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  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(500-C)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, C-14 S.
    Series Statement: U.S. Geological Survey professional paper 500-C
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    In:  Bull. Seism. Soc. Am., Taipei, 3-4, vol. 89, no. 5, pp. 1296-1312, pp. 2151, (ISSN: 1340-4202)
    Publication Date: 1999
    Keywords: Seismology ; Source ; Surface waves ; Rayleigh waves ; Earthquake precursor: others (animal behav., wobble, tides) ; Earthquake precursor: prediction research ; BSSA
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  • 3
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    Univ. Toronto Press
    In:  Toronto, 3rd Edition, 353 pp., Univ. Toronto Press, vol. 20, no. Publ. No. 12, pp. 23-40, (ISBN 1-4020-3326-5, VIII + 343 pp.)
    Publication Date: 1974
    Keywords: Textbook of geophysics ; Stress ; Friction ; Fluids ; Physical properties of rocks
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  • 4
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    In:  Bull. Seism. Soc. Am., Hokkaido University, Pergamon, vol. 47, no. 1-2, pp. 89-110, pp. B10302, (ISSN: 1340-4202)
    Publication Date: 1957
    Keywords: Source ; Seismology ; Fault plane solution, focal mechanism ; BSSA
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  • 5
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    In:  Bull. Seism. Soc. Am., Hokkaido University, Pergamon, vol. 54, no. 1-2, pp. 1519-1528, pp. B10302, (ISSN: 1340-4202)
    Publication Date: 1964
    Keywords: Source ; Seismology ; Fault plane solution, focal mechanism ; BSSA
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  • 6
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    In:  Bull. Seism. Soc. Am., London, Am. Soc. Mech. Eng., vol. 53, no. 4, pp. 811-816, pp. 2099, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1963
    Keywords: Fault plane solution, focal mechanism ; Statistical investigations ; Earthquake ; Source ; BSSA
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 31 (1982), S. 269-272 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Die Stellungen einer Reihe von Klüften wurden in Zentraläthiopien gemessen. Es wird gezeigt, daß diese sehr gut mit dem Spannungssystem zusammenpassen, welches gewöhnlich als Ursache des ostafrikanischen Grabensystems angenommen wird, falls sie als Scherphänomene interpretiert werden.
    Notes: Summary The orientations of some joints were measured in Central Ethiopia. It is shown that these fit very well into the commonly assumed stress system causing the Rift Valley, if they are interpreted as shearing phenomena.
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  • 8
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Summary An attempt was made to obtain indications of the present-day geotectonic stresses in Austria from records of hydraulic fracturing operations in oil wells. Inasmuch as only the course of the well-head pressure was available and no data regarding the rock formations were known, it was only possible to determine the smallest principal pressure value for eight different holes. The values found range between 63 and 94 per cent of the overburden pressure. This corresponds to values normally found in the world and Austria is thus recognized as a normal intraplate region.
