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  • English  (622)
  • 2020-2024  (5)
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  • 1985-1989  (4)
  • 1950-1954  (2)
  • 1992  (622)
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Years
Year
  • 1
    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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  • 2
    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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  • 3
    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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  • 4
  • 5
    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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  • 6
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    Geophysical Inst., Czechoslovak Acad. of Sciences
    In:  ESC-Proceedings
    Publication Date: 2020-02-12
    Language: English
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  • 7
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    Geophysical Inst., Czechoslovak Acad. of Sciences
    In:  ESC-Proceedings
    Publication Date: 2020-02-12
    Language: English
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  • 8
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-06
    Language: English
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  • 9
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-06
    Language: English
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  • 10
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-06
    Language: English
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  • 11
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-06
    Language: English
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  • 12
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-01
    Language: English
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  • 13
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-01
    Language: English
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  • 14
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Language: English
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  • 15
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: A depth migration is very sensitive to tl1e velocity model especially in the case of steeply dipping reflectors like the so-called SE reflectors at the KTB site. Velocity models derived from first breaks in vertical seismic profiling (YSP) experiments were used and compared with velocity data at the top of the crystalline refractor derived by short range measurements. Because of high picking errors, the possibility to compare seismic events with information of the upper part of the KTB HB hole allows only a very limited calibration of the velocity model. Based on the cutting profile, we assume that the reflectors SE-2 and SE--3 represent faults at 3600-3660 m depth and 5440-5560 m depth ( or a lithological contrast at 5540-5610 m depth). We suppose that the velocity of an average model starts at about 5.2 km/s at the surface, reaches a value of 6.0 km/s in about 2.5 km depth and remains approximately constant below. In that case, the reflector SE-1 will be hit at a depth of 7 .0 km. Because of the steep dip of reflector SE-1 which increases the size of the error range (from inaccurate velocity models and picking errors). the tolerance of about ±0.4 km is very high.
    Language: English
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  • 16
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: The 3-D expanding spread experiment, performed within ISO 89 at the KTB site, has been evaluated under two aspects. The first aspect was the estimation of velocity-depth functions. Due to the limited reflection strength, estimating NMO velocities as a function of twoway traveltime was possible in east-west direction only. Thus the calculation of interval velocities, requiring the correction of 3D effects, was not possible. The second aspect was the directional dependency of the P-wave velocity at the top of the crystalline by evaluating the direct waves. After eliminating the effects of the lithology, a least-mean-squares anisotropy-velocity ellipse was fitted to the data with WSW as the direction of the maximum velocity and a velocity contrast of about 6%.
    Language: English
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  • 17
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: A preliminary interpretation of the major 3-D reflectors is given by correlation with the surface geology and the drilled sections of the KTB Vorbohrung and the Hauptbohrung. Possible explanations for the reflections are discussed: lithological boundaries, cataclastic fault zones (partly filled with fluids) and other structural properties (e.g. foliation). Flat reflectors near the surface (MFl - 4) can be correlated with Permocarboniferous and Mesozoic sediments of the South German Platform. Special attention is drawn to a group of steeply NE-dipping reflectors (SEl, SE2, SE3) which are, obviously, produced by en-echelon fault structures of the Franconian Lineament. In the boreholes, SE2 can be identified as a bundle of faults near 3600 m. The calculated depth of the most prominent reflector SEl in the Hauptbohrung is between 6600 and 7100 m. It represents, probably, a deepreaching reverse fault zone which produces an offset of the reflections of the midcrustal "Erbendorf body" (B1 - B2/G4 - Gl).
    Language: English
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  • 18
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: The determination of 3D-static corrections usually is possible only with the exact knowledge of thickness and velocity of the superficial layers. In order to determine these parameters extensive additional measurements are necessary, e.g. refraction seismics. These measurements can be reduced considerably if there is already a borehole in the survey area; the shots generated for the seismic survey can be recorded with a borehole geophone chain. The direct traveltimes determined from these records are lying on a 2nd-order plane (ideally a hyperboloid). If these traveltimes are influenced by e.g. differences in the elevations of the source location or velocity inhomogeneities, the first arrival traveltimes scatter around such a hyperboloid. The static corrections can be determined from the difference between the measured traveltime and the ideal hyperboloid. Further measurements are not required, because a precise knowledge of the parameters of the weathered layer is not necessary. In the following a method is presented (developed by Albrecht (1991) and Teichert (1991)) to determine the theoretical hyperboloid. Another method, described at the end of this report, is the determination of average velocities from picked and corrected first arrival traveltimes.
    Language: English
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  • 19
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: A kinematic evaluation of first breaks of the direct P-wave in several VSPs, carried out at the KTB pilot hole in 1988 and 1989, is presented. After picking and correction to vertical traveltime, average and interval velocities were computed. The average velocity increases with depth caused by the successive closing of microcracks under increasing confining pressure. Tl1is average velocity-depth curve is the most accurate velocity information at the KTB site and can be used in migration and time-depth conversion problems in 2D- and 3D reflection surveys.
    Language: English
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  • 20
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: The recordings of the wide-angle shots by 3-component geophones in the KTB pilot hole exhibit the effect of shear-wave splitting, that is the most diagnostic evidence of seismic anisotropy (Crampin, 1989). The possible reasons for seismic anisotropy will be discussed and the lateral extension of the anisotropic region will be estimated.
    Language: English
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  • 21
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: Based on the DEKORP ISO 89 borehole experiments, the question of the existence of "seismic anisotropy at the KTB deep drilling site" has to be answered unambiguously with "yes". The anisotropy could be quantified in situ for a gneiss packet where it is apparently influenced by both rock foliation and cracks. The values obtained in the direct vicinity of the KTB pilot hole, however, cannot be extrapo l ated into its surroundings without modification: While the general trend of anisotropy with high velocity values towards SE-ESE is conserved, the amount of anisotropy shows smaller average values. This seems to reflect the inhomogeneous distribution of metamorphic rocks and granite in the target area. The direction of high seismic velocities (ESE) coincides approximately with the postulated direction of maximum horizontal tectonic stress in the Oberpfalz region.
    Language: English
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  • 22
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-05-11
    Description: The detection of permeable fractures is one of the research objectives of the KTB-project. Among seismic methods the tube wave survey is suggested for this purpose. Open permeable fractures intersecting the borehole may generate secondary tube waves which show up as V-shaped traveltime patterns (Chevron pattern) in sonograms. We investigated tube waves transmitted and recorded by the VAL-(Variable Acoustic Logging)-tool technique. The depths of tube wave generation were determined. 85 percent of them correlate with planar structures seen in acoustic borehole televiewer (BHTV) logs. BHTV data reveal many structures. One third of these coincide with tube wave events in the VAL data. To verify the hypothesis that the occurence of a structure in both, traveltime and amplitude displays of BHTV data indicates an open fracture, we compared this dataset with stronger tube wave events assuming that the latter can be correlated to open fractures. We found no evidence for the correctness of the hypothesis. We compared tube wave events with caliper logs, temperature and mud conductivity anomalies during hydraulic tests, temperature anomalies during heat exchange test, core sample observations and gas-geochemical anomalies The comparison between these various borehole data is not as satisfactory as to ensure the reliability of tube wave analysis to determine open fractures. Earlier investigations suggest that amplitudes of tube wave events are related to hydraulic permeabilities. Deficiencies of the present tube wave dataset (VAL) and missing fluid logging for calibration purposes prevents us from quantitative analysis.
