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  • English  (814)
  • 1995-1999  (397)
  • 1980-1984  (421)
  • 1997  (397)
  • 1984  (421)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Stuttgart : Schweizerbart Science Publishers ; Volume 1, number 1 (1978)-
    Call number: M 18.91571
    Type of Medium: Monograph available for loan
    Pages: 134 Seiten
    ISSN: 2363-7196
    Series Statement: Global tectonics and metallogeny : special issue Vol. 10/2-4
    Classification:
    Tectonics
    Parallel Title: Erscheint auch als Global tectonics and metallogeny
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 3
  • 4
    Monograph available for loan
    Monograph available for loan
    [Edgecumbe, N.Z.] : A. Muller
    Call number: M 15.89146
    Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains
    Type of Medium: Monograph available for loan
    Pages: 223 S., , Ill.
    Language: English
    Branch Library: GFZ Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Institut für atmosphärische Umweltforschung der Fraunhofer- Gesellschaft
    Call number: MOP 44829 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 25 S. , graph. Darst.
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 6
    Publication Date: 2020-02-12
    Description: A local, broadband, seismic network of four observatory-quality stations (KTB-NET) was operated during the drilling of the KTB hole, within the framework of the interdisciplinary German Continental Deep Drilling Program (KTB). The aim was to investigate the seismic activity with regard to the tectonic stress field and to compare it with data from in situ measurements in the 9.1-km deep borehole sections (bottom temperature of 260°C and heat flow of 82–85 mW/m2). From October 1990 to November 1995, over 80 local microearthquakes with magnitudes from 0.2 to 2.8 ML were recorded: eight small events by the KTB-NET only and four earthquake swarms with 73 events by the KTB-NET and stations of the Vogtland/Western Bohemia networks. Six of the small events are located within or close to the KTB-NET. The swarm events occurred at the southwestern extension of the Ohre rift, in an area 20 km north of the drill site, which is revealed to be part of the Vogtland/Western Bohemia seismotectonic unit, characterized by swarm activity. The hypocenters are limited to the upper 13 km of the crust, with a distinct concentration between 10 and 12 km. All types of fault plane solutions are found, but at depths greater than 8 km, reversed faulting mechanisms predominate. P axes are very uniformly oriented in a NNW-SSE direction, corresponding to the well-known regional stress orientation in central Europe and in agreement with the special in situ stress measurements of the KTB program. The focal mechanism of a ML=1.2 event induced by a fluid injection experiment fits into the results obtained from the natural events. Possible indications for the brittle-ductile transition are discussed in view of the observed earthquake depth and focal mechanism distributions.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 7
    Publication Date: 2020-02-12
    Description: For almost 10 years the KTB superdeep drilling project has offered an excellent field laboratory for adapting seismic techniques to crystalline environments and for testing new ideas for interpreting seismic reflections in terms of lithological or textural properties of metamorphic rock units. The seismic investigations culminated in a three-dimensional (3-D) reflection survey on a 19 × 19 km area with the drill site at its center. Interpretation of these data resulted in a detailed, structural model of the German Continental Deep Drilling Program (KTB) location with dominant, steep faults in the upper crust. The 3-D reflection survey was part of a suite of seismic experiments, ranging from wide-angle reflection and refraction profiles to standard vertical seismic profiles (VSP) and more sophisticated surface-to-borehole observations. It was predicted that the drill bit would meet the most prominent, steeply dipping, crustal reflector at a depth of about 6500–7000 m, and indeed, the borehole penetrated a major fault zone in the depth interval between 6850 and 7300 m. This reflector offered the rare opportunity to relate logging results, reflective properties, and geology to observed and modeled data. Post-Variscan thrusting caused cataclastic deformation, with partial, strong alterations within a steeply dipping reverse fault zone. This process generated impedance contrasts within the fault zone on a lateral scale large enough to cause seismic reflections. This was confirmed by borehole measurements along the whole 9.1 km deep KTB profile. The strongest, reflected signals originated from fluid-filled fractures and cataclastic fracture zones rather than from lithological boundaries (i.e., first-order discontinuities between different rock types) or from texture- and/or foliation-induced anisotropy. During the interpretation of seismic data at KTB several lessons were learned: Conventional processing of two-dimensional (2-D) reflection data from a presite survey showed predominantly subhorizontal layering in the upper crust with reflectivity striking in the Variscan direction. Drilling, however, revealed that all rock units are steeply dipping. This confirms that surface common depth point (CDP) seismics strongly enhances subhorizontal reflectivity and may thus produce a very misleading crustal image. Although this was shown for synthetic examples earlier, the KTB provides the experimental proof of how crucial this insight can be.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 8
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    GFZ Data Services
    Publication Date: 2020-11-04
    Description: The PUNA (Plateau Untersuchung Nw Argentinien) seismograph network was deployed across the Andes at ∼23.5°S. The array was centered in the backarc, atop the Puna high plateau in NW Argentina and was in operation for approximately 100 days between late August and late November 1997. Most stations were equipped with short-period1-Hz 3-component seismometers and PDAS data loggers recording continuously 100 sps. The deployment was part of the collaborative research center „Deformation processes in the Andes - SFB267”. Waveform data are available from the GEOFON data centre, under network code ZB under CC-BY 4.0 license.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 9
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    In:  Upper Mantle Heterogeneities from Active and Passive Seismology
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/bookPart
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  • 10
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 11
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    In:  Geophysical Research Letters
    Publication Date: 2020-02-12
    Description: The tremor wave‐field at Mt.Etna was recorded with an array of three 3‐component broadband seismometers. The analysis of its polarisation and dispersion properties leads to the conclusions that (1) the wave‐field consists mainly of surface waves and that (2) two of the observed spectral peaks are caused by a wave guide effect along the propagation path.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 12
    Publication Date: 2020-02-12
    Description: The wave-field of volcano-induced seismic signals at Stromboli volcano (Italy) was observed using a network of four broadband seismometers. In addition to the standard spectral analysis of the recorded signals, new spectral techniques such as wavelet transform and wavelet coherence analysis were also used in order to discriminate between signals related to volcanic tremor and volcanic explosions. The common features of these two types of signals are characterised by the maximum of the power spectral density values located in the frequency band > 2.0 Hz, and the main orientation of the principal axes of the particle motion ellipsoids in the frequency bands analysed. The seismic signals of the volcanic explosions at Stromboli cover the total frequency band, whereas the spectral content of the volcanic tremor is restricted to narrow frequency bands ranging from 0.3–5.0 Hz. In order to localize both types of signals, a modified inversion technique was used. The result of this beam-forming on diffraction hyperboloids of both types of signals reveal a surprisingly shallow source location ranging from 0.2 km–0.7 km above sea level, suggesting that the sources of the volcanic explosions, as well as of the volcanic tremor, are restricted to the uppermost parts of the volcano. This is in agreement with several nonseismological observations of this volcano. The combination of spectral analysis of volcanic tremor and volcanic explosions with the analysis of ground displacement implies a mechanism which can be described by an ascending bubble of volcanic gas in a nearly closed volcanic system, and finally the forced ejection of the material through a narrow channel at the top of the magma column.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 13
    Publication Date: 2020-02-12
    Description: A fluid injection-induced seismicity experiment was conducted in the German Continental Deep Drilling Program (KTB) main borehole at 9.1 km depth (in situ temperature of 260°C) to extend knowledge about stress magnitudes and brittle faulting to depths and temperatures approaching the brittle-ductile transition. Almost 400 microearthquakes were induced at an average depth of 8.8 km by injection of KBr/KCl brine into a ∼70 m open hole section near the bottom of the borehole. Although most focal plane mechanisms were poorly constrained due to the very small size of the induced earthquakes, several different clusters of microearthquakes with distinct mechanisms were defined. Most of the microearthquakes for which focal plane mechanisms were determined were strike-slip events with a NNW trending P axis, essentially parallel to the direction of maximum horizontal compression observed in the borehole. The largest induced earthquake, M 1.2, occurred 18 hours after injection was started. This event was a strike-slip/reverse faulting event which also had a NNW trending P axis. Utilization of a precise relative location technique indicates that many of microearthquakes occurred relatively far (50–100 m) from the well bore. Modeling of the pore pressure disturbance caused by injection suggests that many of the earthquakes were induced by extremely small pore pressure perturbations (〈1 MPa) less than 1% greater than the ambient, approximately hydrostatic pore pressure at depth. Thus it is apparent that there are critically stressed, permeable fault zones in the crust, even at great depth and temperature. A frictional analysis of the focal plane mechanisms of the induced microearthquakes indicates that fault slip is consistent with the stress magnitudes and orientations determined in situ at depths to 7.7 km in the borehole and relatively high coefficients of friction (∼0.6–0.7) reported by Brudy et al. [this issue]. This and the observation that very small pore pressure perturbations were able to trigger seismicity appear to confirm the hypothesis that “Byerlee's law” (i.e., that differential stresses in situ are limited by the frictional strength of well-oriented, preexisting faults) is valid to great crustal depth and that the crust is in brittle failure equilibrium at depths and temperatures approaching the brittle-ductile transition, even in this relatively stable intraplate area.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 14
    Publication Date: 2020-02-12
    Language: English
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  • 15
    Publication Date: 2020-02-12
    Description: For many years, in situ stress in the brittle crust has been measured at relatively shallow depth and related to the mechanical behavior of the crust as inferred from laboratory studies and faulting theory. A continuous profile of the magnitudes and orientations of the three principal stresses has been estimated to depths of 7.7 km and 8.6 km in the German Continental Deep Drilling Program (KTB). This was achieved by hydraulic fracturing tests at relatively shallow depth (1–3 km), estimates of the magnitude of the least horizontal principal stress provided by modified hydraulic fracturing experiments at 6 km and 9 km depths, and analysis of compressional (breakouts) and tensile (drilling-induced tensile wall fractures) failures of the borehole wall over nearly the entire depth of the KTB borehole. The orientation of the maximum horizontal principal stress was found to be uniform with depth with an orientation of N160°±10°E, which is consistent with the average orientation found throughout western Europe. The only significant change in stress orientation was observed directly below a major fault zone crosscutting the borehole. The profile of stress magnitudes we have obtained demonstrates that to a depth of 8 km, the state of stress in the brittle crust in southern Germany is in frictional equilibrium. That is, the ratio of shear to normal stress as resolved on preexisting faults which are well-oriented to the in situ stress field is comparable to their frictional strength based on predictions of Coulomb faulting theory for a coefficient of friction of about 0.7 and near-hydrostatic pore pressure.
