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  • 1
    Publication Date: 2020-02-12
    Language: German , English
    Type: info:eu-repo/semantics/conferenceObject
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  • 2
    Publication Date: 2020-02-12
    Language: German , English
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  • 3
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2020-02-12
    Language: German , English
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  • 4
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    In:  GeoForschungsZeitung / Ausgabe Dezember 2011
    Publication Date: 2020-02-12
    Language: German
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  • 5
    Call number: M 99.0277 ; Q 1093 / Regal 50
    In: Nova acta Academiae Caesareae Leopoldino-Carolinae Germanicae Naturae Curiosorum
    Type of Medium: Monograph non-lending collection
    Pages: 216 S.
    Series Statement: Nova acta Academiae Caesareae Leopoldino-Carolinae Germanicae Naturae Curiosorum Bd. 60, Nr. 1
    Language: German
    Location: Pendulum room
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 6
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2020-02-12
    Description: The Eifel is the youngest volcanic area of Central Europe. The last eruption occurred approximately 11000 years ago. Little is known about the deep origin and the mechanism responsible for the Eifel volcanic activity. Earthquake activity indicates that the Eifel is one of the most geodynamically active areas of Central Europe. In this work the receiver function method is used to investigate the upper mantle structure beneath the Eifel. Data from 96 teleseismic events (mb 〉 5.2) that were recorded by both permanent stations and a temporary network of 33 broadband and 129 short period stations had been analyzed. The temporary network was operating from November 1997 till June 1998 and covered an area of approximately 400x250 km^2 centered on the Eifel volcanic fields. The receiver function analysis reveals a clear image of the Moho and the mantle discontinuities at 410 km and 660 km depth. Average Moho depth is approximately 30 km and it shows little variation over the extent of the network. The observed variations of converted waveforms are possibly caused by lateral variations in crustal structure, which could not resolved by it receiver functions}. Inversions of data and migrated it receiver functions} from stations of the central Eifel array suggest that a low velocity zone is present at about 60 to 90 km depth in the western Eifel region. There are also indications for a high velocity zone around 200 km depth, perhaps caused by dehydration of the rising plume material. The results suggest that P-to-S conversions from the 410-km discontinuity arrive later than in the IASP91 reference model. The migrated data show a depression of the 410 km discontinuity of about 20 km, which correspond to an increase of temperature of about 140° Celsius. The 660 km discontinuity seems to be unaffected. This indicates that no mantel material rises up from directly below the 660 km discontinuity in the Eifel region or the Eifel-Plume has its origin within the transition zone.
    Language: German
    Type: info:eu-repo/semantics/doctoralThesis
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  • 7
    Publication Date: 2020-02-12
    Description: The interior of the Earth is the least accessible region in our environment. Elastic waves, generated by large earthquakes, are used to explore the interior of the Earth. The globally recorded seismic signals must be inverted with mathematical techniques into models of the Earth. The reflectivity method, developed about fifty years ago for a one dimensional Earth model, is still one of the most successful techniques for modeling waveforms. The big advantage of this method is that it provides the complete response of the medium. It is not uncommon that new seismic signals are first discovered in theoretical seismograms before they are found in the observed data. Global seismology is primarily an observational science. It was founded by Ernst von Rebeur-Paschwitz in 1889 with the announcement in the journal “Nature” of the successful recording at the Royal Prussian Observatories in Potsdam of an earthquake that occurred in Japan. The installation of seismic stations and collection of data is still the primary task in Seismology. The GFZ German Research Centre for Geosciences and other international institutions are installing increasing numbers of seismic stations primarily for monitoring the global seismicity but also to study the dynamics of the Earth’s interior. With the increasing amount of data, it becomes clear that three dimensional models of the Earth’s interior are required to fit the data and that we might have a chance to identify the ongoing dynamics of the Earth in much greater detail. This requires new mathematical modeling and wave form inversion techniques for three dimensional Earth models, which are now the frontiers of computational seismology.