    Language: English
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  • 23
    Publication Date: 2022-05-09
    Description: Dürbaum, H.-J.: Introduction. p. 1-2. Stiller, M.: Preliminary generation of a stacked data volume of the entire ISO'89-3D data set using an envelope technique. p. 3-29. Hluchy, P., Körbe, M., Thomas, R.: Preliminary Interpretation of the 3D-Seismic Survey at the KTB Location. p. 31-52. Stiller, M., Tormann, M.: Application of a simplified horizon migration process to the data of the 3D-seismics ISO'89. p. 53-65. Wiederhold, H.: Interpretation of envelope-stacked 3D seismic data and its migration - another approach. p. 67-113; Hannover. Körbe, M., Reichert, C.: On the character of "Steep Event SE-1" reflected energy, reflected refraction, diffraction or any artifact?. p. 115-131. Janik, M., Harjes, H. P.: Structural Interpretation of the MSP-Experiment. p. 133-148. DEKORP Research Group: Depth determination of prominent seismic structures beneath the KTB main drillhole KTB-HB. p. 149-160. Simon, M.: Structural images from 3D-isochron migration of wide-angle data in the surroundings of KTB. p. 161-168. Söllner, W., Lüschen, E., Li, X.-P., Hubral, P., Gut, T. W., Widmaier, M.: VSP - A Link between Reflection Seismic Profiling and Lithology. p. 169-199. Rühl, T., Hanitzsch, C.: Average and interval velocities derived from first breaks of vertical seismic profiles at the KTB pilot hole. p. 201-219. Bönnemann, C., Buttkus, B: Results of the 3-D expanding spread experiment. p. 221-232. Martini, N., Stiller, M.: Results of the ISO'89 experiment "Durchschallung": Recording of the vibrator sweeps of the 3D-seismics in the KTB borehole. p. 233-246. Lüschen, E., Werner, U.: Fluid/Gas indications in 8 km depth beneath the KTB and rock anisotropy from shear-wave reflection surveys. p. 247-274. Rabbel, W.: Seismic anisotropy at the KTB Deep Drilling Site. p. 275-289. Gut, T. W., Söllner, W., Lüschen, E., Edelmann, H. A. K.: More reliable shear-wave data from VSP by using CIPHER-technique. p. 291-295. Bopp, M: Shear-wave splitting observed by wide-angle measurement. p. 297-308. Hanitzsch, C., Rühl, T., Heinemann, B. B.: Detection of permeable fracture zones by tube waves in the KTB pilot hole. p. 309-332. Hanitzsch, C., Hubral, P., Rühl, T., Söllner, W.: Migration of steeply dipping reflectors at the KTB site: Depth errors caused by inaccurate velocity models. p. 333-341. Stettner, G.: Zur Korrelation des tektonischen Baues mit den seismischen Strukturen im Raum KTB-Oberpfalz - Münchberger Gneismasse. p. 343-349. Hirschmann, G.: On the Geological Interpretation of the 3-D Seismic Data with Special Regard to the Information from the KTB Boreholes. p. 351-373.
    Language: English , German
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  • 24
    Publication Date: 2020-02-13
    Description: Dietrich, H.-G., Lauterjung, J., Wöhrl, Th.: Introduction. p. A1-A26. Lich, S., Duyster, J., Godizart, G., Keyssner, S., de Wall, H.: German Continental Deep Drilling Program (KTB) - Geological Survey of the Hauptbohrung 0 - 6000 m. p. B1-B42. de Wall, H., Lich, S.: Drilling Artifacts in Cuttings Samples. p. B43-B46. Hirschmann, G.: The Geological Section of the KTB Hauptbohrung - Correlation with the KTB Vorbohrung and preliminary structural interpretation. p. B47-B52. WGs Geology, Geochemistry, Geophysics: Cutting Profile. p. B53-B83. Figgemeier, Chr., Machon, L., Kamm, H., Hansmann, J., Gleiß, N., Umsonst, T., Zimmer, M.: KTB Hauptbohrung, Geoscientific Investigations in the KTB-Field- Laboratory, Depth interval 0 - 6000 m: Geochemistry/Mineralogy. p. C1-C38. Erzinger, J., Hansmann, J., Kamm, H., Heinschild, H.-J.: On-line Determination of 222-Radon in Drilling Fluids of the KTB Hauptbohrung. p. C39-C45. Pribnow, D., Bücker, Ch., Rauen, A., Spangenberg, E., Wienand, J., Soffel, H.C.: KTB Hauptbohrung, Geoscientific Investigations in the KTB-Field- Laboratory, Depth interval 0 - 6000 m: Geophysics. p. D1-42. Röckel, Th., Natau, O.: KTB Main Hole, Geoscientific Investigations in the KTB-Field- Laboratory, Depth interval 0 - 6000 m: Rock Mechanics. p. E1-E7. Röckel, Th., Natau, O., Dietrich, H.-G.: Core Reorientation by Comparison of Core Instabilities and Borehole Instabilities. p. F1-F17. Rischmüller, H., Chur, C., Engeser, B., Hoffers, B., Sperber, A., Tran Viet, T., Wohlgemuth, L.: Advanced Drilling Technology for the Continental Deep Drilling Program (KTB): Part of International Lithosphere Research. p. G1-G17.
    Language: English
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  • 25
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    Schweizerbart
    In:  KTB Reports
    Publication Date: 2020-07-24
    Description: Hirschmann, G.: Vorläufige strukturelle Interpretation von KTB-Vor- und Hauptbohrung. p. 3-6. Schalkwijk, G., Stöckhert, B.: Metabasites in the pilot borehole of the KTB, structures and fabrics. p. 7-13. Pieper, U., Stöckhert, B.: Quantitative analysis of reaction fabrics in the KTB-pilot-borehole. p. 15-22. Heinisch, H.,Kohl, J.,Sprenger, W.,Zadow, A.: Kinematische Analyse von Porphyroklasten-Systemen in Gneisen der KTB-VB auf der Basis kontinuierlicher Kernaufnahme. p. 23-41. Heinicke, F.,de Wall, H.: Gefügeuntersuchungen an Paragneisen aus der KTB-Vorbohrung. p. 43-66. Vollbrecht, A.,Weber, K.: Mikrorisse und Quarz-Deformationslamellen in Paragneisen der KTB-Vorbohrung: Indikatoren für Paläospannungsrichtungen. p. 67-83. de Wall, H.,Huenges, E.,Weber, K.: Untersuchungen zur Richtungsabhängigkeit der Wärmeleitfähigkeit an Paragneisen der KTB-Vorbohrung. p. 85-99. Weber, K.: Die tektonische Position der KTB-Lokation. p. 103-132. Stein, E.,Kleemann, U.: Evidence for Late Variscan emplacement of the ZEV. p. 133-146. Bernbach, W.,Stein, E.: Die Tektonik im zentralen Teil der Zone Erbendorf-Vohenstrauss (ZEV). p. 147-159. Rohrmüller, J.,Höll, R.,Stettner, G.: Deformationsmerkmale im Umfeld der Kontinentalen Tiefbohrung (KTB) Windischeschenbach/Opf. p. 161-169. Stettner, G. (1992): Zu den tektonischen Beziehungen zwischen der Neustädter Scholle (ZEV), der Erbendorfer Grünschiefereinheit und dem Moldanubikum. p. 171-179. Röhr, C.,Zulauf, G.: Zur tektonometamorphen Entwicklung der Erbendorfer Grünschieferzone - abgeleitet aus petrologischen, geothermobarometrischen und strukturgeologischen Untersuchungen. p. 181-212. Franke, W.,Prössl, K. F.,Schwarz, J.: Devonische Grauwacken im Erbendorfer Paläozoikum - Alter, tektonische Stellung und geotektonische Bedeutung. p. 213-223. Franke, W.,Behrmann, J.,Moehrmann, H.: Zur Deformationsgeschichte des Kristallins im Münchberger Deckenstapel p. 225-240. Lapp, M.,Weber, K.: Postkinematische Alteration von Metagrauwacken und Phylliten der Bohrung Neualbenreuth p. 241-250. Stein, E.: Die Alterstellung der Arzberger Serie, abgeleitet aus der tektonischen Entwicklung des S' Saxothuringikums p. 251-260. Skrotzki, W.,Weber, K.,Müller, W. F.: Gefügekundliche Untersuchungen im KTB mittels TEM. p. 261-276. Maier, M.,Stöckhert, B.: Conditions of crystallization and deformation of the Falkenberg Granite/Eastern Bavaria, Germany. p. 277-286. Schröder, B.: Post-Hercynican fault block activities in the basement area near KTB - drilling site. p. 287-294. Franzke,H.-J.: Bruchentwicklung und hydrothermale Gangmineralisation an der Flossbergstörung bei Ilmenau/Thüringer Wald. p. 295-315. Teufel,S.,Ahrendt,H.,Hansen,B.T.: U-Pb-Isotopensystematik von Monaziten aus metamorphen Gesteinen der Oberpfalz. p. 319-331. Grauert, B.,Blümel, P.,Lork, A.: Hinweise auf prädevone und karbone Metamorphosen in Gneisen der KTB-Vorbohrung: Ergebnisse aus Rb-Sr-Kleinbereichsanalysen. p. 333-347. Wemmer, K.,Ahrendt, H.: Geochronologische Erfassung von retrograden Prozessen in Gesteinen der KTB-Vorbohrung mit Hilfe der K/Ar-Methode. p. 349-372. Welzel, B.,Ahrendt, H.,Behr, H.-J.,Schröder, B.,Weber, K.: Die Bedeutung von K/Ar-Datierungen an detritischen Muskoviten fr die Rekonstruktion tektonometamorpher Einheiten im erweiterten KTB-Lokationsgebiet. p. 373-397. Welzel, B.,Ahrendt, H.,Behr, H.-J.,Schröder, B.,Weber, K.: Alter und Intensität der postsedimentären Überprägung im erweiterten KTB-Lokationsgebiet (Ostteil der Süddeutschen Scholle). p. 399-415.