    Language: English
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  • 16
    Publication Date: 2021-08-09
    Language: English
    Type: info:eu-repo/semantics/report
    Format: application/pdf
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  • 17
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    Chichester : Wiley | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 18
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    Chichester : Wiley | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 19
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    Hamburg : Dt. Überseeinst. | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 20
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 21
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 22
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: workingpaper , doc-type:workingPaper
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  • 23
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    Chichester : Wiley | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:600
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    Language: English
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  • 24
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: report , doc-type:report
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  • 25
    Publication Date: 2016-04-28
    Description: Five years after the Earth Summit in Rio de Janeiro, the hesitancy of developed countries is turning out to be the main impediment to implementing an effective policy for sustainable development. Alongside the further development of international environmental regimes, setting up national action plans is necessary to close the action-gap in the North. However, this can only succeed if the action plans include binding objectives that can be monitored and evaluated. Current national strategies for sustainable development only meet this criterion in exceptional cases; in most cases only qualitatively and legally nonbinding objectives are included. In the present paper, a suggestion for a cluster of environmental policy targets is put forth, which - using Germany as an example - establishes the sustainability concept at the national level. Particular emphasis is placed on the normative dimension of target setting.
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 26
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    Milano : Nagard | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 27
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    Washington : World Resources Inst. | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 28
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    Berlin : Wissenschaftszentrum Berlin für Sozialforschung | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 29
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    Bonn : Federal Ministry for the Environment, Nature Protection and Nuclear Safety | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-03-26
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 30
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-11-21
    Description: The issue or concept of "sustainable development" entered onto the public and political agenda only relatively recently, and, five years after signing Agenda 21, perceptions of it are still ambiguous. A review of organisational adjustments and of German communications to the United Nations Commission on Sustainable Development shows that the German government's level of commitment to Agenda 21 is still low. This view is supported by an assessment of developments, and the Government's poor performance so far, in three institutional indicators. However, there is evidence that some incremental steps towards a sustainability transition are being taken as in some areas of business and industry and local government attitudes are begining to change. In addition, awareness of sustainable development is being raised by the efforts of non‐governmental organisations and the scientific community. Generally though, the lack of institutional reorganisation is the major obstacle to a German sustainability transition. This is an expression of the generally low priority of environmental and global development issues in the aftermath of German unification and the related economic and social problems. The traditional economic paradigm where economic growth is believed to be the precondition for welfare prevails and is considered by a majority of decision‐makers not to be compatible with the sustainability transition.
    Keywords: ddc:320
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  • 31
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    Cheltenham : Elsevier | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:330
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    Language: English
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  • 32
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    Bonn : Federal Ministry for the Environment, Nature Protection and Nuclear Safety | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
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  • 33
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:380
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  • 34
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    Oslo : ProSus | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-03-26
    Keywords: ddc:320
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  • 35
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
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  • 36
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
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  • 37
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
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  • 38
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    Cheltenham : Elgar | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-04-12
    Keywords: ddc:320
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  • 39
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    Kiel : Inst. für die Pädagogik der Naturwissenschaften | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
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  • 40
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
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  • 41
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-03-26
    Keywords: ddc:320
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  • 42
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    Oslo : Scandinavian Univ. Press | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-03-26
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  • 43
    Publication Date: 2018-03-26
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  • 44
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    [S. l.] : Environment Agency of Japan | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
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  • 45
    Publication Date: 2018-11-19
    Keywords: ddc:300
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  • 46
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2022-02-18
    Description: This paper takes a look at the development of freight transport and its further perspectives in the light of environmental sustainability. It clearly challenges the traditional view that further growth in freight transport is indispensable whatever stage of economic development an individual economy has achieved. Moreover it suggests measures to be taken into consideration in sectors other than the transport sector which may help to break the trend of continuing freight transport growth. Current developments of freight transport volume and modal split are rather counterproductive as regards curbing the unwanted environmental impacts. As growth in volume is a major contributing factor for most adverse effects caused, a substantial decoupling of economic growth and freight transport would be extremely helpful. While freight transport activity is almost entirely derived demand there can be no sufficient solution for the resulting environmental problems within the sector itself. Therefore, it is necessary to examine potentials for reducing demand for freight transport in all sectors of the economy. Contrasting to the widely held view that freight transport is in general an inevitable prerequisite of economic development, there are potentials for reducing the freight intensity of the economy which could be far more exploited. Such potentials are increasing the share of regional production, slowing down the metabolism of materials in the economy, and substituting transfer of information for transport of physical products. While each of these potentials on its own may appear to offer limited effects, a proper combination might yield substantial results. The presented preliminary ideas suggest that the notion of everlasting freight transport growth is misleading and hint at the necessity for further research.
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: workingpaper , doc-type:workingPaper
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  • 47
    facet.materialart.
    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: Contents ; List of Contributors ; Introduction ; I. General Problems of Sponge Biology. S. M. Efremova: Once more on the position among Metazoa - Gastrulation and germinal layers of sponges ; N. N. Marfenin: Sponges viewed in the light of up-to-date conception on coloniality ; A. V. Ereskovsky & G. P. Korotkova: The reasons of sponge sexual morphogenesis peculiarities II. Developmental Biology of Sponges. O. M. Ivanova-Kazas: Analysis of the sponges ontogeny at sexual reproduction ; R. P. Anakina: The cleavage specifity in embryos of the Barents Sea sponge Leucosolenia complicata Montagu (Calcispongiae, Calcaronea) ; L. V. Ivanova: New data about morphology and metamorphosis of the spongillid larvae (Porifera, Spongillidae). 1. Morphology of the free-swimming larvae ; L. V. Ivanova: New data about morphology and metamorphosis of the spongillid larvae (Porifera, Spongillidae). 2. The metamorphosis of the spongillid larvae ; L. V. Ivanova & V. V. Semenov: Feeding habits of the larvae of sponges ; N. A. Sizova & A. V. Ereskovsky: Ultrastructural peculiarities of the early embryogenesis in a White Sea sponge Halisarca dujardini (Demospongiae, Dendroceratida) ; III. Ecology of Sponges. R. P. Anakina & E. I. Slepian: Spiculas' malformations of freshwater sponges as indicators of water environment in St. Petersburg City ; A. S. Plotkin & A. V. Ereskovsky: Ecological aspects of asexual reproduction of the White Sea sponge Polymastia mammillaris (Demospongiae, Tetractinomorpha) in Kandalaksha Bay ; I. S. Smirnov & V. M. Koltun: Symbiosis of the antarctic sponge genus lophon (Porifera) and ophiuroid genus Ophiurolepis (Ophiuroidea, Echinodermata) ; IV. Palaeontology and Systematics. L. V. Bolshakova: Stromatoporoids - the fossil sponges ; E. V. Veinberg, 0. M. Khlystov, S. S. Vorobyova, E. G. Kornakova, 0. V. Levina, S. M. Efremova, & M. A. Grachev: Distribution of sponge spicules in sediments of the underwater Akademichesky ridge of Lake Baikal ; K. R. Tabachnik & C. Levi: Amphidiscophoran Hexasterophora (Part I & II) ;
    Description: conference
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Porifera ; Paläobiologie
    Language: English
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  • 48
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: At the beginning of Late Jurassic both the Lochen (LA) and the Cracow areas (CA) were palaeotopographic highs in an epicontinental basin located at the stable northern margin of the Tethyan Ocean. The topographically high position of the LA was probably caused by intensive carbonate production which proceeded on a small sea-floor bulge located close to the boundary between middle and lower parts of the low-angle carbonate ramp. Lack of deep structural control of this rise caused prograding facial unification during the Oxfordian and Kimmeridgian and led to gradual disappearance of the LA individuality in relation to the neighbouring areas. The topographical high of the CA resulted from anomalously low subsidence rate in comparison to the adjacent areas which has lasted at least for the whole Oxfordian. Low subsidence directly gave rise to the development of a barrier (so-called Cracovian Platform) which separated the interior basin in the north from the deeper parts of the basin in the south. Topography of the Polish part of epicontinental basin along the Czestochowa-Cracow line corresponds to the low-gradient rimmed carbonate shelf which graded laterally (to the northeast and east) into the low-angle carbonate ramp. Stratigraphic subdivision of Upper Jurassic strata is very precise in the LA and rather poor in the CA due to scarcity of ammonites in the massive facies which predominates in the latter area. However, ammonite fauna from both areas belongs to the same German-Polish Submediterranean Subprovince which allows to attempt the correlation of lithologies and determination of factors which controlled deposition. Both the studied areas show distinct differences in the development of carbonate buildups. In the LA the main components of carbonate buildups during whole Oxfordian and the Early Kimmeridgian were siliceous sponges and microbolites whilst in the CA the flourishing growth of microbolites and gradual decline of siliceous sponges domination took place during the Late Oxfordian. The sediment was initially diversified into the two varieties: that formed by siliceous sponges and the microbolites incipient rigid framework, and the soft mud. In such carbonate buildups stromatactis cavities might have developed even in early diagenesis due to internal erosion of the soft mud. The principal reason of the internal erosion was turbulent water flow through the sediment. However, in generally low-energy sedimentary environments such flow could be triggered by submarine gravity flows or strong bottom currents. Pseudonodular textures encountered in carbonate buildups in both the areas resulted from shallow-burial diagenesis. During the burial diagenesis some parts of the sediment has been disintegrated under the pressure of overlying strata owing to the existing open spaces and different susceptibility to compaction showed by the incipient rigid framework and the soft sediment. Deposition in the LA was controlled mainly by sea-level pulses and ecological factors. In the CA principal control was provided by subsidence rate supported by synsedimentary tectonics, sea-level changes and ecological factors. All these controlling factors were variable in time which provoked changes in carbonate production rates from intensive, aggradational growth of the buildups to drowning of the carbonate ramp and rimmed shelf. The drowning of carbonate ramp on which the LA was located took place at the Oxfordian/Kimmeridgian break. It is documented by spectacular development of redeposited pelagites of skeletal-calciturbidites type with abundant fragments of Saccocoma sp. which have appeared for the first time in mass quantities in the Upper Jurassic. By analogy, it can be inferred that in the CA similar Saccocoma-calciturbidites prove the drowning of rimmed shelf related to the same trangressive event at the Oxfordian/Kimmeridgian break.