    Language: German
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  • 8
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    In:  System Erde
    Publication Date: 2020-02-12
    Description: Seismology is often associated with the investigation of earthquake processes and indeed this is a very important target of the science. However, seismology is also the primary means by which we can obtain images of the internal structure of the Earth on all scales, ranging from the deep interior, i.e. the Earth’s core and lower mantle over the mantle lithosphere and crust, the scale at which plate tectonics ‘happens’ all the way to the unconsolidated material in the near-surface. Seismology uses earthquakes and artificial sources as signal generators but also the ambient background wavefield, previously considered to be merely noise. Methodological and instrumental innovations have allowed ever more detailed investigations of the earthquake process and the seismic structure, and opened up new targets such as as the monitoring of geomorphological events and investigations of the time-dependency of seismic structure. Finally seismology is not restricted to waveform analysis and the instrumental period but draws on historical data and, in the field of paleoseismology, geological markers to constrain seismic activity in the pre-instrumental past. Direct societal benefits from seismology accrue for example from improved seismic hazard estimates and early-warning technologies in the area of natural hazards, from improved recovery and usage of natural resources, including geothermal energy as a sustainable energy source and much more, e.g. the possibility to monitor and thus enforce compliance with the nuclear test ban treaty.
    Language: German
    Type: info:eu-repo/semantics/article
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  • 9
    Publication Date: 2020-02-12
    Description: Im Juni 2011 fand ein Fest-Kolloquium für Prof. Dr. Rainer Kind statt. Langjährige Kollegen berichteten in Vorträgen über die gemeinsame Laufbahn und Freundschaft zu dem Seismologen mit dem verschmitzen Humor. Abgerundet wurde die Veranstaltung mit einem Dokumentarfilm seiner Söhne über den Astronomen Ernst von Rebeur-Paschwitz (RP), der 1889 auf dem Telegrafenberg als erster ein Fernbeben bei Japan aufzeichnete und als einer der Begründer der modernen Seismologie gilt.
    Language: German
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  • 10
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    In:  System Erde
    Publication Date: 2020-02-12
    Language: German
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  • 11
    Publication Date: 2020-02-12
    Language: German
    Type: info:eu-repo/semantics/other
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  • 12
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2021-01-28
    Language: German
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  • 13
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2021-01-28
    Language: German
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  • 14
    Call number: 21/SR 90.0917(64) ; 21/SR 22.19544(64)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr.64
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Diagramme, Illustrationen, Fotos, Karten , 30 cm
    Edition: Als Manuskript gedruckt
    ISSN: 0514-8790
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 64
    Language: German
    Note: Vorwort Adlung, A. Die Entwicklung der Fernübertragung in der Seismologie und Seismik Bormann, P. : Der Beitrag Immanuel KANTs zur Entwicklung wissenschaftlicher Vorstellungen über die Natur der Erdbeben Elstner, C. : Beiträge von Erdgezeitenuntersuchungen zu Vorstellungen über die Struktur des Erdkörpers Germann, D. : Die seismische Station an der Universität Jena und die Neugründung einer deutschen Zentralstation für Erdbebenforschung 1923 Heckeler, V. : Registrierung und Auswertung von Erdbebenwechselwellen zur Erforschung des Tiefbaus der Erdkruste Hurtig, E. Ernst August v. Rebeur-Paschwitz und seine Bedeutung für die Entwicklung der Seismologie Kessler, J. ; Rotter, D. : Entwicklung der Untersuchung und Bekämpfung von Gas-Salz-Ausbrüchen in der DDR Kowalle, G. : Entwicklung der Vorstellungen über den Bau des Erdinnern Kozâk, J. ; Schmidt P. : Abbildungen seismologischen Inhalts in europäischen Drucken des 15. bis 18. Jahrhunderts Kühn, P. : Zur Geschichte der Erforschung der Seismotektonik des Nordatlantik Meinhold, R. : Von den Anfängen der angewandten Seismik in Deutschland Meyer, H. : Die Erdbebenstation Leipzig (1902 - 1934) Meyer, H. ; Jacobs, F. : Zur Entwicklung der Angewandten Seismik an der Karl-Marx-Universität Leipzig Neunhöfer, H. ; Weidermann, V. : Seismische Überwachung von Bergbaugebieten, dargestellt am Beispiel der Mansfelder Mulde Pätz, H. : Zur Geschichte der Seismik beim Nachweis von Erdöl- und Erdgaslagerstätten - Versuch einer gesellschaftsbezogenen Wichtung Reinhardt, H.