    Language: German , English
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  • 26
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    Schweizerbart
    In:  KTB Reports
    Publication Date: 2020-07-24
    Description: Behr, H.-J., Gerler, J., Große, S., Heinrichs, T., Löffler, T., Reutel, Chr., Schmidt-Mumm, A., Welzel, B.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation. p. 3-85. Gerler, J., Schmidt-Mumm, A., Behr, H.-J.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation: 1.4.2 Thermische Schallemissionsanalyse. p. 13-17. Behr, H.-J., West, M.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation: 1.4.3 Röntgen-Tomographie an Bohrkernen. p. 17. Behr, H.-J., Große, S., Heinrichs, T.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation: 2.0 Störungstektonik und Schwerefeld am Westrand der Böhmischen Masse. p. 17-19. Löffler, T.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation: 6.1 Sedimentologisch-fazielle Profilaufnahme der Thermalwasser-Bohrung Weiden. p. 47-52. Welzel, B.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation: 6.2 K/Ar- Datierungen an detritischen Muskoviten aus dem Permokarbon der Bohrung Weiden. p.52-55. Behr, H.-J., Reutel, Chr.: Lineare Krustenstrukturen im Umfeld der KTB-Lokation: 8.0 Krustenstruktur und Krustenfluide. p. 58-61. Hirschmann, G. : Das Bruchstörungsmuster im KTB-Umfeld. p. 85-124. Lich, S., Hirschmann, G.: Petrographische Bearbeitung der Weitwinkel-Schußbohrungen ISO 89. p. 127-164. Dahlheim, H.-A., Gebrande, H., Schmedes, E., Soffel, H.C.: The KTB Seismological Network. p. 167-204. Günzel, F., Soffel, H. C.: Feldmagnetische Bodenmessungen im Bereich des Amphibolitkörpers der KTB-Bohrung und ihre Interpretation. p. 207-228. Soffel, H. C., Harzer, F.: Palaeomagnetic Investigations on Permo-Carboniferous Rocks in the Area of the KTB Drill Site. p. 231-245. Worm, H.-U.: Die Anisotropie der magnetischen Suszeptibilität in der KTB-Oberpfalz VB. p. 249-261.
    Language: German , English
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  • 27
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    In:  Protokoll über das 14. Kolloquium Elektromagnetische Tiefenforschung: Borkheide, 25.05.- 29.05.1992
    Publication Date: 2022-07-20
    Language: English
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  • 28
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    In:  Protokoll über das 14. Kolloquium Elektromagnetische Tiefenforschung: Borkheide, 25.05.- 29.05.1992
    Publication Date: 2022-07-24
    Language: English
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  • 29
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    In:  Protokoll über das 14. Kolloquium Elektromagnetische Tiefenforschung: Borkheide, 25.05.- 29.05.1992
    Publication Date: 2022-07-24
    Language: English
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  • 30
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    In:  Protokoll über das 14. Kolloquium Elektromagnetische Tiefenforschung: Borkheide, 25.05.- 29.05.1992
    Publication Date: 2022-07-24
    Language: English
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  • 31
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-05
    Description: For several reasons the IS0'89 3D-seismic data are at hand not as conventional, phase-consistent stack so far but as 'envelope stack' only. Therefore, the common wave-field migration procedures cannot be applied to attain information on the spatially correct position of the particular reflector elements. To cope with this problem a simplified 3D-horizon migration program was developed at the DEKORP Processing Center Clausthal. It allows to migrate not the sejsmic traces of the IS0'89-3D survey themselves but the traveltime values for specific horizons derived by interactive picking with a 3D-seismic interpretation system on the basis of an envelope stack. The motivation, the basic assumptions and the principles of this procedure are outlined as well as the mathematical background and the particular processing steps. The migration results of some selected key horizons in the area of the KTB are depicted by isochrone maps and 3D-views. By this, a preliminary geological interpretation based upon the true position and shape of several detected seismic surfaces is enabled although the final processing, i. e. a phase-consistent stack of the entire JO-dataset (and its subsequent wave-field migration), has not been finished yet.
    Language: English
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  • 32
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-05
    Description: A preliminar)' interpretation ha, been done on an envelope tack of the three-dimen ional eismic nrW)' of the ISO 89 experiment. This kind of~ tack is interpretable as well a a normal stack with ome re tri tion . but all major elements are detectable. The major tructural elemPnt , which haw been the targPt of the interpretation in thi special case. can be diYided into five groups. The three most important groups are a bundle of steeply northeast dipping reflections with outcrops in the area of the outcrop of the Franconian Line. a zone of high refl.ectiYity with five reflections named Erbendorf body and two curved interfaces at the time range 3.5 to 4.5 s TWT. The results of this interpretation are in good correspondence to the former interpretations done on the two-dimensional seismic lines in the survey area.
    Language: English
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  • 33
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-05
    Language: English
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  • 34
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-05
    Description: The heart of the Integrated Seisrnics Oberpfalz 1989 experiment (ISO89) is a 3D seismic survey with a subsurface covered area of 19.1 km* 17.85 km and the KTB borehole at its centre. The brute processing by the DEKORP Processing Center (DPC) at Clausthal resulted in an envelope-stacked data set that is used for a preliminary interpretation. Several strong reflections are addressed and mapped in 3D. The results are presented in form of time contour maps. For the depth conversion several velocity models are discussed and compared. The depth _ conversion itself is realized by a map migration of the interpreted horizons (SATTLEGGER 1986). The true 3D geometry for several horizons is presented as well as the depth they will be encountered in the KTB borehole.
    Language: English
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  • 35
    facet.materialart.
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    In:  KTB Report 92-5: Integrated Seismics Oberpfalz 1989; Data evaluation and interpretation as of October 1992
    Publication Date: 2022-04-05
    Description: A reflection survey using shear-wave sources and 3-component receivers bas been performed on two orthogonal lines across the KTB-deep dril1ing site in the Oberpfa]z area (Bohemian crysta11ine Massif). A combination of surfaceconsistent statics and automatic residual statics proved to be of crucial importance to obtain good coherency and a good signal/noise ratio for deep crustal shear-wave reflections after CMP-stacking. Direct comparisons with previously processed standard P-wave CMP stack sections exhibit deep structures ('Erbendorf-body', 10-12 km depth) which reflect equally strong in P- and S-waves indicating normal lithological variations. In contrast to this, in 8 km depth a bright reflection is seen only on the P-wave section. It is absent on the S-wave section. This behaviour can be explained by two alternative geological models. The first one is an accumulation of fluid or gas under sti11 unknown reservoir condHions. The aJtemative, purely compositional model is a crystalline body with an anomalously low Vp!Ys-ratio. A rock mass with a high amount of quartz could also produce impedance contrasts for P-waves but not for S-waves. Pronounced S-wave splitting, observed for the 'Erbendorf-reflections, indicates that the symmetry system of the rock anisotropy is rotated by 90 degrees below 3 km against the one which was detected above 3 km by S-wave vertical seismic profiles.