    Notes: Zusammepfassung Es wurde versucht, aus Aufzeichnungen von österreichischen Fracoperationen Angaben für die Berechnung von Spannungen zu finden. Da jedoch nur der Druckverlauf am Sondenkopf zur Verfügung stand und keine Formationsdaten bekannt waren, konnte nur $$P_p = \sigma _{h_2 } $$ die kleinste Hauptspannung, für insgesamt acht verschiedene Sonden abgeschätzt werden. Die Werte lagen zwischen 63% und 94% des Überlagerungsgewichtes. Dies entspricht durchaus globalen Normalwerten, womit Österreich als „normale Intraplateregion” erkannt wird.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 28 (1979), S. 89-106 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Die vorliegende Studie hat den Zweck, einen Beitrag zur Tektonik der westlichen Himalaya-Regionen von Jammu, Kashmir und Ladakh zu leisten. Während des Sommers 1978 wurde die Orientierung vieler Klüfte in Aufschlüssen längs der Straße von Jammu über Srinagar nach Leh gemessen. Aufgrund der Annahme, daß die sichtbaren Felsklüfte Gleitflächen des neotektonischen Spannungsfeldes darstellen, ist es möglich, die Hauptspannungsrichtungen aus den Kluftstellungen mit einer statistischen Methode zu berechnen. Weiters wurde auch schon der Ansatz gemacht, daß die Talrichtungen ebenfalls neotektonischen Gleitzonen entsprechen. Somit wurde auch eine statistische Analyse der Talrichtungen von Jammu und Kaschmir gemacht und mit den Kluftstellungen verglichen. Es ergab sich, daß sowohl bei Klüften als auch bei Talrichtungen zwei Paare je zueinander konjugierter Richtungssysteme existieren. Das erste ist vorrangig; es zeigt Polrichtungen von N 55°E und N 138°E, was einer Hauptdruckspannung in Richtung N 7°E entspricht. Das zweite Paar ist bei den Klüften nur spärlich entwickelt; es hat Polazimute von N 92°E und N 358°E. Feldbeobachtungen zeigen, daß dieses zweite System durch das erste, vorrangige, begrenzt ist, so daß es als älter gelten und daher einer früheren Orientierung des tektonischen Sapnnungssystems entsprechen muß. Bei den Tälern sind beide Richtungspaare vorhanden, was bedeutet, daß die älteren Orientierungen hier länger konserviert werden als bei den Klüften. Die Orientierung des neotektonischen Spannungsfeldes, wie es aus den Kluftstellungen abgeleitet wurde, ist in guter Übereinstimmung mit den Vorstellungen der Plattentektonik. So schiebt sich Indien nordwärts; die Klüfte sind Gleitflächen, die in dieses Schema passen.
    Notes: Summary The present study aims at making a contribution to the tectonics of the Western Himalayan Regions of Jammu, Kashmir and Ladakh. During the summer of 1978, the orientation of many joints has been measured in outcrops along the road from Jammuvia Srinagar to Leh. Based upon the contention that the visible rock-joints are shear surfaces produced by the neotectonic stress field, the principal stress directions of the latter can be calculated from a statistical analysis of the orientations of the joints. Furthermore, it has also been proposed that many valley trends follow tectonic shear zones. Thus, a statistical evaluation of the valley trends in Jammu and Kashmir has been made. The analysis of the orientations of joints and river valley trends has shown that, in both these features, there are two pairs of conjugate systems of directions. The first, the preponderant one, has preferred pole directions of N 55°E and N 138°E; it is produced by a principal horizontal compression with an azimuth of N 7°E. The second system is only vestigially developed in the joints, it has preferred pole-azimuths around N 92°E and N 358°E. Field evidence shows joints belonging to this second system to terminate at joints belonging to the first (preponderant) system which permits one to infer that the second system is older than the first and, thus, belongs to previous orientation of the tectonic stress field. In the valleys, both systems are almost equally well developed which indicates that earlier orientations are preserved in valleys for a longer time than in joints. The orientations of the neotectonic stress field deduced from joint-orientation measurements are in good conformity with the ideas of plate tectonics. Thus, India “pushes” (or is dragged) northward; the joints are slip surfaces fitting into this pattern.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 32 (1983), S. 191-196 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Während drei Expeditionen in das Grenzgebiet zwischen Algerien, Libyen und Niger wurden Kluftorientierungen an einer Reihe von Aufschlüssen gemessen. Die bevorzugten Streichrichtungen der Klüfte sind NW-SO und NO-SW. Dies bezeugt, daß die Hauptachsen des neotektonischen Spannungsfeldes NS und OW gerichtet sind.
    Notes: Summary During three expeditions into the border area of Algeria, Niger and Libya, the orientations of joints were measured in a variety of outcrops. The preferred orientations (strikes) of these joints are NW-SE and NE-SW, indicating a neotectonic stress field with principal stress directions oriented NS and EW.
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