-G. : Zur Entwicklung der seismischen Erkundung im VEB Geophysik Savarenski, E. F. : Abriß der 60jährigen Entwicklung der sowjetischen Seismologie (1917 bis 1977) Schneider, M. M. : Über die Vorgeschichte der experimentellen Erdgezeitenforschung bis zum Ausgang des 19. Jahrhunderts ( Zusammenfassung) Sponheuer, W. ; Grünthal, G. : Das Mitteldeutsche Erdbeben vom 6. März 1872 Teupser, Ch. : Seismologische Forschungen in Jena seit 1923 Tittel, B. : Fortschritte des seismologischen Meßprogramms am Geophysikalischen Observatorium Collm (Zusammenfassung) Wilsdorf, H. ; Schmidt, P. : Erdbebentheorien und Prodigia in der griechisch-römischen Antike und einige Aspekte ihrer Rezeption in späterer Zeit
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 15
    Call number: 10.2312/zipe.1981.064
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 64
    Type of Medium: 12
    Pages: 1 Online-Ressource (218 Seiten) , Diagramme, Illustrationen, Fotos, Karten
    ISSN: 0514-8790
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 64
    Language: German
    Note: Vorwort Adlung, A. Die Entwicklung der Fernübertragung in der Seismologie und Seismik Bormann, P. : Der Beitrag Immanuel KANTs zur Entwicklung wissenschaftlicher Vorstellungen über die Natur der Erdbeben Elstner, C. : Beiträge von Erdgezeitenuntersuchungen zu Vorstellungen über die Struktur des Erdkörpers Germann, D. : Die seismische Station an der Universität Jena und die Neugründung einer deutschen Zentralstation für Erdbebenforschung 1923 Heckeler, V. : Registrierung und Auswertung von Erdbebenwechselwellen zur Erforschung des Tiefbaus der Erdkruste Hurtig, E. Ernst August v. Rebeur-Paschwitz und seine Bedeutung für die Entwicklung der Seismologie Kessler, J. ; Rotter, D. : Entwicklung der Untersuchung und Bekämpfung von Gas-Salz-Ausbrüchen in der DDR Kowalle, G. : Entwicklung der Vorstellungen über den Bau des Erdinnern Kozâk, J. ; Schmidt P. : Abbildungen seismologischen Inhalts in europäischen Drucken des 15. bis 18. Jahrhunderts Kühn, P. : Zur Geschichte der Erforschung der Seismotektonik des Nordatlantik Meinhold, R. : Von den Anfängen der angewandten Seismik in Deutschland Meyer, H. : Die Erdbebenstation Leipzig (1902 - 1934) Meyer, H. ; Jacobs, F. : Zur Entwicklung der Angewandten Seismik an der Karl-Marx-Universität Leipzig Neunhöfer, H. ; Weidermann, V. : Seismische Überwachung von Bergbaugebieten, dargestellt am Beispiel der Mansfelder Mulde Pätz, H. : Zur Geschichte der Seismik beim Nachweis von Erdöl- und Erdgaslagerstätten - Versuch einer gesellschaftsbezogenen Wichtung Reinhardt, H.-G. : Zur Entwicklung der seismischen Erkundung im VEB Geophysik Savarenski, E. F. : Abriß der 60jährigen Entwicklung der sowjetischen Seismologie (1917 bis 1977) Schneider, M. M. : Über die Vorgeschichte der experimentellen Erdgezeitenforschung bis zum Ausgang des 19. Jahrhunderts ( Zusammenfassung) Sponheuer, W. ; Grünthal, G. : Das Mitteldeutsche Erdbeben vom 6. März 1872 Teupser, Ch. : Seismologische Forschungen in Jena seit 1923 Tittel, B. : Fortschritte des seismologischen Meßprogramms am Geophysikalischen Observatorium Collm (Zusammenfassung) Wilsdorf, H. ; Schmidt, P. : Erdbebentheorien und Prodigia in der griechisch-römischen Antike und einige Aspekte ihrer Rezeption in späterer Zeit
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  • 16
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    Zentralinstitut Physik der Erde
    In:  Veröffentlichungen des Zentralinstituts Physik der Erde
    Publication Date: 2023-02-01
    Description: Vorwort Adlung, A. Die Entwicklung der Fernübertragung in der Seismologie und Seismik Bormann, P. : Der Beitrag Immanuel KANTs zur Entwicklung wissenschaftlicher Vorstellungen über die Natur der Erdbeben Elstner, C. : Beiträge von Erdgezeitenuntersuchungen zu Vorstellungen über die Struktur des Erdkörpers Germann, D. : Die seismische Station an der Universität Jena und die Neugründung einer deutschen Zentralstation für Erdbebenforschung 1923 Heckeler, V. : Registrierung und Auswertung von Erdbebenwechselwellen zur Erforschung des Tiefbaus der Erdkruste Hurtig, E. Ernst August v. Rebeur-Paschwitz und seine Bedeutung für die Entwicklung der Seismologie Kessler, J. ; Rotter, D. : Entwicklung der Untersuchung und Bekämpfung von Gas-Salz-Ausbrüchen in der DDR Kowalle, G. : Entwicklung der Vorstellungen über den Bau des Erdinnern Kozâk, J. ; Schmidt P. : Abbildungen seismologischen Inhalts in europäischen Drucken des 15. bis 18. Jahrhunderts Kühn, P. : Zur Geschichte der Erforschung der Seismotektonik des Nordatlantik Meinhold, R. : Von den Anfängen der angewandten Seismik in Deutschland Meyer, H. : Die Erdbebenstation Leipzig (1902 - 1934) Meyer, H. ; Jacobs, F. : Zur Entwicklung der Angewandten Seismik an der Karl-Marx-Universität Leipzig Neunhöfer, H. ; Weidermann, V. : Seismische Überwachung von Bergbaugebieten, dargestellt am Beispiel der Mansfelder Mulde Pätz, H. : Zur Geschichte der Seismik beim Nachweis von Erdöl- und Erdgaslagerstätten - Versuch einer gesellschaftsbezogenen Wichtung Reinhardt, H.