    Language: English
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  • 36
    Publication Date: 2022-07-18
    Language: German , English
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  • 37
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    Deutsche Geophysikalische Gesellschaft
    Publication Date: 2024-05-22
    Language: German , English
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  • 38
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    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
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 39
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 40
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    London : Zed Books | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 41
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 42
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    London : Zed Books | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-11-19
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 43
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    Fachbereich Geowissenschaften, FU Berlin, Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-17
    Description: Prof. Dr. B. KREBS zum 60. Geburtstag. ... 3 ; Inhalt. ... 7 ; HAHN, G. & HAHN, R.: Nachweis des Septomaxillare bei Pseudobolodon krebsi n. sp. (Multituberculata) aus dem Malm Portugals. ... 9 ; BONAPARTE, J.F.: Approach to the Significance of the Late Cretaceous Mammals of South America. ... 31 ; KOENIGSWALD, W. von: Differenzierung im Zahnschmelz der Marsupialia im Vergleich zu den Verhältnissen bei den Placentalia (Mammalia). ... 45 ; STORCH, G. & MARTIN, T.: Eomanis krebsi, ein neues Schuppentier aus dem Mittel-Eozän der Grube Messel bei Darmstadt (Mammalia: Pholidota).... 83 ; ROTHAUSEN, K.: Die Schritte der Tetrapoden in die Meere des frühen Känozoikums. ... 99 ; FAHLBUSCH, V.: Fossile Kleinsäuger - gerät ihre Erforschung in die Sackgasse? ... 113 ; BUFFETAUT, E.: The significance of dinosaur remains in marine sediments: an investigation based on the French record. ... 125 ; RICHTER, A.: Der problematische Lacertilier llerdaesaurus (Reptilia, Squamata) aus der Unter-Kreide von Una und Galve (Spanien). ... 135 ; ZINKE, J. & RAUHUT, O.: Small theropods (Dinosauria, Saurischia) from the Upper Jurassic and Lower Cretaceous of the Iberian Peninsula. ... 163 ; RAUHUT, O. & KRIWET, J.: Teeth of a big Theropod Dinosaur from Porto das Barcas (Portugal).... 179 ; KOHRING, R. & REITNER, J.: Zur Eischalenstruktur von Varanus komodoensis OuwENS 1912. ... 187 ; LiLLEGRAVEN, J. A.: Age of upper reaches of Hanna Formation, northern Hanna Basin, south-central Wyoming. ... 203 ; WERNER, C.: Die kontinentale Wirbeltierfauna aus der unteren Oberkreide des Sudan (Wadi Milk Formation). ... 221 ; HEINRICH, W.-D.: Biostratigraphische Aussagen der Säugetierpaläontologie zur Alterstellung pleistozäner Travertinfundstätten in Thüringen. ... 251 ; FECHNER, G.: Der 'mitteloligozäne’ Septarienton bei Bad Freienwalde (nordöstl. Mark Brandenburg) und seine Dinoflagellaten-Zysten-Flora. ... 269 ; FECHNER, G.: Phytoplankton aus ästuarinen Ablagerungen des Miozäns der Bohrung "Groß-Apenburg" (Altmark). ... 283 ; MEHL, D., REITNER, J. & REISWIG, H.M.: Soft tissue organization of the deep water hexactinellid Schaudinnia arctica SCHULZE, 1900 from the Arctic Seamount Vesterisbanken (Central Greenland Sea). ... 301 ; MEHL, D. & ERDTMANN, B.-D.: Sanshapentella dapingi n.gen.n.sp.- a new hexactinellid sponge from the Early Cambrian (Tommotian) of China. ... 315 ; KEUPP, H. & ILG, A.: Paläopathologische Nachlese zur Ammoniten-Fauna aus dem Ober-Callovium der Normandie. ... 321 ; BANDEL, K. & RiEDEL F.: Classification of fossil and Recent Calyptraeoidea (Caenogastropoda) with a discussion on neomesogastropod phylogeny. ... 329 ; BECKER, R.T. & SCHREIBER, G.: Zur Trilobiten-Stratigraphie im Letmather Famennium (nördliches Rheinisches Schiefergebirge). ... 369 ; KOHRING, R. & SCHREIBER, G.: 'Latex-Micro-Molding' als neue Untersuchungsmethode von Bemstein-Inklusen - Vorläufige Mitteilung. ... 389 ; REITNER, J.: Mikrobialith-Porifera-Fazies eines Exogyren/Korallen-Patchreefs des Oberen Korallenooliths im Steinbruch Langenberg bei Oker (Niedersachsen). ... 397 ; MATYSZKIEWICZ, J.: Remarks on the Deposition of Pseudonodular Limestones in the Cracow Area (Oxfordian, Southern Poland). ... 419 ; BARON-SZABO, R.: Palökologie von nordspanischen Korallen des Urgon (Playa de Laga, Prov. Guemica). ... 441 ; SCHLÜTER, T.: Zur Verbreitung, Fazies und Stratigraphie der Karoo in Uganda. ... 453 ; KEUPP, H., BELLAS, S.M., FRYDAS, D. & KOHRING, R.: Aghia Irini, ein Neogenprofil auf der Halbinsel Gramvoüssa/NW-Kreta. ... 469 ; FRYDAS, D.: Stratigraphie und Taxonomie von Silicoflagellaten aus Diatomiten des Ober-Miozän von Zentral-Kreta (Griechenland). ... 483 ; FRYDAS, D.: Bericht über ein neues Silicoflagellaten-Vorkommen aus dem Piacenzium von Kreta, Griechenland. ... 495 ; RÖPSTORF, P. & REITNER, J.: Morphologie einiger Süßwasserporifera (Baikalospongia bacillifera, Lubomirskia baicalensis, Swartschewskia papyraced) des Baikal-Sees (Sibirien, Rußland.). ... 507 ; GLOY, U.: Bibliographie Institut für Paläontologie 1993. ... 527 ;
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläontologie
    Language: German , English
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  • 44
    Call number: ZSP-SCAR-570-14
    In: National Antarctic Research Report to SCAR, No. 14
    Type of Medium: Series available for loan
    Pages: 133 Seiten , Illustrationen
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 14
    Language: English
    Note: CONTENTS: I. National Committee for Antarctic Research, and National Operating Body. - II. Map of Stations. - Ill. Permanent Observatories, Regular Observations and Long-term Monitoring. - IV. Report on Highlights of Science Activities from Previous Reporting Period (1 Oct. 91 - 31 March 92). - A. Biology. - B. Geodesy & Geographic Information. - C. Geology. - D. Solid Earth Geophysics. - E. Glaciology. - F. Human Biology & Medicine. - G. Atmospheric Sciences. - H. Logistics. - I. Ocean Physical Sciences (incl. Marine Chemistry). - V. List of Permits and Rationale for Entry into SPAs and SSSIs. - VI. Prospectus of Planned Activities for Coming Reporting Period (1 April 92 - 31 March 93). - A. Biology. - B. Geodesy & Geographic Information. - C. Geology. - D. Solid Earth Geophysics. - E. Glaciology. - F. Human Biology & Medicine. - G. Atmospheric Sciences. - H. Logistics. - I. Ocean Physical Sciences (incl. Marine Chemistry). - VII. Future Activities Planned & Funded (beyond 31 March 93). - A. Biology. - B. Geodesy & Geographic Information. - C. Geology. - D. Solid Earth Geophysics. - E. Glaciology. - F. Human Biology & Medicine. - G. Atmospheric Sciences. - H. Logistics. - I. Ocean Physical Sciences (incl. Marine Chemistry). - VIII. Bibliography. - IX. List of Principal Investigators and Responsible Authorities.
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  • 45
    Call number: PIK M 490-19-93048
    Type of Medium: Monograph available for loan
    Pages: XIII, 577 S , Illustrationen, Diagramme
    Series Statement: Physica 191,1-4
    Language: English
    Location: A 18 - must be ordered
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  • 46
    Call number: MR 22.94995
    Type of Medium: Monograph available for loan
    Pages: 195 Seiten , Illustrationen, graphische Darstellungen, Karten
    Edition: First edition
    ISBN: 7-116-01128-5
    Language: English
    Location: Upper compact magazine
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  • 47
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-92/17
    In: CRREL Report, 92-17
    Description / Table of Contents: The CRREL Instrumented Vehicle (CIV), shear annulus, direct shear, andtriaxial compression devices were used to characterize the strength ofthawed and thawing soil. These strength values can be used in simpletraction models to predict the tractive performance of vehicles. Strength was evaluated in terms of the parameters c' and Φ' based on the Mohr-Coulomb failure criterion. It is proposed here that an instrumented vehicle is best suited for terrain characterization for mobility studies because the conditions created by a tire slipping on a soil surface are exactly duplicated. The c' and Φ' values from the shear annulus were found to overpredict traction because of the low normal stress applied by the annulus and the curved nature of the failure envelope. Of all the tests, the direct shear test yielded the highest Φ' value, most likely because the test was run at a slow deformation rate under drained conditions. The triaxial test results were the most similar to those from the vehicle. All test methods show Φ' increasingwith soil moisture up to the liquid limit of the soil and then decreasing. As measured with the vehicle, was also found to be strongly influenced by the thaw depth.
    Type of Medium: Series available for loan
    Pages: 17 Seiten , Illustrationen
    Series Statement: CRREL Report 92-17
    Language: English
    Note: CONTENTS Introduction Objective Background Strength measurement techniques Triaxial compression Direct shear Shear annulus device CRREL Instrumented Vehicle Discussion Comparison of methods Influence of soil conditions Traction prediction Conclusions References Abstract
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  • 48
    Call number: MOP 41324/I / Mitte
    Type of Medium: Monograph available for loan
    Pages: 162 Seiten
    Language: English
    Location: MOP - must be ordered
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  • 49
    Call number: AWI G4-22-94986
    Description / Table of Contents: Hydrological processes occurring within the vadose zone, especially in heterogeneous soils and tills typical of the Canadian shield, are not well understood. This research investigates the importance of the vadose zone in a small headwater basin (Harp 4-21) in the Canadian shield with respect to the generation of stream runoff quantity and quality during episodic rainfall and snowmelt events. The study focused specifically on: firstly the effect of variable antecedent moisture conditions on water-table and stream response, secondly, the significance of the stored vadose water in water extracted from a rising water-table, and thirdly the significance of preferential flowpathways in the vadose zone as a means of rapidly rotating, stored vadose water to the stream during runoff events. The instrumentation of the Harp 4-21 basin includes three v-notch weirs along the stream, numerous piezometers and wells, several soil lysimeters, and three tensiometer nests. Much of the data used in this study was obtained from five sites located along a hillslope transect. Soil water content at each of the hillslope sites was accurately determined using time domain reflectometry (TDR), whereas water table elevations were measured using both electronic water level tapes and calibrated rod floats. Preferential flowpath data was derived from flow gauging and chemical analyses of water samples. Results obtained from the near-stream and lower slope reaches of the hillslope transect indicated that soil water content in the vadose zone is maintained at a high level of saturation by shallow water-table depths. Further analysis of simultaneously measured soil water content and depth to water—table data clearly showed that the existence of a thick essentially saturated zone overlying the water table (capillary fringe) was responsible for the large and rapid water-table responses observed during many of the nine studied precipitation events. On a basin scale, the seasonal variability of the area in which the capillary fringe extended to the ground surface was largely responsible for the observed trend in basin yield (runoff volume/ rainfall volume) for the nine runoff events. Chemical tracing results using silica, pH and DOC showed that the large vadose water reservoir in the near-stream and lower slope areas was a dominant component in water extracted from a rising water-table during most precipitation events. Silica results from the near-stream vadose zone showed that only the massive groundwater recharge associated with spring snowmelt could completely replace the vadose water reservoir with shorter residence time snowmelt/rainfall water. The rapid routing of stored near-stream capillary fringe vadose water through preferential pathways (macropores, soil pipes) was a significant source of runoff to the stream during runoff events. The presence of soil pipes, along with the significant vadose water reservoir in near-stream and lower slope areas are sufficient to explain the large phreatic/vadose water component typically identified in two component flow separation models, and constitutes the basis of a physically-based conceptual runoff model for the Harp 4-21 basin.