    Description: Zu Beginn des Ober-Jura waren das Lochengebiet (Schwäbische Alb) und der Raum Krakau (Südpolen) übereinstimmend Hochgebiete eines epikontinentalen Beckens auf dem passiven nördlichen Schelf der Tethys. Die topographische Hochposition des Lochengebietes war vermutlich durch eine hohe Karbonat-Produktion bedingt, welche auf einer schmalen submarinen Schwelle nahe dem Übergangsbereich zwischen unterem und mittlerem Abschnitt einer flach geneigten Karbonatrampe erfolgte. Während des Oxfordiums und Kimmeridgiums war die Lochenschwelle tektonisch inaktiv und ermöglichte einen zunehmenden Faziesausgleich mit den benachbarten Gebieten und führte dadurch zu einer successiven Aufgabe ihrer individuellen Entwicklung. Die Hochposition der Krakau-Region resultierte aus ihrer im Vergleich zur Umgebung ungewöhnlich geringen Subsidenzrate, welche mindestens während des gesamten Oxfordiums anhielt. Die geringe Subsidenz war unmittelbare Ursache für die Entwicklung einer Barriere (die sogenannte Krakau-Plattform), welche das seichtere Innenschelf-Becken im Norden von den tieferen Beckenanteilen im Süden trennte. Die Topographie des polnischen Anteils dieses epikontinentalen Beckens entsprach entlang der Czestochowa-Krakau-Linie einem „low-gradient rimmed carbonate shelf, der nach Nordosten und Osten lateral in eine flache Karbonatrampe überging. Die stratigraphische Gliederungsmöglichkeit der Ober-Jura-Schichfolge ist im Lochengebiet gut und feinauflösend, in der Krakau-Region dagegen, in der die Massenfazies vorherrscht, aufgrund der selteneren Ammonitenfunde zum Teil problematisch. Ungeachtet dessen, gehören die Ammoniten-Vergesellschaftungen beider Regionen derselben deutsch-polnischen, submediterranen Faunensubprovinz an und ermutigen zu einer Korrelation beider lithologischer Abfolgen und einer vergleichenden Abstraktion der Steuermechanismen für die Sedimentation. Beide Gebiete zeigen deutliche Unterschiede in der Entwicklung von karbonatischen Buildups. Im Lochen-Gebiet stellen während des Oxfordiums und Unter-Kimmeridgiums Kieselschwämme und Mikrobolithe die Hauptkomponenten der Riffstrukturen, während in der Krakau-Region die Bedeutung der Mikrobolithe und Kieselschwämme während des Ober-Oxfordiums successive abnimmt. Ursprünglich erfolgte eine Differenzierung der Riffstrukturen in einen autochthonen Hartsubstrat-Anteil, in dem Kieselschwämme und Mikrobolithe eine rigides Gerüst stellten, und in schlammiges Weichsubstrat. Innerhalb der Riffkörper konnten sich wohl frühdiagenetisch durch die interne Erosion der Schlamm-Anteile Stromatactis-Gefüge bilden. Grundsätzlich kann eine solche interne Erosion auf turbulente Porenwasserströme zurückgeführt werden. In den vorliegenden sedimentären Stillwasser-Milieus könnte ein solcher Porenwasserstrom durch submarine Schuttströme oder starke Bodenströmungen ausgelöst worden sein. Pseudonodulare Strukturen, wie sie in den Buildups beider Untersuchungsgebiete angetroffen wurden, werden durch eine flache Versenkungsdiagenese erklärt. Während dieser Vorgänge wurden unter dem Druck der Sedimentauflast aufgrund des vorhandenen, offenen Porenraumes und der unterschiedlichen Kompaktion von primär zementierten Riffkalken und des mergeligen Weichsubstrates Karbonatanteile gelöst. Das Sedimentationsgeschehen wurde in der Lochen-Region vor allem durch Meeresspiegel-Schwankungen und ökologische Parameter beeinflußt. In der Krakau-Region konnte als hauptsächlicher Kontrollfaktor die Subsidenzrate erkannt werden, in deren Gefolge synsedimentäre Tektonik, Änderungen von Meeresspiegel und der ökologischen Faktoren einhergingen. Veränderungen dieser Steuerfaktoren in der Zeit beeinflußten jeweils die Rate der Karbonatproduktion von intensiv (Aggradation der Buildups) bis zum Ertrinken der Karbonatrampe bzw. des Schelfrandes. Das Abtauchen der Karbonatrampe setzte in der Lochen-Region an der Oxfordium-Kimmeridgium-Wende ein. Es wird durch eine auffällige sedimentäre Entwicklung dokumentiert: Resedimentation pelagischer Kalke (skeletal calciturbidites), die häufig Saccocoma-Reste enthalten. Erste Massenvorkommen von Saccocoma treten in der Erdgeschichte im Oberjura auf. Ähnliche Saccoco/na-Kalkturbidite an der Oxfordium-Kimmeridgium-Grenze markieren in der Krakau-Region das Abtauchen des „rimmed shelf. Sie können auf dasselbe transgressive Ereignis zurückgeführt werden.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; ddc:554 ; Paläobiologie
    Language: English
    Type: doc-type:book
    Format: 116
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  • 49
    Publication Date: 2024-04-17
    Description: The present study considered calcareous nannofossils from material represented by outcrops of Flysch successions of the External Hellenides belt in the area of the Ionian Zone (I.Z.), northwestern Greece. The studied outcrops are located in Epirus mainland and the Ionian island Korfu. Three subdivisions have been traditionally in literature distinguished in the I.Z., the Internal, Middle and External (moving from east to the west), each of which was subsequently recognized in the Flysch deposits as well. Aim of the study was, a refinement of the current biostratigraphic resolution of the area through detailed taxonomic descriptions and consequently, a reliably better correlation of the investigated sedimentary deposits with the help of calcareous nannofossils. The biostratigraphic data were also processed semiquentitatively (frequency variations and distributions), in order to accurately determine important biohorizons. For this purpose, the nannofossils were studied under the LM and the SEM, from ten closely sampled sections representing clastic sequences of all the three subdivisions of the I.Z. The investigated sections are situated at about 39° northern mid latitudes, a fact which resulted to mixed nannoflora assemblages of low and high latitudes character. The sections are namely: Elatos, Korfovouni (Internal I.Z. subdivision), Kato Despotiko, Strouga Goumenou and Ekklisia (Middle I.Z. subdivision), lower and upper Argyrotopos, National Road, Monos and Anacharavi (External I.Z. subdivision). They were found to range in age from the latest Eocene to the Early Miocene. Based on the systematic palaeontology, 107 species of calcareous nannofossils were observed and documented in the studied material. Among them, a new species Rhabdosphaera epirotica sp. nov. was described, and four recombinations were proposed. Moreover, two calcareous dinoflagellate cysts, Cervisiella saxea and Obliquipithonella sp. were reported for the first time from the I.Z. in Greece. Despite the mid latitude palaeogeographic position of the sections, all the conventional calcareous nannofossil zonal markers for the Oligocene and Early Miocene were recorded, although some in fewer abundances than in low latitudes. Improving the biostratigraphic reliability, a new zonational scheme was here developed and proposed for the Oligocene to Early Miocene interval. It was mainly established on use of redefined biohorizons and composed of five zones and five subzones following below: 1. Latest Eocene: Ericsonia formosa Partial-range Zone, 2. Oligocene: llselithina fusa / Ericsonia formosa Concurrent-range Zone, Ericsonia formosa-Reticulofenestra umbilicus/R. hillae Interval Zone, Cyclicargolithus abisectus Partial-range Zone, including the subzones: Rhabdosphaera spp. Interval Subzone, and Sphenolithus predistentus Interval Subzone, Reticulofenestra scissura Interval Zone, including the Sphenolithus delphix Abundance Subzone, and 3. Earliest Miocene: Triquetrorhabdulus spp. Partial-range Subzone Sphenolithus conicus Interval Subzone. Based on a new biohorizon of the absolute First Occurrence (FO) of llselithina fusa, the Eocene/Oligocene (E/O) boundary was identified in the lower part of the Argyrotopos section. On the absence of disc-shaped discoasters, the I. fusa biohorizon represented a better approximation of the boundary, which was clearly correlated with the other studied sections of the three subdivisions of the I.Z. The Oligocene/Miocene (O/M) boundary was identified in the Monos section located in the Plataria syncline (External I.Z.), but Early Miocene strata were recorded in the Middle I.Z. as well. This boundary was placed at the Last Common Occurrence (LCO) biohorizon of the Reticulofenestra scissura. Moreover, six associate bioevents were reported near the O/M boundary, among them the highest occurrence of I. fusa, located above the boundary, in the Anacharavi section of Korfu island (western part of the External I.Z.). For the first time were evaluated reworked together with „autochton“ taxa of calcareous nannofossils in Greece. Maximum diversity values along each of the studied sections, have shown increased reworking and erosional processes in the Internal subdivision of the I.Z. than in the Middle and the External ones. This is interpreted to be connected with the higher tectonic instability along the Pindos thrust to the east, in relation to the central and western parts of the Ionian basin mainly during the Oligocene.
