 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: This paper presents an updated interpretation of seismic anisotropy within the uppermost mantle of southern Germany. The dense network of reversed and crossing refraction profiles in this area made it possible to observe almost 900 traveltimes of the Pn phase that could be effectively used in a time-term analysis to determine horizontal velocity distribution immediately below the Moho. For 12 crossing profiles, amplitude ratios of the Pn phase compared to the dominant crustal phase were utilized to resolve azimuthally dependent velocity gradients with depth. A P-wave anisotropy of 3–4 per cent in a horizontal plane immediately below the Moho at a depth of 30 km, increasing to 11 per cent at a depth of 40 km, was determined. For the axis of the highest velocity of about 8.03 km s−1 at a depth of 30 km a direction of N31°F was obtained. The azimuthal dependence of the observed Pn amplitude is explained by an azimuth-dependent sub-Moho velocity gradient decreasing from 0.06 s−1 in the fast direction to 0 s−1 in the slow direction of horizontal P-wave velocity. From the seismic results in this study a petrological model suggesting a change of modal composition and percentage of oriented olivine with depth was derived.
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 103 (1990), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Compared to clear crustal P- and S-waves as well as a strong refracted Pn-wave propagating in the topmost mantle (i.e., 10 to 15 km below the Moho), an anomalously weak appearance of the corresponding refracted shear wave Sn is observed on refraction seismic profiles in SW Germany, France, coastal Maine (NE United States) and Fennoscandia. It is possible that the observation of Pn/PMP ratios close to unity combined with small Sn/SMS ratios (i.e., small Sn amplitudes) is typical for the continental uppermost mantle since this was observed for quite different types of continental crust. It is shown that the observed phenomenon is not a source effect. Several possible causes to explain the observations are studied, also with the aid of synthetic seismograms. The effects of temperature, attentuation and anisotropy have been investigated. Their influence cannot explain the observations. The most likely candidate is a depth-increasing VP/VS ratio (an increase in the order of 0.027 over a depth range of 10 km), forcing P- and S-waves to propagate on different paths in the topmost mantle. The observed phenomenon provides new constraints on the change of composition with depth for the crust mantle transition zone with basalt depletion as the most likely explanation.
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