    Type of Medium: Dissertations
    Pages: 172 Seiten , Illustrationen
    Language: English
    Note: Masterarbeit, Wilfrid Laurier University, Waterloo, 1992 , Table of Contents Abstract Acknowledgements List of Figures List of Tables Chapter 1 Introduction and Literature Review 1.1 introduction 1.2 Research objectives 1.3 Literature review 1.3.1 Overland flow 1.3.2 Overland flow from partial areas 1.3.3 Subsurface stormflow 1.3.4 The variable source area subsurface stormtlow concept 1.3.5 Groundwater and the capillary fringe effect 1.3.6 Preferential flow 1.3.6.1 Macropore flow 1.3.6.2 Unstable flow 1.4 Summary of uncertainties in the vadose zone Chapter 2 Methodology 2.1 Introduction 2.2 The Harp 4-21 basin: site description 2.2.1 Basin topography 2.2.2 Bedrock and surficial geology 2.2.3 Vegetation 2.2.4 General hydrology 2.3 Basin instrumentatio 2.3.1 Stream 2.3.2 Phreatic zone 2.3.3 Vadose zone 2.3.3.1 Soil moisture 2.3.3.2 Preferential flowpaths 2.4 Hillslope transect instrumentation 2.4.1 The hillslope transect 2.4.2 Time domain reflectometry 2.4.3 Vadose water extraction 2.5 Sampling techniques, frequency and chemical analyses 2.5.1 Precipitation 2.5.2 Stream 2.5.3 Phreatic zone 2.5.4 Vadose zone 2.5.4.1 Soil moisture measurement and analysis of the TDR trace 2.5.4.2 Vadose water sampling 2.5.5 Chemical analysis Chapter 3 Results and Discussion: Antecedent Moisture Conditions 3.1 Introduction 3.2 Runoff events ~ampled during the May 1990 - April 1991 field season 3.3 Assessment of antecedent moisture conditions in the Harp 4-21 basin 3.3.1 Seasonal basin yield 3.3.2 Seasonal depth to water-table 3.3.3 Tensiometric data 3.3.4 Soil moisture conditions in the hillslope transect (Time Domain Reflectometry) 3.3.4.1 Soil water content/depth to water-table relationship 3.3.4.2 Estimation of the capillary fringe thickness and the temporal variation of basin area in which it extends to the ground surface 3.4 Assessment of the origin of water in the vadose zone of near-stream and lower slope areas which experience significant water-table responses during runoff generating events 3.4.1 Introduction 3.4.2 Near-stream 07 piezometer nest 3.4.3 Lower slope TD4 mini-piezometer nest Chapter 4 Preferential flowpathways: Results and discussion 4.1. Discharge contributions to streamflow during runoff events 4.2. Assessment of the origin of water emmitted from the soil pipes during runoff events Chapter 5 Conclusions References Appendix I Appendix II Appendix Ill Appendix IV Appendix V , Englisch
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  • 50
    Series available for loan
    Series available for loan
    Boulder, Colo. : Geological Society of America
    Associated volumes
    Call number: S 90.0095(268)
    In: Special paper / The Geological Society of America, 268
    Type of Medium: Series available for loan
    Pages: ix, 406 Seiten , illustrationen, Karten , 28 cm
    ISBN: 0-8137-2268-3
    Series Statement: Special paper / The Geological Society of America 268
    Language: English
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  • 51
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-92/14
    In: CRREL Report, 92-14
    Description / Table of Contents: Large ice jams on the Salmon River have reached Salmon, Idaho, and resulted in major flood damage during 16 winters since the winter of 1936-37. Two recent ice jams, in February 1982 and January 1984, caused flooding that resulted in damages of $1 million and $1.8 million respectively. A detailed analysis of the winter air temperature records from 1936-37 through 1991-92 revealed a strong relationship between the duration and intensity of severe cold periods, the air temperature record prior to the severe cold periods, and the occurrence of ice jams reaching the city of Salmon that result in flooding. A threshold condition is identified from which the probability of icejams reaching the city can be determined from inspection of forecasted air temperatures. It was found that once an icejam reaches the city, average daily air temperatures of approximately 18 deg F are necessary to keep the jam in place. The effects of discharge on ice thickness, and therefore ice jam length, are shown to be minor and no relation could be found in this study. An ice control structure located upstream of the city of Salmon appears to be helping to alleviate ice-jam flooding.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 92-14
    Language: English
    Note: CONTENTS Preface Conversion factors Introduction Data sources and analysis Air temperature records Air temperature curves Air temperature record analysis Discharge records Results Phase 1 Phase 2 Phase 3 Effects of discharge Salmon River ice control Conclusions Literature cited Abstract
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  • 52
    Call number: AWI P5-22-95026
    Type of Medium: Monograph available for loan
    Pages: IV, 164 Seiten , Illustrationen
    ISBN: 0-920603-44-0
    Language: English
    Note: CONTENTS Introduction / Ming-ko Woo and Denis J. Gregor No Great Change: A Commentary on 50 Years of Watching Arctic Science / F. Kenneth Hare Arctic Climate in the Future / David Etkin and Tom Agnew Ice and Snow in the Arctic and Global Change / Peter Adams Snow, Sea· Ice and Climate: A Study of Scales / Ellsworth F. LeDrew and David G. Barber Past Climate Changes as Deduced from Canadian Ice Cores / Roy M. Koerner Natural and Anthropogenic Influences on the Chemical Composition of the Arctic Troposphere / Leonard A. Barrie Organic Micropollutants in Arctic Snow and Pim / Denis J. Gregor Climatic Change and the Permafrost Landscape / Antoni G. Lewkowicz Arctic Streamflow / Ming-ko Woo Ecology and Palaeocology of the Northern Treeline / Glen M. MacDonald and K. Gajewski Climate Change and its Effects on Canadian Arctic Plant Communities / Sylvia A. Edlund Environmental Change and Prehistory in Arctic Canada / Patricia D. Sutherland Concluding Remarks / George D. Hobson Glossary
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  • 53
    Monograph available for loan
    Monograph available for loan
    San Antonio, Tex : Geochemical Society
    Associated volumes
    Call number: MR 22.94901
    In: Special publication / The Geochemical Society, 4
    Type of Medium: Monograph available for loan
    Pages: xi, 184 Seiten , Illustrationen , 27 cm
    ISBN: 0-941809-03-X
    Series Statement: Special publication / The Geochemical Society No. 4
    Language: English
    Location: Upper compact magazine
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  • 54
    Monograph available for loan
    Monograph available for loan
    London : MacMillan
    Call number: PIK 23-95092
    Type of Medium: Monograph available for loan
    Pages: VIII, 328 S. , Ill., graph. Darst.
    ISBN: 0333572963
    Uniform Title: Caféiers et cafés
    Language: English
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  • 55
    Call number: M 94.0621
    In: The Institute of Mathematics and its applications conference series : N.S.
    Type of Medium: Monograph available for loan
    Pages: xiv, 457 S.
    ISBN: 0198536593
    Series Statement: The Institute of Mathematics and its applications conference series : N.S. 39
    Classification:
    C.1.8.
    Language: English
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  • 56
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Press
    Call number: M 93.0866
    Type of Medium: Monograph available for loan
    Pages: XII, 476 S.
    Edition: [1st publ.]
    ISBN: 0521430429
    Classification:
    Meteorology and Climatology
    Language: English
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  • 57
    Call number: S 90.0081(420)
    In: Reports of the Department of Geodetic Science and Surveying
    Type of Medium: Series available for loan
    Pages: XVIII, 214 S.
    Series Statement: Report / Department of Geodetic Science and Surveying, the Ohio State University 420
    Language: English
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    Call number: S 90.0081(424)
    In: Reports of the Department of Geodetic Science and Surveying
    Type of Medium: Series available for loan
    Pages: IX, 68 S.