-G. : Zur Entwicklung der seismischen Erkundung im VEB Geophysik Savarenski, E. F. : Abriß der 60jährigen Entwicklung der sowjetischen Seismologie (1917 bis 1977) Schneider, M. M. : Über die Vorgeschichte der experimentellen Erdgezeitenforschung bis zum Ausgang des 19. Jahrhunderts ( Zusammenfassung) Sponheuer, W. ; Grünthal, G. : Das Mitteldeutsche Erdbeben vom 6. März 1872 Teupser, Ch. : Seismologische Forschungen in Jena seit 1923 Tittel, B. : Fortschritte des seismologischen Meßprogramms am Geophysikalischen Observatorium Collm (Zusammenfassung) Wilsdorf, H. ; Schmidt, P. : Erdbebentheorien und Prodigia in der griechisch-römischen Antike und einige Aspekte ihrer Rezeption in späterer Zeit
    Language: German
    Type: info:eu-repo/semantics/book
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  • 17
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    Zentralinstitut Physik der Erde
    In:  Veröffentlichungen des Zentralinstituts Physik der Erde
    Publication Date: 2021-01-25
    Language: German
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  • 18
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    Deutsches GeoForschungsZentrum GFZ
    In:  System Erde
    Publication Date: 2022-01-28
    Language: German
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  • 19
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    Deutsches GeoForschungsZentrum GFZ
    In:  System Erde
    Publication Date: 2022-01-28
    Language: German
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  • 20
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2020-02-12
    Language: German
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  • 21
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2020-02-12
    Language: German
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  • 22
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2020-02-12
    Language: German
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  • 23
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    Deutsches GeoForschungsZentrum GFZ
    Publication Date: 2020-02-12
    Description: Die vorliegende Ausgabe des GFZ-Journals „System Erde“ soll einen Einblick in die am GFZ betriebene Forschung zur Seismologie geben.
    Language: German
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  • 24
    Publication Date: 2020-02-12
    Description: Significant scientific findings are often directly related to innovations in measurement technology. For investigating the Earth’s interior the invention of the seismography played the most important role. Starting with the first seismograph suitable for scientific investigations by Ewing, Gray and Milne in the 1870s and its improvement by Wiechert around 1900, seismic instrumentation was available in the beginning of the last century to reveal the layered structure of our planet. Since then, instruments were steadily improved, and controlled source experiments and seismic networks significantly contribute today to our understanding of the Earth’s structure and the ongoing dynamic processes as well as to the exploration of resources as oil, gas, water and minerals. At the GFZ German Research Centre for Geosciences we work on technical innovations and apply them in experiments around the world and at a variety of scales. We develop highly portable, low-cost, high-performance seismic data recording systems, which are designed to be used in “large-N” array configurations (〉1000 receivers) and on the sea floor (shallow water). Distributed accoustic sensors (DAS) based on fibre-optic cables allow extremely dense sampling of the seismic wavefields. Seismic sources and receivers integrated in borehole tools illuminate in high-resolution the subsurface during drilling operations (Seismic prediction while drilling, SPWD).
    Language: German
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  • 25
    Publication Date: 2022-05-18
    Language: German
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  • 26
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    In:  Beiträge zur Geophysik : Zeitschrift für physikalische Erdkunde
    Publication Date: 2020-02-12
    Language: German
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  • 27
    Publication Date: 2020-02-12
    Language: German
    Type: info:eu-repo/semantics/other
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