    Description: Die der vorliegenden Arbeit zugrundeliegenden kalkigen Nannofossilien stammen von Flyschabfolgen der Externen Helleniden (Ionische Zone) Nordwest-Griechenlands.So wurden in die Untersuchung Aufschlüsse des Festlandes in Epirus und der Ionischen Insel Korfu aus dem stratigraphischen Intervall vom obersten Eozän bis zum untersten Miozän einbezogen. Die Ionische Zone (I.Z.) wird traditionell von Osten nach Westen in die Interne, Mittlere und Externe Subzone unterteilt. Diese Einteilung läßt sich auch auf die Flyschablagerungen übertragen. Ziel der Arbeit ist eine Verfeinerung der bestehenden Biostratigraphie durch detaillierte taxonomische Beschreibungen, um damit eine bessere Korrelation der untersuchten Ablagerungen mit Hilfe der kalkigen Nannofossilien zu erreichen. Mit einer halbquantitativen Erfassung der biostratigraphischen Daten (Häufigkeitsvariation und -Verteilung) gelingt es darüberhinaus, einzelne Biohorizonte genauer zu definieren. Zu diesem Zwecke wurde das kalkige Nannoplankton von zehn eng-beprobten Profilen aus klastischen Abfolgen aller drei Subzonen der I. Z. unter dem Licht- und Elektronenmikroskop (REM) untersucht. Die Profile im einzelnen sind: Elatos und Korfovouni (Interne Subzone), Kato Despotiko, Strouga Goumenou und Ekklisia (Mittlere Subzone), Unter bzw. Ober Argyrotopos, National Road, Monos und Anacharavi (Externe Subzone). Zur Ablagerungszeit befanden sich die untersuchten Profile in einer nördlichen Paläobreite um 39°, was zu einer gemischten Nannoflora aus charakteristischen Vertretern niedriger und höherer Breiten führte. In dem untersuchten Material konnten insgesamt 107 Spezies von kalkigem Nannoplankton gefunden und dokumentiert werden. Die Art Rhabdosphaera epirotica nov. sp.wird neu beschrieben und vier Rekombinationen werden vorgeschlagen. Darüberhinaus konnten zwei kalkige Dinoflagellatenzysten Cervisiella saxea und Obliquipithonella sp. zum ersten Mal in der I.Z. nachgewiesen werden. Trotz der paläogeographischen Position der Profile in mittleren Paläobreitenbereich konnten alle konventionellen Zonenleitformen des kalkigen Nannoplanktons für das Oligozän und das Untermiozän gefunden werden, einige davon jedoch in geringerer Häufigkeit als in den niedrigeren Breiten. Durch die Verbesserung der biostratigraphischen Genauigkeit wird hier ein neues mediterranes Zonenschema für das Oligozän und das Untermiozän entwickelt, das im wesentlichen auf neu definierten Biohorizonten basiert. Es enthält fünf Zonen und fünf Subzonen: 1. Jüngstes Eozän: Ericsonia formosa Partial-range Zone, 2. Oligozän: llselithina fusa/Ericsonia formosa Concurrent-range Zone, Ericsonia formosa-Reticulofenestra umbilicus/R. hillae Interval Zone, Cyclicargolithus abisectus Partial-range Zone, gegliedert in den Subzonen: Rhabdosphaera spp. Interval Subzone, und Sphenolithus predistentus Interval Subzone, Reticulofenestra scissura Interval Zone, die eine Subzone enthält: Sphenolithus delphix Abundance Subzone, und 3. Ältestes Miozän: Triquetrorhabdulus spp. Partial-range Subzone Sphenolithus conicus Interval Subzone. Mit dem ersten Auftreten (FO) von llselithina fusa wird ein neuer Biohorizont definiert, mit dem die Grenze Eozän/Oligozän (E/O) in dem unteren Teil des Argyrotopos-Profils nachgewiesen wird. Trotz der Abwesenheit von scheibenförmigen Discoasteriden läßt sich nun diese Grenze mit dem I. fusa-Biohorizont besser fassen und kann eindeutig mit den Profilen in den beiden anderen Subzonen der I.Z. korreliert werden. Die Oligozän/Miozän-Grenze (O/M) konnte im Monos-Profil der Plataria-Synklinale (Externe I.Z.) charakterisiert werden. Untermiozän ließ sich aber auch in der Mittleren Subzone nachweisen. Die Grenze O/M ist durch das letzte Vorkommen (LCO) von Reticulofenestra scissura bestimmt. Sechs assoziierte Bioevents fallen in diesen Grenzbereich, darunter im Anacharavi-Profil der Insel Korfu (Westteil der Externen Subzone) das jüngste Vorkommen von I. fusa, unmittelbar über der Grenze O/M. Zum erstem Mal für Griechenland konnten aufgearbeitete Taxa von kalkigen Nannofossilien zusammen mit den autochthonen Taxa nachgewiesen werden. Ein Vergleich der maximalen Diversitätswerte in den untersuchten Profilen zeigt eine signifikant höhere Aufarbeitungsrate in der Internen Subzone gegenüber der Mittleren und Externen Subzonen. Dieser Umstand dürfte mit der höheren tektonischen Instabilität entlang der Pindos-Decken-Front im Osten des Arbeitsgebietes Zusammenhängen.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Tertiär ; Flysch ; Nannofossil ; Biostratigraphie ; Systematik ; Paläobiologie ; Paläontologie
    Language: English
    Type: doc-type:book
    Format: 206
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  • 50
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, Freie Universität Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-02-14
    Description: Die Geologie des Arbeitsgebietes Derudeb ist mit Methoden der Fernerkundung und Geo- Informationssystemen auf der Grundlage einer begrenzten Datenbasis untersucht worden. Als Ergebnis wurde ein geologisches Kartenblatt im Maßstab 1 : 250 000 erstellt. Das Gebiet der südlichen Red Sea Hills, im NE des Sudan gelegen, bildet den nubischen Teil des Arabisch-Nubischen Schildes.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:556 ; ddc:550.285 ; Sudan ; GIS ; Spektralmessungen ; spectral analysis
    Language: English
    Type: doc-type:book
    Format: 122
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  • 51
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    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-05-06
    Description: Klaus Bandel & Thorsten Kowalke: Systematic value of the larval shell of fossil and modern Vanikoridae, Pickworthiidae and the genus Fossarus (Caenogastropoda, Mollusca) … 3 ; R. Thomas Becker: Eine neue und älteste Glatziella (Clymeniida) aus dem höheren Oberdevon des Nordsauerlandes (Rheinisches Schiefergebirge) … 31 ; Glenn G. Rechner: Eine Dinoflagellaten-Zysten-Vergesellschaftung des tieferen Rupelium (Unter-Oligozän) aus transgressiven Ablagerungen nördlich von Altenhausen in Sachsen-Anhalt (Blatt 3733, Erxleben) … 43 ; Joachim Gründel: Zur Kenntis einiger Gastropoden-Gattungen aus dem französischen Jura und allgemeine Bemerkungen zur Gastropodenfauna aus dem Dogger Mittel- und Westeuropas … 69 ; Joachim Gründel: Heterostropha (Gastropoda) aus dem Dogger Norddeutschlands und Nordpolens. I. Mathildoidea (Mathildidae) … 131 ; Joachim Gründel: Heterostropha (Gastropoda) aus dem Dogger Norddeutschlands und Nordpolens. III. Opisthobranchia … 177 ; C. M. Hampton & J. E. Rae: Genesis of the fossiliferous Pleistocene Hima Limestone, western Uganda, as indicated by its isotopic composition … 225 ; Helmut Keupp: Anomal kiellose Hildoceratidae (= „Subfamilie Monestierinae SAPUNOV 1965“): Ursache taxonomischer Konfusionen (Ammonoidea, Toarcium) … 233 ; Helmut Keupp: Paläopathologische Analyse einer „Population“ von Dactylioceras athleticum (SIMPSON) aus dem Unter-Toarcium von Schlaifhausen/Oberfranken … 243 ; Rolf Kohring: Eischalen neognather Vögel aus dem mitteleozänen Geiseltal (Deutschland) … 269 ; Rolf Kohring: Eggshell Structure as Evidence in Avian Systematics - Preliminary Results … 281 ; Jürgen Kriwet: Beitrag zur Kenntnis der Fischfauna des Oberjura (unteres Kimmeridgium) der Kohlengrube Guimarota bei Leiria, Mittel-Portugal: 2. Neoselachii (Pisces, Elasmobranchii) ... 293 ; Thomas Schlüter: Validity of the Paratrichoptera - an extinct Insect Order related to the Mecoptera, Diptera, Trichoptera or Lepidoptera? Suggestions based on discoveries in the Upper Triassic Molteno Formation of South Africa … 303 ; Rolf Kohring: Bibliographie 1996, Institut für Paläontologie, Freie Universität Berlin … 313 ;
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläobiologie ; Paläontologie
    Language: German , English
    Type: doc-type:book
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  • 52
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-244
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 141 S. : Abb., graph. Darst., Diagr. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 244
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 53
    Monograph available for loan
    Monograph available for loan
    Köln : Inst. für Geophysik und Meteorologie
    Associated volumes
    Call number: ZSP-560-120
    In: Mitteilungen aus dem Institut für Geophysik und Meteorologie der Universität zu Köln
    Type of Medium: Monograph available for loan
    Pages: 172 S. : Abb. ; 21 cm
    ISSN: 0069-5882
    Series Statement: Mitteilungen aus dem Institut für Geophysik und Meteorologie der Universität zu Köln 120
    Language: English
    Branch Library: GFZ Library
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  • 54
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-237
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 197 S. : graph. Darst. Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 237
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 55
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: AWI A5-98-0026
    Description / Table of Contents: Dr Houghton has revised the acclaimed first edition of The Physics of Atmospheres in order to bring this important textbook completely up-to-date. Several factors have led to vigorous growth in the atmospheric sciences, particularly the availability of powerful computers for detailed modelling, the investigation of the atmospheres of other planets, and techniques of remote sensing. The author describes the physical processes governing the structure and circulation of the atmosphere. Simple physical models are constructed by applying the principles of classical thermodynamics, radiative transfer and fluid mechanics, together with analytic and numerical techniques. These models are applied to real planetary atmospheres. This new edition is essential for undergraduates or graduate students studying atmospheric physics, climatology or meteorology, as well as planetary scientists with an interest in atmospheres.
    Type of Medium: Monograph available for loan
    Pages: XIV, 271 S. , Ill., graph. Darst
    Edition: 2nd ed., reprint.