    Series Statement: Report / Department of Geodetic Science and Surveying, the Ohio State University 424
    Language: English
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  • 59
    Monograph available for loan
    Monograph available for loan
    San Diego [u.a.] : Academic Press
    Associated volumes
    Call number: 5/M 94.0534/A
    In: Geophysical field theory and method
    Type of Medium: Monograph available for loan
    Pages: 581 S.
    ISBN: 0124020410
    Classification:
    A.2.1.
    Language: English
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  • 60
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-99
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 241 S. : graph. Darst., Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 99
    Language: English
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  • 61
    GFZ publications
    GFZ publications
    Potsdam
    Associated volumes
    Call number: AR 95.0052/1 / Regal 6
    In: Lecture material
    Type of Medium: GFZ publications
    Pages: 238 S.
    Classification:
    Seismology
    Language: English
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  • 62
    Call number: ZSP-553-27 ; ZSP-553-27(2. Ex.)
    In: Meddelelser om Grønland
    Type of Medium: Series available for loan
    Pages: 42 S. : Abb. + 2 Anl. ; 24 cm
    ISBN: 8750396048
    Series Statement: Meddelelser om Grønland : Geoscience 27
    Language: English
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  • 63
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley
    Call number: M 94.0658
    Type of Medium: Monograph available for loan
    Pages: xx, 508 S.
    ISBN: 0471545716
    Classification:
    C.1.9.
    Language: English
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  • 64
    Call number: M 94.0540
    Type of Medium: Monograph available for loan
    Pages: ix, 193 S.
    ISBN: 0750302488
    Classification:
    C.5.1.
    Language: English
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  • 65
    Monograph available for loan
    Monograph available for loan
    Philadelphia : Society for Industrial and Applied
    Associated volumes
    Call number: 19/M 95.0186
    In: Frontiers in applied mathematics
    Type of Medium: Monograph available for loan
    Pages: XIII, 273 S.
    ISBN: 0898712858
    Series Statement: Frontiers in applied mathematics 10
    Classification:
    C.2.10.
    Language: English
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  • 66
    Call number: AWI G9-94-0096
    Type of Medium: Monograph available for loan
    Pages: XII, 796 Seiten , Illustrationen
    ISBN: 4887041098
    Language: English
    Note: Contents 1. Crustal Evolution: East Antarctic Shield Archaean Events in Antarctica / L. P. BLACK, J. W. SHERATON and P. D. KINNY Metamorphic Evolution of the Sør Rondane Mountains, East Antarctica / M. ASAMI, Y. OSANAI, K. SHIRAISHI and H. MAKIMOTO Geochemical Characteristics of Metamorphic Rocks from the Central Sør Rondane Mountains, East Antarctica / Y. OSANAI, K. SHIRAISHI, Y. TAKAHASHI, H. ISHIZUKA, Y. TAINOSHO, N. TSUCHIYA, T. SAKIYAMA and S. KODAMA Sm-Nd and Rb-Sr Ages of Metamorphic Rocks from the Sør Rondane Mountains, East Antarctica / K. SHIRAISHI and H. KAGAMI Reconnaissance Geochronologic Data on Proterozoic Polymetamorphic Rocks of the Eastern Sør Rondane Mountains, East Antarctica / E. S. GREW, W. I. MANTON, M. ASAMI and H. MAKIMOTO Petrochemical Character and Rb-Sr Isotopic Investigation of the Granitic Rocks from the Sør Rondane Mountains, East Antarctica / Y. T AINOSHO, Y. TAKAHASHI, Y. ARAKAWA, Y. OSANAI, N. TSUCHIYA, T. SAKIYAMA and M. OWADA Carbon and Oxygen Isotopic Compositions of Marbles from the Sør Rondane Mountains, East Antarctica / N. TSUCHIYA, Y. OSANAI and H. WADA 40Ar-39Ar Geochronological Studies on some Paleomagnetic Samples of East Antarctica / Y. T AKIGAMI, M. FUN AKI and K. TOKIEDA The First Report of a Cambrian Orogenic Belt in East Antarctica - An Ion Microprobe Study of the Lützow-Holm Complex / K. SHIRAISHI, Y. HIROI, D. J. ELLIS, C. M. FANNING, Y. MOTOYOSHI and Y. NAKAI A New Insight of Possible Correlation between the Lützow-Holm Bay Granulites (East Antarctica) and the Sri Lankan Granulites / Y. OGO, Y. HIROI, K. B. N. PRAME and Y. MOTOYOSHI Osumilite-Producing Reactions in High Temperature Granulites from the Napier Complex, East Antarctica: Tectonic Implications / B. J. HENSEN and Y. MOTOYOSHI Gneisses of the Porthos and Athos Ranges, Northern Prince Charles Mountains, East Antarctica: Constraints on the Prograde and Retrograde P-T Path / D. E. THOST and B. J. HENSEN Mineral Reaction Textures in High-Grade Gneisses: Evidence for Contrasting Pressure-Temperature Paths in the Proterozoic Complex of East Antarctica / I. C. W. FITZSIMONS and S. L. HARLEY Mode of Occurrence, Geochemistry and Mineral Textures of Mafic to Ultramafic Rocks from the Bolingen Islands, Prydz Bay, East Antarctica / D. E. THOST, Y. MOTOYOSHI and B. J. HENSEN The Significance of Reworking, Fluids and Partial Melting in Granulite Metamorphism, East Prydz Bay, Antarctica / S. L. HARLEY, I. C. W. FITZSIMONS, I. S. BUICK and G. WATT Stable Isotope Studies of Granulite Facies Metamorphism in the Rauer Group, East Antarctica / I. S. BUICK, S. L. HARLEY and D. MATTEY A Late-Proterozoic Extensional-Compressional Tectonic Cycle in East Antarctica / J. D. HOEK, P. H. G. M. DIRKS and C. W. PASSCHIER Re-Examination of the Metamorphic Evolution of the Larsemann Hills, East Antarctica / L. REN, Y. ZHAO, X. LIU and T. CHEN Geochronology of the Late Granite in the Larsemann Hills, East Antarctica / Y. ZHAO, B. SONG, Y. WANG, L. REN, J. LI and T. CHEN The First Study of Upper Mantle Inclusions from the Prince Charles Mountains, East Antarctica / A. V. ANDRONIKOV Mafic Igneous Suites in the Lambert Rift Zone / E. V. MIKHALSKY, A. V. ANDRONIKOV and B. V. BELIATSKY Granitic Rocks of the Jetty Peninsula, Amery Ice Shelf Area, East Antarctica / W. I. MANTON, E. S. GREW, J. HOFMANN J. W. SHERATON Paleomagnetic and 40 Ar/39 Ar Dating Studies of the Mawson Charnockite and Some Rocks from the Christensen Coast / M. FUNAKI and K. SAITO 2. Crustal Evolution: Transantarctic Mountains and West Antarctica Multiple Petrotectonic Events in High-Grade Metamorphic Rocks of the Nimrod Group, Central Transantarctic Mountains, Antarctica / J. W. GOODGE, V. L. HANSEN and S. M. PEACOCK Metamorphic Facies of the Ross Orogeny in the Southern Wilson Terrane of Northern Victoria Land, Antarctica / F. TALARICO, M. FRANCESCHELLI, B. LOMBARDO, R. PALMERI, P. C. PERTUSATI, N. RASTELLI and C. A. RICCI Metasedimentary Rocks of Western Wilson Terrane (Victoria Land - Oates Land) and Gondwana Connections to Australia / D. N. B. SKINNER Compressional Causes for the Early Paleozoic Ross Orogen - Evidence from Victoria Land and the Shackleton Range / G. KLEINSCHMIDT, W. BUGGISCH and T. FLOETTMANN Pre-Beacon Tectonic Development of the Transantarctic Mountains / E. STUMP Statistical Analysis of Geochemical Patterns in Fine-Grained Permian Mudrocks from the Beardmore Glacier Region, Antarctica / T. C. HORNER and L. A. KRlSSEK Stratigraphy and Sedimentology of Vertebrate Bone-Bearing Beds in the Triassic (and Jurassic?) Fremouw and Falla Formations, Beardmore Glacier Region, Antarctica / L. A. KRISSEK, T. C. HORNER, D. H. ELLIOT and J. W. COLLINSON Early Paleozoic Lamprophyre Dikes of Southern Victoria Land: Geology, Petrology and Geochemistry / B. Wu and J. H. BERG Crustal Xenoliths from Cape McCormick Crater, Northern Victoria Land / J. H. BERG and B. Wu Xenoliths from the Volcanic Province of West Antarctica and Implications for Lithospheric Structure and Processes / R. J. WYSOCZANSKI and J. A. GAMBLE Geological and Geophysical Exploration in the Northern Ford Ranges, Marie Byrd Land, West Antarctica / B. P. LUYENDYK, S. M. RICHARD, C. H. SMITH and D. L. KIMBROUGH Structure and Cooling History of the Fosdick Metamorphic Complex, Marie Byrd Land, West Antarctica / S. M. RICHARD Metapelites and Migmatites at the Granulite Facies Transition, Fosdick Metamorphic Complex, Marie Byrd Land, West Antarctica / C. H. SMITH 3. Syn- and Post-Breakup of Gondwana Mesozoic and Cenozoic Kinematic Evolution of the Transantarctic Mountains / T. J. WILSON The West Antarctic Rift System - A Propagating Rift "Captured" by a Mantle Plume? / J. C. BEHRENDT, W. LEMASURIER and A. K. COOPER Apatite Fission Track Evidence for Contrasting Thermal and Uplift Histories of Metamorphic Basement Blocks in Western Dronning Maud Land / J. JACOBS, E. HEJL, G. A. WAGNER and K. WEBER Early Cretaceous Uplift of the Southern Sentinel Range, Ellsworth Mountains, West Antarctica / P. G. FITZGERALD and E. STUMP Petrologic Comparison of Paleozoic Rocks from the English Coast, Eastern Ellsworth Land, and the Ellsworth Mountains / T. S. LAUDON and C. CRADDOCK Provenance of Paleocene Strata, Seymour Island / D. H. ELLIOT, S. M. HOFFMAN and D. E. RIESKE Sedimentology of the Miers Bluff Formation, Livingston Island, South Shetland Islands / A. ARCHE, J. LOPEZ-MARTINEZ and E. MARTINEZ DE PISON Late Cretaceous and Eocene Palynofloras from Fildes Peninsula, King George Island (South Shetland Islands), Antarctica / L. CAO Early Tertiary Palaeoclimate of King George Island, Antarctica - Evidence from the Fossil Hill Flora / H.M. LI Modes of Formation and Accretion of Oceanic Material in the Mesozoic Fore-Arc of Central and Southern Alexander Island, Antarctica: A Summary / P.A. DOUBLEDAY and T. H. TRANTER The Magmatic Complexes of the Rouen Mountains and Elgar Uplands from Alexander Island, Antarctic Peninsula: Geochemical Constraints / B. K. KAMENOV and C. T. PIMPIREV Transverse Variations in the Gerlache Strait Plutonic Rocks: Effects of the Aluk Ridge-Trench Collision in the Northern Antarctic Peninsula / M.A. PARADA, J.-B. ORSINI and R. ARDILA 4. Recent Tectonics of Antarctic Peninsula and Subantarctic Regions Evolution of the Bransfield Basin and Rift, West Antarctica / K. BIRKENMAJER Uplift Movements in King George Island Associated Bransfield Rift Activity / M. ARANEDA and O. GONZALEZ-FERRAN Geotransect Drake Passage - Weddell Sea, Antarctica / R. A. J. TROUW and L. A. P. GAMBOA Long-Range Sidescan Sonar (GLORIA) Survey of the Antarctic Peninsula Pacific Margin / J. S. TOMLINSON, C. J. PUDSEY, R. A. LIVERMORE, R. D. LARTER and P. F. BARKER Marine Magnetic Anomalies in Bransfield Strait, Antarctica / Y. KIM, T. W. CHUNG and S. H. NAM Geochronology and Geochemistry of the Igneous Rocks from Barton and Fildes Peninsulas, King George Island: A Review / Y.-J. JWA, B.-K. PARK and Y. KIM Geophysical Features of Deception Island / R. ORT
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  • 67
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley & Sons
    Call number: M 94.0154 ; M 94.0597 ; AWI G1-92-0462
    Type of Medium: Monograph available for loan
    Pages: xiv, 570 S.
    Edition: 2nd ed.
    ISBN: 0471531316
    Classification:
    A.2.1.
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 68
    Monograph available for loan
    Monograph available for loan
    Washington : National Academy Press
    Call number: M 93.1023
    Type of Medium: Monograph available for loan
    Pages: xii, 202 S.
    ISBN: 0309047943
    Classification:
    Oceanology
    Language: English
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  • 69
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Oxford Univ. Press
    Call number: M 94.0585
    Type of Medium: Monograph available for loan
    Pages: ix, 441 S.
    ISBN: 0195044428
    Classification:
    Mineralogy
    Language: English
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  • 70
    Monograph available for loan
    Monograph available for loan
    Yverdon [u.a.] : Gordon and Breach Science Publishers
    Associated volumes
    Call number: M 94.0666
    In: Developments in nanotechnology
    Type of Medium: Monograph available for loan
    Pages: xv, 348 S.
    ISBN: 2884490019
    Series Statement: Developments in nanotechnology 2
    Classification:
    C.5.2.
    Language: English
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  • 71
    Monograph available for loan
    Monograph available for loan
    Boston [u.a.] : Academic Press
    Call number: M 94.0532 ; AWI S1-92-0472
    Description / Table of Contents: Contents: Preface to the third edition. - Preface to the second edition. - Preface to the first edition. - 1 Fundamentals. - 2 Parabolic equations. - 3 Elliptic equations. - 4 Hyperbolic Equations. - 5 Special Topics. - Author Index. - Subject Index
    Type of Medium: Monograph available for loan
    Pages: ix, 451 S.
    Edition: 3rd ed.
    ISBN: 012056761X
    Series Statement: Computer science and scientific computing
    Classification:
    C.1.8.
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 72
    Monograph available for loan
    Monograph available for loan
    Providence, RI : American Mathematical Society
    Associated volumes
    Call number: M 94.0630
    In: Translations of mathematical monographs
    Type of Medium: Monograph available for loan
    Pages: ix, 225 S.
    ISBN: 0821845705
    Series Statement: Translations of mathematical monographs 114
    Classification:
    C.1.6.
    Language: English
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  • 73
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 95.0073/2
    In: Geographical information systems
    Type of Medium: Monograph available for loan
    Pages: xxix, 447 S.
    ISBN: 0582056616
    Classification:
    Photogrammetry, Remote Sensing
    Language: English
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  • 74
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs, NJ : Prentice-Hall
    Call number: M 96.0053 ; 19/M 94.0691
    Type of Medium: Monograph available for loan
    Pages: x, 646 S.
    Edition: 2nd ed.
    ISBN: 0136250475
    Series Statement: Prentice-Hall international editions
    Classification:
    C.1.8.
    Language: English
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  • 75
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-105
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: III, 72 S. : Ill., graph. Darst.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 105
    Language: English
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  • 76
    Monograph available for loan
    Monograph available for loan
    Chichester : Wiley
    Call number: AWI G8-92-0460
    Description / Table of Contents: Designed to help anyone involved with small-scale geophysical surveys, this handbook has been written at a level suitable for undergraduate students of geology and geophysics, as well as professional workers in the field. It contains a wealth of practical information based upon the author's many years of field experience as a consultant geophysicist. Essential field techniques and associated equipment are described with particular emphasis being given to practical limitations, common problems and pitfalls. The author has provided many useful examples, tables, checklists and illustrations, making the book concise and easy to use.
    Type of Medium: Monograph available for loan
    Pages: VII, 182 Seiten , Illustrationen
    Edition: Reprinted
    ISBN: 0471932485
    Series Statement: Geological Society of London handbook
    Language: English
    Note: Contents Preface 1 Introduction 1.1 Fields 1.2 Geophysical equipment 1.3 Geophysical data 1.4 Bases and base networks 2 Gravity method 2.1 Physical basis of the gravity method 2.2 Gravity meters 2.3 Gravity reductions 2.4 Gravity surveys 2.5 Field interpretation 3 Magnetic method 3.1 Magnetic properties 3.2 The magnetic field of the Earth 3.3 Magnetic instruments 3.4 Magnetic survey practice 3.5 5 imple magnetic interpretation 4 Radioactivity surveys 4.1 Natural radiation 4.2 Radiation detectors 4.3 Radiometric surveys 5 Electric current methodsgeneral considerations 5.1 Resistivity 5.2 Electrode arrays 5.3 Equipment for resistivity surveys 6 Direct-current methods 6.1 SP surveys 6.2 Resistivity profiling 6.3 Resistivity depth-sounding 7 Induced polarization 7.1 Polarization fundamentals 7.2 Time-domain IP surveys 7.3 Frequency-domain surveys 7.4 Handling IP data 8 Electromagnetic methods 8.1 Induction principles 8.2 Continuous-wave systems 8.3 Other e.m. techniques 9 VLF methods 9.1 VLF radiation 9.2 VLF instruments 9.3 VLF maps 10 Seismic methods - general considerations 10.1 Seismic waves 10.2 Seismic sources 10.3 Detection of seismic waves 10.4 Recording seismic waves 11 Seismic reflection 11.1 Reflection theory 11.2 Reflection surveys 12 Seismic refraction 12.1 Refraction surveys 12.2 Field interpretation 12.3 Limitations of the refraction method Appendix Terrain corrections for Hammer zones B to M References and further reading Index
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  • 77
    Monograph available for loan
    Monograph available for loan
    Pachuca, Hgo., México : Secretaría de Energía, Minas e Industria Paraestatal, Subsecretaría de Minas e Industria Básica
    Call number: M 04.0310
    Type of Medium: Monograph available for loan
    Pages: 154 S. + 3 Kt.-Beil.