    ISBN: 0521339561
    Language: English
    Note: Contents: Preface to first edition. - Preface to second edition. - Acknowledgements. - 1 Some basic ideas. - 1.1 Planetary atmospheres. - 1.2 Equilibrium temperatures. - 1.3 Hydrostatic equation. - 1.4 Adiabatic lapse rate. - 1.5 Sandström's theorem. - Problems. - 2 A radiative equilibrium model. - 2.1 Black-body radiation. - 2.2 Absorption and emission. - 2.3 Radiative equilibrium in a grey atmosphere. - 2.4 Radiative time constants. - 2.5 The greenhouse effect. - Problems. - 3 Thermodynamics. - 3.1 Entropy of dry air. - 3.2 Vertical motion of saturated air. - 3.3 The tephigram. - 3.4 Total potential energy of an air column. - 3.5 Available potential energy. - 3.6 Zonal and eddy energy. - Problems. - 4 More complex radiation transfer. - 4.1 Solar radiation: its modification by scattering. - 4.2 Absorption of solar radiation by ozone. - 4.3 Absorption by single lines. - 4.4 Transmission of an atmospheric path. - 4.5 The integral equation of transfer. - 4.6 Integration over frequency. - 4.7 Heating rate due to radiative processes. - 4.8 Cooling by carbon dioxide emission from upper stratosphere and lower mesosphere. - 4.9 Bandmodels. - 4.10 Continuum absorption. - 4.11 Global radiation budget. - Problems. - 5 The middle and upper atmospheres. - 5.1 Temperature structure. - 5.2 Diffusive separation. - 5.3 The escape of hydrogen. - 5.4 The energy balance of the thermosphere. - 5.5 Photochemical processes. - 5.6 Breakdown of thermodynamic equilibrium. - Problems. - 6 Clouds. - 6.1 Cloud formation. - 6.2 The growth of cloud particles. - 6.3 The radiative properties of clouds. - 6.4 Radiative transfer in clouds. - Problems. - 7 Dynamics. - 7.1 Total and partial derivatives. - 7.2 Equations of motion. - 7.3 The geostrophic approximation. - 7.4 Cyclostrophic motion. - 7.5 Surfaces of constant pressure. - 7.6 The thermal wind equation. - 7.7 The equation of continuity. - Problems. - 8 Atmospberic waves. - 8.1 Introduction. - 8.2 Sound waves. - 8.3 Gravity waves. - 8.4 Rossby waves. - 8.5 The vorticity equation. - 8.6 Three dimensional Rossby-type waves. - Problems. - 9 Turbulence. - 9.1 The Reynolds number. - 9.2 Reynolds stresses. - 9.3 Ekman's solution. - 9.4 The mixing-length hypothesis. - 9.5 Ekman pumping. - 9.6 The spectrum of atmospheric turbulence. - Problems. - 10 The general circulation. - 10.1 Labaratory experiments. - 10.2 A symmetric circulation. - 10.3 Inertial Instability. - 10.4 Barotropic instability. - 10.5 Baroclinic instability. - 10.6 Sloping convection. - 10.7 Energy transport. - 10.8 Transport of angular momentum. - 10.9 The general circulation of the middle atmosphere. - Problems. - 11 Numerical modelling. - 11.1 A barotropic model. - 11.2 Baroclinic models. - 11.3 Primitive equation models. - 11.4 Inclusion of orography. - 11.5 Convection. - 11.6 Moist processes. - 11.7 Radiation transfer. - 11.8 Inclusion of clouds. - 11.9 Sub grid scale processes. - 11.10 Transfer across the surface. - 11.11 Forecasting models. - 11.12 Other models. - Problems. - 12 Global observation. - 12.1 What Observations are required?. - 12.2 ConventionaJ observations. - 12.3 Remote sounding from satellites. - 12.4 Remote sounding of atmospheric temperature. - 12.5 Remote measurements of composition. - 12.6 Other remote sounding observations. - 12.7 Observations from remote platforms. - 12.8 Achieving global coverage. - Problems. - 13 Atmospheric predictability and climatic change. - 13.1 Short-term predictability. - 13.2 Variations of climate. - 13.3 Atmospheric feedback processes. - 13.4 Different kinds of predictability. - 13.5 Jupiter's Great Red Spot. - 13.6 The challenge of climate research. - Problems. - Appendices. - 1 Some useful physical constants and data on dry air. - 2 Properties of water vapour. - 3 Atmospheric composition. - 4 Relation of geopotential to geometric height. - 5 Model atmospheres (0-105 km). - 6 Mean reference atmosphere (110- 500 km). - 7 The Planck function. - 8 Solar radiation. - 9 Absorption of solar radiation by oxygen and ozone. - 10 Spectral band information. - Bibliography. - References to works cited in the text. - Answers to problems and hints to their solution. - Index.
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    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
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    Call number: ZSP-168-255
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 235 S. : Abb. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 255
    Language: English
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    Call number: AWI G5-00-0046
    In: Special paper / The Geological Society of America, 317
    Type of Medium: Series available for loan
    Pages: v, 165 Seiten , Illustrationen
    ISBN: 0-8137-2317-5
    Series Statement: Special paper / The Geological Society of America 317
    Language: English
    Note: Contents: Preface. - 1. Core OL-92 from Owens Lake: Project rationale, geologic setting, drilling procedures, and summary / G. I. Smith and J. L. Bischoff. - 2. Stratigraphy, lithologies, and sedimentary structures of Owens Lake core OL-92 / G. I. Smith. - 3. Climatic signals in clay mineralogy and grain-size variations in Owens Lake core OL-92, southeast California / K. M. Menking. - 4. Responses of sediment geochemistry to climate change in Owens Lake sediment: An 800-k.y. record of saline/fresh cycles in core OL-92 / J. L. Bischoff, J. P. Fitts, and J. A. Fitzpatrick. - 5. Movement and diffusion of pore fluids in Owens Lake sediments from core OL-92 as shown by salinity and deuterium-hydrogen ratios / I. Friedman, J. L. Bischoff, C. A. Johnson, S. W. Tyler, and J. P. Fitts. - 6. Paleomagnetism and magnetic susceptibility of Pleistocene sediments from drill hole OL-92, Owens Lake, California / J. M. Glen and R. S. Coe. - 7. Age and correlation of tephra layers, position of the Matuyama-Brunhes chron boundary, and effects of Bishop ash eruption on Owens Lake, as determined from drill hole OL-92, southeast California / A. M. Sarna-Wojcicki, C. E. Meyer, and E. Wan. - 8. A time-depth scale for Owens Lake sediments of core OL-92: Radiocarbon dates and constant mass-accumulation rate / J. L. Bischoff, T. W. Stafford, Jr., and M. Rubin. - 9. A diatom-based paleohydrologic record of climate change for the past 800 k.y. from Owens Lake, California / J. P. Bradbury. - 10. Ostracodes in Owens Lake core OL-92: Alternation of saline and freshwater forms through time / C. Carter. - 11. Paleobiotic and isotopic analysis of mollusks, fish, and plants from core OL-92: Indicators for an open or closed lake system / J. R. Firby, S. E. Sharpe, J. F. Whelan, G. R. Smith, and W. G. Spaulding. - 12. An 800,000-year pollen record from Owens Lake, California: Preliminary analyses / R. J. Litwin, D. P. Adam, N. O. Frederiksen, and W. B. Woolfenden. - 13. Synthesis of the paleoclimatic record from Owens Lake core OL-92 / G. I. Smith, J. L. Bischoff, and J. P. Bradbury. - Index.
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    Call number: ZSP-168-236 ; Mitte 48032 / Mitte
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 309 S. : graph. Darst.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 236
    Language: English
    Note: Zugl.: Braunschweig, Univ., Diss., 1996
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    Call number: ZSP-168-226
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 157, 173 S. : Ill., graph. Darst., Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 226
    Language: English
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    Call number: ZSP-168-238
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: XII, 99 S. : graph. Darst.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 238
    Language: English
    Note: Zugl.: Bremen, Univ., Diss., 1996
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    Call number: ZSP-168-248
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 210 S. : Abb. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 248
    Language: English
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    Call number: ZSP-168-222
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 153 S. : graph. Darst., Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 222
    Language: English
    Note: Zugl.: Bremen, Univ., Diss., 1996
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    Call number: AWI G3-98-0114
    Type of Medium: Monograph available for loan
    Pages: 113 S. : graph. Darst. , 30 cm
    Language: English
    Note: York, Univ., Diss., 1997
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    Call number: ZSP-168-221
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 136 S. : graph. Darst., Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 221
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer
    Associated volumes
    Call number: AWI S2-98-0194
    In: Atmospheric and oceanographic sciences library
    Type of Medium: Monograph available for loan
    Pages: IX, 279 S.
    ISBN: 079234801X
    Series Statement: Atmospheric and oceanographic sciences library 19
    Language: English
    Note: Contents: Editor's Preface. - Preface. - Chapter 1. Introduction. - 1.1 Spatial and temporal averaging in meteorological problems. - 1.2 Some information on the statistical characteristics of meteorological fields. - Chapter 2. Statistical Description of Averaged Fields. - 2.1 Statistical structure of averaged data. - 2.2 Representativeness of point measurements with respect to averaged values. - 2.3 Influence of area shape on the representativeness of a point value. - Chapter 3. The Accuracy of Averaging Discrete Data. - 3.1 The accuracy of representing average quantities by discrete data. - 3.2 Approximate evaluation of the averaging accuracy. - 3.3 Optimal averaging of discrete data. - 3.4 Accuracy of averaging the characteristics of statistical structure. - Chapter 4. Problems of Averaging Some Meteorological Fields. - 4.1 The representativeness of precipitation data. - 4.2 Accuracy of zonal averaging of air temperature. - Chapter 5. Practical Aspects of the Spatial Averaging of Meteorological Fields. - 5.1 Methods of averaging meteorological fields and numerical applications. - 5.2 A brief description of the averaging algorithms. - 5.3 Comparative accuracy of some averaging algorithms. - Conclusions. - List of Symbols. - References. - Subject Index. , Aus dem Russ. übers.
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    Call number: S 90.1032(58)
    In: Veröffentlichungen der Bayerischen Kommission für die Internationale Erdmessung der Bayerischen Akademie der Wissenschaften
    Type of Medium: Series available for loan
    Pages: 274 S.