    Edition: 1st ed.
    ISBN: 9686710078
    Series Statement: Geological-mining monograph of the state ... M-2e
    Uniform Title: Monografía geológico-minera del estado de Zacatecas
    Classification:
    Regional Geology
    Language: English
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  • 78
    Monograph available for loan
    Monograph available for loan
    New York : IEEE Press
    Call number: M 94.0528
    Type of Medium: Monograph available for loan
    Pages: xi, 539 S.
    ISBN: 0780304225
    Classification:
    C.2.9.
    Language: English
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  • 79
    Monograph available for loan
    Monograph available for loan
    Tulsa, Okla. : Soc. of Exploration Geophysicists
    Associated volumes
    Call number: M 94.0613
    In: Geophysical references
    Type of Medium: Monograph available for loan
    Pages: viii, 330 S.
    Edition: repr.
    ISBN: 0931830397
    Series Statement: Geophysical references vol. 2
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 80
    facet.materialart.
    Unknown
    Kensington
    Associated volumes
    Call number: 92.0608
    In: Annual report ...
    Pages: 40 S.
    Classification:
    A.1.1.
    Language: English
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  • 81
    Call number: PIK N 071-92-0629
    Type of Medium: Monograph available for loan
    Pages: 200 p.
    Edition: first published
    ISBN: 0521438292
    Language: English
    Location: A 18 - must be ordered
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  • 82
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    Monograph available for loan
    Berlin : Akad.-Verl
    Associated volumes
    Call number: M 95.0597
    In: Mathematical research
    Type of Medium: Monograph available for loan
    Pages: 170 S.
    ISBN: 3055015789
    Series Statement: Mathematical research 68
    Classification:
    C.1.8.
    Language: English
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  • 83
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    Monograph available for loan
    Jülich : Forschungszentrum
    Associated volumes
    Call number: M 95.0570
    In: Berichte des Forschungszentrums Jülich
    Type of Medium: Monograph available for loan
    Pages: 157 S.
    Series Statement: Berichte des Forschungszentrums Jülich 2684
    Classification:
    Regional Geology
    Language: English
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  • 84
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    Monograph available for loan
    Minneapolis : University of Minnesota Press
    Associated volumes
    Call number: M 96.0157
    In: Minnesota studies in the philosophy of science
    Type of Medium: Monograph available for loan
    Pages: xxviii, 508 S.
    ISBN: 0816619794
    Series Statement: Minnesota studies in the philosophy of science vol. xv
    Classification:
    E.7.
    Language: English
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  • 85
    Call number: 12/M 96.0315
    In: Developments in atmospheric science
    Type of Medium: Monograph available for loan
    Pages: XII, 265 S.
    ISBN: 0444889140
    Series Statement: Developments in atmospheric science 21
    Classification:
    Meteorology and Climatology
    Language: English
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  • 86
    Call number: 96.0303
    In: Special publication / Norges Geologiske Undersøkelse
    Pages: 45 S.
    ISBN: 8273850854
    Series Statement: Special publication / Norges Geologiske Undersøkelse 5
    Classification:
    Regional Geology
    Language: English
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  • 87
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    Monograph available for loan
    Stuttgart [u.a.] : Fischer
    Associated volumes
    Call number: M 96.0187/2
    In: Evolution of palaeoecology and palaeoenvironment of permian and triassic fluvial basins in Europe
    Type of Medium: Monograph available for loan
    Pages: XXII, S. 739 - 1340
    Classification:
    Historical Geology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 88
    Monograph available for loan
    Monograph available for loan
    San Diego [u.a.] : Academic Press
    Call number: M 96.0424
    Type of Medium: Monograph available for loan
    Pages: xi, 518 S.
    ISBN: 0126434204
    Classification:
    Geodynamics
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 89
    Call number: ZSP-166(27)
    In: Berichte aus dem MARUM und dem Fachbereich Geowissenschaften der Universität Bremen, Nr. 27
    Type of Medium: Series available for loan
    Pages: 205 Seiten , Illustrationen , 29 cm
    ISSN: 0931-0800
    Series Statement: Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen 27
    Language: German , English
    Note: Zugleich: Dissertation, Universität Bremen, 1992
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 90
    Monograph available for loan
    Monograph available for loan
    San Diego [u.a.] : Academic Press
    Call number: M 97.0022
    Type of Medium: Monograph available for loan
    Pages: xx, 574 S.
    Edition: 2nd ed.
    ISBN: 0122236513
    Classification:
    Petrophysics
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 91
    Call number: ZSP-708-7
    In: SCAR report, No. 7
    Type of Medium: Series available for loan
    Pages: 54 Seiten , Illustrationen, graphische Darstellungen
    Series Statement: SCAR report 7
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 92
    Call number: ZSP-708-8
    In: SCAR report, No. 8
    Type of Medium: Series available for loan
    Pages: 40 Seiten
    Series Statement: SCAR Report 8
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 93
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Springer
    Associated volumes
    Call number: M 95.0672
    In: Graduate texts in mathematics
    Type of Medium: Monograph available for loan
    Pages: xii, 231 S.
    ISBN: 0387978755
    Series Statement: Graduate texts in mathematics 137
    Classification:
    C.1.6.
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 94
    Monograph available for loan
    Monograph available for loan
    New York : The Free Press
    Call number: M 96.0539
    Type of Medium: Monograph available for loan
    Pages: xx, 473 S.
    ISBN: 0029256151
    Classification:
    E.8.
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 95
    Monograph available for loan
    Monograph available for loan
    New York : Freeman
    Call number: M 96.0458
    Type of Medium: Monograph available for loan
    Pages: xii, 531 S.
    ISBN: 0716722526
    Classification:
    Tectonics
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 96
    Monograph available for loan
    Monograph available for loan
    Boca Raton [u.a.] : CRC Press
    Call number: M 15.89102
    Type of Medium: Monograph available for loan
    Pages: X, 190 S. , graph. Darst.
    ISBN: 0849388309
    Language: English
    Location: Reading room
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  • 97
    Series available for loan
    Series available for loan
    Boulder, Colo. : National Center for Atmospheric Research
    Associated volumes
    Call number: AWI A6-16-90344
    In: NCAR technical notes / National Center for Atmospheric Research : STR ; 366
    Type of Medium: Series available for loan
    Pages: 256 S , Ill., graph. Darst
    Series Statement: NCAR-TN 366 : STR
    Language: English
    Note: Table of Contents: 1. Data description. - Origin. - Changes in Operational Analysis Systems. - Geopotential grid processing. - Temperature, wind and wave flux calculations. - 2. Statistical calculations. - 3. References. - 4. Results. - Monthly average meridional cross sections. - Means and variances of zonal mean winds, temperatures and wave fluxes, plus stationary and transient wave statistics. - Hemispheric polar projections for January, April, July and October. - Mean geopotential height, temperature, wind speed and daily geopotential variance maps for 700, 500, 300, 100, 50, 10 and 1 mb. - Ensemble average latitude-time diagrams. - Zonal mean winds and temperatures, and stationary and transient eddy geopotential height, temperature and wave flux quantities. - Ensemble average height-time diagrams. - Zonal mean winds and temperatures, and stationary and transient eddy geopotential heights and temperatures. - Latitude-time and height-time diagrams of zonal winds and rms geopotential, height wave amplitudes for individual years 1979-1990. - Tables of monthly mean temperatures and zonal winds.
    Location: AWI Reading room
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  • 98
    Monograph available for loan
    Monograph available for loan
    Bochum : Institut für Geophysik der Ruhr-Universität Bochum
    Call number: M 17.90806
    Type of Medium: Monograph available for loan
    Pages: v, 74 S. , Ill., graph. Darst.
    Language: English
    Note: Univ., Diplomarbeit--Bochum, 1992
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 99
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Macmillan Publishing Comp. [u.a.]
    Call number: M 95.0694
    Type of Medium: Monograph available for loan
    Pages: xiv, 717 S.
    ISBN: 0023393599
    Classification:
    Sedimentology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 100
    Monograph available for loan
    Monograph available for loan
    Basel [u.a.] : Birkhäuser
    Associated volumes
    Call number: M 96.0042
    In: Theory of function spaces
    Type of Medium: Monograph available for loan
    Pages: VIII, 370 S.
    ISBN: 3764326395
    Series Statement: 84
    Classification:
    C.1.6.
    Language: English
    Location: Upper compact magazine
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