    ISBN: 3769696212
    Series Statement: Veröffentlichungen der Bayerischen Kommission für die Internationale Erdmessung bei der Bayerischen Akademie der Wissenschaften : Astronomisch-geodätische Arbeiten 58
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: 19/M 98.0482 ; AWI S1-98-0189
    Type of Medium: Monograph available for loan
    Pages: xix, 1008 S.
    ISBN: 052155506X
    Classification:
    C.1.9.
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
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    Call number: AWI S2-98-0216
    In: Cambridge nonlinear science series, 7
    Description / Table of Contents: Deterministic chaos offers a striking explanation for irregular behaviour and anomalies in systems which do not seem to be inherently stochastic. The most direct link between chaos theory and the real world is the analysis of time series from real systems in terms of nonlinear dynamics. This book provides experimentalists with methods for processing, enhancing, and analysing measured signals using these methods; and for theorists it also demonstrates the practical applicability of mathematical results. The framework of deterministic chaos constitutes a new approach to the analysis of irregular time series. Traditionally, nonperiodic signals have been modelled by linear stochastic processes. But even very simple chaotic dynamical systems can exhibit strongly irregular time evolution without random inputs. Chaos theory offers completely new concepts and algorithms for time series analysis which can lead to a thorough understanding of the signals. The book introduces a broad choice of such concepts and methods, including phase space embeddings, nonlinear prediction and noise reduction, Lyapunov exponents, dimensions and entropies, as well as statistical tests for nonlinearity. Related topics such as chaos control, wavelet analysis, and pattern dynamics are also discussed. Applications range from high-quality, strictly deterministic laboratory data to short, noisy sequences which typically occur in medicine, biology, geophysics, and the social sciences. All the material discussed is illustrated using real experimental data. This book will be of value to any graduate student or researcher who needs to be able to analyse time series data, especially in the fields of physics, chemistry, biology, geophysics, medicine, economics, and the social sciences.
    Type of Medium: Monograph available for loan
    Pages: XVI, 304 Seiten , Illustrationen , 25 cm
    Edition: First published
    ISBN: 0-521-55144-7
    Series Statement: Cambridge nonlinear science series 7
    Language: English
    Note: Preface Acknowledgements Part S Basic topics Chapter I Introduction: Why nonlinear methods? Chapter 2 Linear tools and general considerations 2.1 Stationarity and sampling 2.2 Testing for stationarity 2.3 Linear correlations and the power spectrum 2.3.1 Stationarity and the low-frequency component in the power spectrum 2.4 Linear filters 2.5 Linear predictions Chapter 3 Phase space methods 3.1 Determinism: Uniqueness in phase space 3.2 Delay reconstruction 3.3 Finding a good embedding 3.4 Visual inspection of data 3.5 Poincare surface of section Chapter 4 Determinism and predictability 4.1 Sources of predictability 4.2 Simple nonlinear prediction algorithm 4.3 Verification of successful prediction 4.4 Probing stationarity with nonlinear predictions 4.5 Simple nonlinear noise reduction Chapter 5 Instability: Lyapunov exponents 5.1 Sensitive dependence on initial conditions 5.2 Exponential divergence 5.3 Measuring the maximal exponent from data Chapter 6 Self-similarity: Dimensions 6.1 Attractor geometry and fractals 6.2 Correlation dimension 6.3 Correlation sum from a time series 6.4 Interpretation and pitfalls 6.5 Temporal correlations, nonstationarity, and space time separation plots 6.6 Practical considerations 6.7 A useful application: Determination of the noise level Chapter 7 Using nonlinear methods when determinism is weak 7.1 Testing for nonlinearity with surrogate data 7.1.1 The null hypothesis 7.1.2 How to make surrogate data sets 7.1.3 Which statistics to use 7.1.4 What can go wrong 7.1.5 What we have learned 7.2 Nonlinear statistics for system discrimination 7.3 Extracting qualitative information from a time series Chapters Selected nonlinear phenomena 8.1 Coexistence of attractors 8.2 Transients 8.3 Intermittency 8.4 Structural stability 8.5 Bifurcations 8.6 Quasi-periodicity Part 2 Advanced topics Chapter 9 Advanced embedding methods 9.1 Embedding theorems 9.1.1 Whitney's embedding theorem 9.1.2 Takens's delay embedding theorem 9.2 The time lag 9.3 Filtered delay embeddings 9.3.1 Derivative coordinates 9.3.2 Principal component analysis 9.4 Fluctuating time intervals 9.5 Multichannel measurements 9.5.1 Equivalent variables at different positions 9.5.2 Variables with different physical meanings 9.5.3 Distributed systems 9.6 Embedding of interspike intervals Chapter 10 Chaotic data and noise 10.1 Measurement noise and dynamical noise 10.2 Effects of noise 10.3 Nonlinear noise reduction 10.3.1 Noise reduction by gradient descent 10.3.2 Local projective noise reduction 10.3.3 Implementation of locally projective noise reduction 10.3.4 How much noise is taken out? 10.3.5 Consistency tests 10.4 An application: Foetal ECG extraction Chapter ! 1 More about invariant quantities 11.1 Ergodicity and strange attractors 11.2 Lyapunov exponents II 11.2.1 The spectrum of Lyapunov exponents and invariant manifolds 11.2.2 Flows versus maps 11.2.3 Tangent space method 11.2.4 Spurious exponents 11.2.5 Almost two-dimensional flows 11.3 Dimensions II 11.3.1 Generalised dimensions, multifractals 11.3.2 Information dimension from a time series 11.4 Entropies 11.4.1 Chaos and the flow of information 11.4.2 Entropies of a static distribution 11.4.3 The Kolmogorov-Sinai entropy 11.4.4 Entropies from time series data 11.5 How things are related 11.5.1 Pesin's identity 11.5.2 Kaplan-Yorke conjecture Chapter 12 Modelling and forecasting 12.1 Stochastic models 12.1.1 Linear filter 12.1.2 Nonlinear filters 12.1.3 Markov models 12.2 Deterministic dynamics 12.3 Local methods in phase space 12.3.1 Almost model free methods 12.3.2 Local linear fits 12.4 Global nonlinear models 12.4.1 Polynomials 12.4.2 Radial basis functions 12.4.3 Afeura/ networks 12.4.4 Wfcat to do in practice 12.5 Improved cost functions 12.5.1 Overfitting and model costs 12.5.2 The errors-in-variables problem 12.6 Model verification Chapter 13 Chaos control 13.1 Unstable periodic orbits and their invariant manifolds 13.1.1 Locating periodic orbits 13.1.2 Stable/unstable manifolds from data 13.2 OGY-control and derivates 13.3 Variants of OGY-control 13.4 Delayed feedback 13.5 Chaos suppression without feedback 13.6 Tracking 13.7 Related aspects Chapter 14 Other selected topics 14.1 High dimensional chaos 14.1.1 Analysis of higher dimensional signals 14.1.2 Spatially extended systems 14.2 Analysis of spatiotemporal patterns 14.3 Multiscale or self-similar signals, wavelets 14.3.1 Dynamical origin of multiscale signals 14.3.2 Scaling laws 14.3.3 Wavelet analysis Appendix A Efficient neighbour searching Appendix B Program listings Appendix C Description of the experimental data sets References Index
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    Call number: A99-0026-28
    ISBN: 9264155783
    Language: English
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    Monograph non-lending collection
    Monograph non-lending collection
    Cambridge : Cambridge University Press
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    Call number: AWI A4-97-0466
    In: Cambridge atmospheric and space science series
    Description / Table of Contents: This book presents a comprehensive survey of the climatology and meteorology of Antarctica. As well as describing the climate which prevails in the Antarctic, the book also considers the processes by which this climate is maintained and explores links between the Antarctic and the global climate system. The first section of the book reviews the methods by which we can observe the Antarctic atmosphere and presents a synthesis of climatological measurements. In the second section, the processes whcih maintain the observed climate are considered, starting with large-scale weather systems to mesoscale and small-scale processes. The final section reviews our current knowledge of the variability of the Antarctic climate and considers changes that may occur in Antarctica as a result of 'greenhouse' warming. Throughout the book, the links between the Antarctic atmosphere and other elements of the Antarctic climate system (oceans, sea ice and ice sheets) are stressed and the processes which couple the Antarctic with the global climate system are examined. The instruments and platforms used in Antarctic climate studies are discussed (including automatic stations and international data centres), with special emphasis on the role of remote sensing from satellites and numerical modelling techniques. This volume will be of greatest interest to meteorologists and climatologists with a specialised interest in Antarctica and the Southern Ocean, but it will also appeal to researchers in Antarctic glaciology, oceanography and biology. Graduates and undergraduates studying physical geography or the earth, atmospheric and environmental sciences will find much useful background material in the book.
    Type of Medium: Monograph non-lending collection
    Pages: XI, 409 Seiten , Illustrationen
    Edition: First published
    ISBN: 0521465605 , 0-521-46560-5
    Series Statement: Cambridge atmospheric and space science series
    Language: English
    Note: Contents: Preface. - 1 Introduction. - 1.1 Physical characteristics of the Antarctic. - 1.2 A brief history of Antarctic meteorology. - 1.3 The role of the Antarctic atmosphere in the global climate system. - 2 Observations and instrumentation. - 2.1 Observing in the Antarctic. - 2.2 Instruments for meteorological measurements. - 2.3 Automatic weather stations. - 2.4 Drifting buoys. - 2.5 Surface-based remote sensing. - 2.6 Satellites, space-based observing systems and ground stations. - 2.7 The station network and communications. - 2.8 Data sets and data centres. - 3 Physical climatology. - 3.1 Radiation. - 3.2 Temperature and humidity. - 3.3 Pressure, geopotential and wind. - 3.4 Clouds and precipitation. - 3.5 Sea ice and the Southern Ocean environment. - 4 The large-scale circulation of the Antarctic atmosphere. - 4.1 Introduction. - 4.2 The heat budget. - 4.3 Atmospheric circulation and the vorticity budget. - 4.4 The water vapour budget. - 4.5 Representation of the Antarctic atmosphere in general circulation models. - 5 Synoptic-scale weather systems and fronts. - 5.1 Introduction. - 5.2 The role of depressions. - 5.3 Depressions in the Antarctic and over the Southern Ocean. - 5.4 Climatology. - 5.5 Preparation of operational analyses and forecasts. - 5.6 Future research needs. - 6 Mesoscale systems and processes. - 6.1 Local wind systems. - 6.2 Internal gravity waves. - 6.3 The atmospheric boundary layer. - 6.4 Blowing snow. - 6.5 Mesocyclones. - 7 Climate variability and change. - 7.1 Variations in the historical climate record. - 7.2 Interactions with the tropical and mid-latitude circulation. - 7.3 Future climate predictions - Antarctica in a 'greenhouse' climate. - Appendix A: A chronological list of stations that have made multi-year meteorological observations in the Antarctic and on the sub-Antarctic islands. - Appendix B: A chronological list of automatic weather stations that have been deployed in the Antarctic and on the sub-Antarctic Islands. - References. - Index.
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    Call number: ZSP-168-253
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 119 S. : Abb. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 253
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    Call number: ZSP-168-218
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: VI, 74 S. : Ill., graph. Darst.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 218
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    Call number: ZSP-168-219
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 188 S. : Ill., graph. Darst., Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 219
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    Call number: ZSP-691-1997
    In: Research in Svalbard
    Type of Medium: Series available for loan
    Pages: 182 S.
    ISBN: 8276661300
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    Call number: ZSP-168-241
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 157 S. : Abb. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 241
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Cambridge : Wiley
    Call number: AWI G1-00-0136
    Type of Medium: Monograph available for loan
    Pages: XI, 175 Seiten , Illustrationen
    ISBN: 0471967114
    Language: English
    Note: Contents Preface Acknowledgements Chapter 1. Recognition of paleosols Traces of life Soil horizons Soil structure What else could it be? Chapter 2. Alteration of paleosols after burial Burial decomposition of organic matter Burial gleization of organic matter Burial reddening of iron oxides and hydroxides Cementation of primary porosity Compaction Illitization of smectite Coalification of peat Kerogen maturation and cracking Recrystallization of carbonate Metamorphism Common patterns of alteration Chapter 3. Interpretation of paleosols Wetland paleosols of coal measures Aridland paleosols of calcareous red beds Paleosols at major geological unconformities Many influences on soils Chapter 4. Colour photographs Root traces Other biogenic traces Soil horizons Soil structures Soil microfabric Formation of paleosols Classification of paleosols Burial alteration of paleosols Chapter 5. Methods in palaeopedology Field documentation and sampling Petrographic thin sections Mineral determination by X-ray diffraction Bulk density determination Bulk chemical analysis Palaeopedology itself References Glossary Index
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    Greifswald
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    Call number: ZSP-343-4
    In: Greifswalder geowissenschaftliche Beiträge
    Type of Medium: Series available for loan
    Pages: 135 S.
    Series Statement: Greifswalder geowissenschaftliche Beiträge 4
    Language: English
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  • 78
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Oxford Univ. Press
    Call number: 21/M 97.0144 ; 9/M 96.0565
    Type of Medium: Monograph available for loan
    Pages: 568 S.
    ISBN: 0195078276
    Classification:
    Seismology
    Language: English
    Location: Reading room
    Location: Reading room
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    Branch Library: GFZ Library
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  • 79
    Monograph available for loan
    Monograph available for loan
    Libreville : ÉCOFAC Gabon
    Call number: PIK N 630-15-89133
    Type of Medium: Monograph available for loan
    Pages: V, 224 S. , zahlr. Ill.
    Edition: Première édition
    ISBN: 0963206427
    Language: English
    Location: A 18 - must be ordered
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  • 80
    facet.materialart.12
    Berlin; Heidelberg : Springer
    Call number: doi:10.1007/BFb0048731
    Description / Table of Contents: This book focuses on the experimental determination of the physical properties of silicate melts and magmas close to glass transition. Abundant new data are presented. The same type of measurement is performed on a range of melts to test the effect of composition on physical properties; and a range of different techniques are used to determine the same physical properties to illustrate the relationships between the relaxation of the melt structure and the relaxation of its physical properties. This book is of interest to experimental researchers in the discussion of data obtained from both a materials science and a geoscientific point of view.
    Type of Medium: 12
    Pages: VIII, 74 Seiten , Diagramme
    ISBN: 3540631291 , 978-3-540-63129-3 , 978-3-540-69152-5
    Series Statement: Lecture notes in earth sciences 67
    Language: English
    Note: Introduction, Pages 1-2 --- Relaxation, Pages 3-16 --- Shear Relaxation, Pages 17-32 --- Volume Relaxation, Pages 33-43 --- Enthalpy Relaxation, Pages 45-62 --- Summary, Pages 63-72
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  • 81
    Monograph available for loan
    Monograph available for loan
    Paris : Editions Technip
    Associated volumes
    Call number: M 99.0005
    In: Rock mechanics
    Type of Medium: Monograph available for loan
    Pages: XXXIII, 661 S.
    ISBN: 2710805863
    Classification:
    Petrophysics
    Language: English
    Location: Upper compact magazine
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  • 82
    Monograph available for loan
    Monograph available for loan
    Chichester : Wiley
    Associated volumes
    Call number: 17/M 99.0009
    In: Chemical analysis
    Type of Medium: Monograph available for loan
    Pages: IX, 514 S.
    ISBN: 0471974161
    ISSN: 415,00
    Series Statement: Chemical analysis 145
    Classification:
    Geochemistry
    Language: English
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  • 83
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1989-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, I-45 S.
    Series Statement: U.S. Geological Survey bulletin 1989-I
    Language: English
    Location: Lower compact magazine
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  • 84
    Call number: SR 90.0001(2094-G)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 16 S.
    ISBN: 0607885726
    Series Statement: U.S. Geological Survey bulletin 2094-G
    Language: English
    Location: Lower compact magazine
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  • 85
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(2127)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IX, 140 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 2127
    Language: English
    Location: Lower compact magazine
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  • 86
    Call number: S 99.0054(88) ; S 99.0054(88)
    In: Geologisches Jahrbuch
    Type of Medium: Series available for loan
    Pages: 269 S. + 5 Kt.-Beil., 8 Beil.
    Series Statement: Geologisches Jahrbuch : Reihe B 88
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 87
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(1574)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: VI, 328 S.
    Series Statement: U.S. Geological Survey professional paper 1574
    Language: English
    Location: Lower compact magazine
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  • 88
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(1579)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: VIII, 115 S.+ 1 pl.
    Series Statement: U.S. Geological Survey professional paper 1579
    Language: English
    Location: Lower compact magazine
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  • 89
    Call number: SR 90.0002(1422-D)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: VIII, D-115 S. + 1 pl.
    Series Statement: U.S. Geological Survey professional paper 1422-D
    Language: English
    Location: Lower compact magazine
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  • 90
    Monograph available for loan
    Monograph available for loan
    Sausalito, Calif. : Univ. Science Books
    Call number: AWI A15-05-0050 ; 16/M 07.0043
    Description / Table of Contents: Preliminary Description of Error Analysis. How to Report and Use Uncertainties. Propagation of Uncertainties. Statistical Analysis of Random Uncertainties. The Normal Distribution. Rejection of Data. Weighted Averages. Least-Squares Fitting. Covariance and Correlation. The Binomial Distribution. The Poisson Distribution. The Chi-Squared Test for a Distribution.
    Type of Medium: Monograph available for loan
    Pages: 327 S. , graph. Darst.
    Edition: 2nd ed.
    ISBN: 0935702423
    Language: English
    Note: Contents: Preface to the Second Edition. - Preface to the First Edition. - Part 1. - 1 Preliminary Description of Error Analysis. - 1.1 Errors as Uncertainties. - 1.2 Inevitability of Uncertainty. - 1.3 Importance of Knowing the Uncertainties. - 1.4 More Examples. - 1.5 Estimating Uncertainties When Reading Scales. - 1.6 Estimating Uncertainties in Repeatable Measurements. - 2. How to Report and Use Uncertainties. - 2.1 Best Estimate ± Uncertainty. - 2.2 Significant Figures. - 2.3 Discrepancy. - 2.4 Comparison of Measured and Accepted Values. - 2.5 Comparison of Two Measured Numbers. - 2.6 Checking Relationships with a Graph. - 2.7 Fractional Uncertainties. - 2.8 Significant Figures and Fractional Uncertainties. - 2.9 Multiplying Two Measured Numbers. - Problems for Chapter 2. - 3. Propagation of Uncertainties. - 3.1 Uncertainties in Direct Measurements. - 3.2 The Square-Root Rule for a Counting Experiment. - 3.3 Sums and Differences; Products and Quotients. - 3.4 Two Important Special Cases. - 3.5 Independent Uncertainties in a Sum. - 3.6 More About Independent Uncertainties. - 3.7 Arbitrary Functions of One Variable. - 3.8 Propagation Step by Step. - 3.9 Examples. - 3.10 A More Complicated Example. - 3.11 General Formula for Error Propagation. - Problems for Chapter 3. - 4. Statistical Analysis of Random Uncertainties. - 4.1 Random and Systematic Errors. - 4.2 The Mean and Standard Deviation. - 4.3 The Standard Deviation as the Uncertainty in a Single Measurement. - 4.4 The Standard Deviation of the Mean. - 4.5 Examples. - 4.6 Systematic Errors. - Problems for Chapter. - 5. The Normal Distribution. - 5.1 Histograms and Distributions. - 5.2 Limiting Distributions. - 5.3 The Normal Distribution. - 5.4 The Standard Deviation as 68% Confidence Limit. - 5.5 Justification of the Mean as Best Estimate. - 5.6 Justification of Addition in Quadrature. - 5.7 Standard Deviation of the Mean. - 5.8 Acceptability of a Measured Answer . - Problems for Chapter 5. - Part II. - 6. Rejection of Data. - 6.1 The Problem of Rejecting Data. - 6.2 Chauvenet's Criterion. - 6.3 Discussion. - Problems for Chapter 6. - 7. Weighted Averages. - 7.1 The Problem of Combining Separate Measurements. - 7.2 The Weighted Average. - 7.3 An Example. - Problems for Chapter 7. - 8. Least-Squares Fitting. - 8.1 Data That Should Fit a Straight Line. - 8.2 Calculation of the Constants A and В. - 8.3 Uncertainty in the Measurements of у. - 8.4 Uncertainty in the Constants A and В. - 8.5 An Example. - 8.6 Least-Squares Fits to Other Curves. - Problems for Chapter 8. - 9. Covariance and Correlation. - 9.1 Review of Error Propagation. - 9.2 Covariance in Error Propagation. - 9.3 Coefficient of Linear Correlation. - 9.4 Quantitative Significance of r. - 9.5 Examples. - Problems for Chapter 9. - 10. The Binomial Distribution. - 10.1 Distributions. - 10.2 Probabilities in Dice Throwing. - 10.3 Definition of the Binomial Distribution. - 10.4 Properties of the Binomial Distribution. - 10.5 The Gauss Distribution for Random Errors. - 10.6 Applications; Testing of Hypotheses. - Problems for Chapter 10. - 11. The Poisson Distribution. - 11.1 Definition of the Poisson Distribution. - 11.2 Properties of the Poisson Distribution. - 11.3 Applications. - 11.4 Subtracting a Background. - Problems for Chapter 11. - 12. The Chi-Squared Test for a Distribution. - 12.1 Introduction to Chi Squared. - 12.2 General Definition of Chi Squared. - 12.3 Degrees of Freedom and Reduced Chi Squared. - 12.4 Probabilities for Chi Squared. - 12.5 Examples. - Problems for Chapter 12. - Appendixes. - Appendix A. Normal Error Integral, I. - Appendix B. Normal Error Integral, II. - Appendix C. Probabilities for Correlation Coefficients. - Appendix D. Probabilities for Chi Squared. - Appendix E. Two Proofs Concerning Sample Standard Deviations. - Bibliography. - Answers to Quick Checks and Odd-Numbered Problems. - Index.
    Location: AWI Reading room
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  • 91
    Monograph available for loan
    Monograph available for loan
    Cape Town : Struik
    Call number: PIK N 630-15-89110
    Type of Medium: Monograph available for loan
    Pages: 536 S , zahlr. farb. Ill
    Edition: 1st publ.
    ISBN: 1868259226
    Language: English
    Location: A 18 - must be ordered
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  • 92
    Monograph available for loan
    Monograph available for loan
    Cape Town : Struik
    Call number: PIK N 630-15-89118
    Type of Medium: Monograph available for loan
    Pages: 144 S , zahlr. Ill
    Edition: 4. impr.
    ISBN: 1868253074
    Language: English
    Location: A 18 - must be ordered
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  • 93
    facet.materialart.12
    Berlin [u.a.] : Springer
    Call number: doi:10.1007/BFb0117747
    Description / Table of Contents: This book takes the reader through the complete weathering cycle, from the continents to the oceans, from the perspective of modern radiogenic isotope geochemistry. Topics include surface weathering, fluvial processes, environmental pollution, oceanography and paleoceanography, sedimentary mineral diagenesis and radiometric dating, thus bridging the gap between processes acting on the Earth today and the geological record. Extensive use is made of carefully selected case studies, both pioneering and state-of-the-art. This book enables the reader to critically assess previous work from the literature as well as encouraging already established researchers to apply the most modern isotopic approaches to their particular field of study.
    Type of Medium: 12
    Pages: XI, 217 S. , Ill., graph. Darst.
    ISBN: 3540631771 (kart.) , 978-3-540-63177-4 (Print) , 978-3-540-69208-9 (Online)
    Series Statement: Lecture notes in earth sciences 68
    Language: English
    Note: Pages 1-10, Introduction and basic principles of isotope geochemistry --- Pages 11-31, Weathering --- Pages 33-45, Isotope geochemistry of river water --- Pages 47-88, Isotope geochemistry in the environment --- Pages 89-153, Isotopic composition of seawater past and present (Sr, Nd, Pb, Os, Ce) --- Pages 155-184, Isotope geochemistry of detrital and authigenic clay minerals in marine sediments (Rb−Sr, K−Ar, O) --- Pages 185-211, The Sm−Nd isotope system in detrital and authigenic argillaceous sediments
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  • 94
    facet.materialart.12
    Berlin, Heidelberg : Springer
    Call number: doi:10.1007/BFb0009557
    Description / Table of Contents: This book, which is divided into three parts, gives a state-of-the-art report on technical developments in instrumentation and on theoretical advancements in acoustic remote sensing. It explains the utilization of acoustic techniques in studies related to the structure of the lower atmosphere and oceans and discusses various atmospheric and oceanic applications. The potential and limitations of acoustic remote sensing are also described. This book will be useful to researchers, graduate students, and teachers interested in the structure of the atmosphere and oceans.
    Type of Medium: 12
    Pages: XIII, 585 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 3540616128 (Springer, Berlin ...) , 0387616128 (Springer, New York ...) , 8173191107 (Narosa Publ. House) , 978-3-540-61612-2 (Print) , 978-3-540-70743-1 (Online)
    Series Statement: Lecture notes in earth sciences 69
    Language: English
    Note: Pages 3-34, Physical grounds for acoustic remote sensing of the atmospheric boundary layer, M. A. Kallistratova --- Pages 35-84, An overview of the technological development of atmospheric echosounders (SODARS), John A. Kleppe --- Pages 85-104, Design of a tri-monostatic doppler sodar system, Yoshiki Ito --- Pages 105-116, A modular PC-based multiband sodar system, G. Mastrantonio, S. Argentini --- Pages 117-132, Mini acoustic sounding, a powerful tool for ABL applications: Recent advances, D. N. Asimakopoulos, C. G. Helmis, M. Petrakis --- Pages 133-141, Radio-acoustic temperature profiling in the troposphere, G. Bonino --- Pages 142-176, Radio acoustic sounding system (RASS) for studying the lower atmosphere, S. P. Singal, Malti Goel --- Pages 179-190, Determination of the turbulent structure parameters, Pan Naixian --- Pages 191-201, Turbulence variables derived from sodar data, R. L. Coulter --- Pages 202-235, Development of sodar detection and its application for studies of atmospheric boundary layer in Beijing, China, Mingyu Zhou --- Pages 236-246, Influence of the nocturnal low-level-jet on the vertical and mesoscale structure of the stable boundary layer as revealed from doppler-sodar-observations, Frank Beyrich, Dieter Kalass, Ulrich Weisensee --- Pages 247-274, Dynamics of the continental boundary layer: The CRPE sodar results (1984–1993), Christine Amory-Mazaudier --- Pages 275-292, Sodar investigations of gravity waves by cross spectral analysis, Günther Bull --- Pages 293-306, Sodar monitoring of nocturnal boundary layer during the harmattan in Ile-Ife, Nigeria, J. A. Adedokun --- Pages 307-324, An overview of similarity methods to estimate turbulence quantities from sodar measurements in the convective boundary layer, Dimitrios Melas --- Pages 325-384, Sodar: A tool to characterize hazardous situations in air pollution and communication, S. P. Singal, B. S. Gera, Neeraj Saxena --- Pages 385-394, Application of sodar in urban air-quality monitoring systems, Jacek Walczewski --- Pages 395-405, Operational use of sodar information in nowcasting, Th. Foken, H.-J. Albrecht, K. Sasz, F. Vogt --- Pages 409-448, Acoustic remote sensing of ocean flows, Antony Joseph K, Ehrlich Desa --- Pages 449-475, Acoustic remote sensing of ocean-atmosphere interactions, A. Weill, H. Dupuis
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  • 95
    facet.materialart.12
    Berlin; Heidelberg : Springer
    Call number: doi:10.1007/BFb0028315
    Description / Table of Contents: This book deals with the application of fractal and nonlinear time-series analysis to seismicity and earthquakes within the framework of earthquake prediction research. Emphasis is on theoretical foundations as well as practical implementation and pitfalls to enable readers to conduct their own analyses. The theoretical parts include introductions to fractals and multifractals, the relation between fractal dimension and entropy, the Hurst phenomenon, basic ideas of low-dimensional chaotic dynamics and a roadmap of nonlinear time-series analysis. Practical implementation is discussed in each case and synthetic data sets are analyzed. Fractal methods are applied to landslide and seismicity patterns in space and time, nonlinear analysis is carried out for radon and strain data as well as earthquake intervals. Due to the comprehensive coverage of theoretical background and step-by-step applications, readers of all levels will benefit from this book.
    Type of Medium: 12
    Pages: XI, 178 Seiten , Diagramme
    ISBN: 3540648933 , 978-3-540-64893-2 , 978-3-540-68459-6
    Series Statement: Lecture notes in earth sciences 77
    Language: English
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  • 96
    Call number: MOP Per 409/C(240)
    In: Technical memorandum, 240
    Type of Medium: Series available for loan
    Pages: 42 S. : graph. Darst.
    Series Statement: Technical memorandum / European Centre for Medium Range Weather Forecasts 240
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 97
    Call number: SR 96.0498(226) ; ZSP-686-226
    In: Report
    Type of Medium: Series available for loan
    Pages: X, 61 S.
    ISSN: 0937-1060
    Series Statement: Report / Max-Planck-Institut für Meteorologie 226
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 98
    Series available for loan
    Series available for loan
    Washinton, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0003(1142)
    In: U.S. Geological Survey circular
    Type of Medium: Series available for loan
    Pages: VII, 70 S.
    Series Statement: U.S. Geological Survey circular 1142
    Classification:
    Mineralogy
    Language: English
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  • 99
    Series available for loan
    Series available for loan
    Washington, DC : Smithsonian Institution Press
    Associated volumes
    Call number: SR 90.0088(83)
    In: Smithsonian contributions to paleobiology
    Type of Medium: Series available for loan
    Pages: III, 37 S.
    Series Statement: Smithsonian contributions to paleobiology 83
    Language: English
    Location: Lower compact magazine
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  • 100
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley
    Call number: M 99.0252
    Type of Medium: Monograph available for loan
    Pages: xxii, 875 S.
    ISBN: 0471546321
    Classification:
    E.9.
    Language: English
    Location: Upper compact magazine
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