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  • 1
    Monograph available for loan
    Monograph available for loan
    Basel [u.a.] : Birkhäuser
    Call number: M 05.0594
    Type of Medium: Monograph available for loan
    Pages: S. 235-731 : Ill., graph. Darst.
    ISBN: 3764360496
    Series Statement: Pageoph topical volumes
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Keywords: Comprehensive Nuclear-Test-Ban Treaty ; CTBT ; crustal structure ; monitoring ; wave propagation
    Description / Table of Contents: On September 1996, the United Nations General Assembly adopted the Comprehensive Nuclear-Test-Ban Treaty (CTBT), prohibiting nuclear explosions worldwide, in all environments. The treaty calls for a global verification system, including a network of 321 monitoring stations distributed around the globe, a data communications network, an international data center (IDC), and on-site inspections to verify compliance. Successful monitoring of a CTBT requires that we detect and identify all nuclear explosions. Since many events of concern will be too small to be detected teleseismically, this capability requires the use of regional-distance seismograms. The complexity of regional seismograms presents many technical challenges for a monitoring program. This issue focuses on problems associated with regional wave propagation through complex media. It includes papers that investigate regional variations of elastic and anelastic properties of Eurasia, the blockage of regional phases by sedimentary basins, methods for modeling regional wave propagation and for calibrating seismic wave paths in order to extract amplitude variations and source parameters. These papers illustrate the research and development necessary for acquiring an understanding of regional wave propagation which in turn provides the foundation for operational tools used to monitor a CTBT.
    Pages: Online-Ressource (V, 211 Seiten)
    ISBN: 9783764365509
    Language: English
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  • 3
    Unknown
    Basel, Boston, Berlin : Birkhäuser
    Keywords: geodynamics ; seismology
    Description / Table of Contents: Variations in seismic Q are sensitive to a much greater extent than are seismic velocity variations on factors such as temperature, fluid content, and the movement of solid state defects in the earth. For that reason an understanding of Q and its variation with position in the earth and with time should provide information in earth's tectonic evolution, as well as on aspects of its internal structure. Progress in understanding Q has suffered from difficulty in obtaining reliable amplitude data at global and temporary stations. Moreover, laboratory determinations of Q, until recently, were most often made at frequencies much higher than those measured by seismologists for waves propagating through the earth. Recent advances in seismic station distribution and quality, as well as in methodology at both high and low fequencies, have greatly improved the quality of observational data available to seismologists from global stations. Concurrent advances have been made in measuring Q using laboratory samples at frequencies that pertain to the earth and in theoretical understanding of seismic wave attenuation. Papers of this volume present new information on Q in the earth from several perspectives: methodology, results from global and regional observations of both body and surface waves, laboratory measurements, and theoretical understanding. The editors believe that we have reached a new threshold in Q studies and that advances in data quality and methodology will spur increased interest in this difficult, but interesting field.
    Pages: Online-Ressource (496 Seiten)
    ISBN: 9783764360498
    Language: English
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 98 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The velocity structure of two regions of Turkey are determined using single-station measurements of Rayleigh and Love wave group velocities in the period range 8–50 s. A differential inversion scheme yields models for Turkey in which crustal and upper mantle shear-wave velocities are slower than those of most of Europe. Comparisons of upper mantle shear-wave velocities we have obtained with reported Pn velocities leads to Poisson's ratio values in the upper mantle between 0.29 and 0.30 for eastern Turkey and between 0.27 and 0.31 for western Turkey. Crustal velocities are slightly slower and upper mantle velocities are slightly faster in western Turkey than in eastern Turkey. The crust-mantle boundary obtained in our studies is gradational, but if a shear velocity of 4.2 km s–1 is taken to define the upper mantle then the crust appears to be about 40 km thick throughout all of Turkey. A sharp crust-mantle boundary may occur, but cannot be resolved. The data of this study require neither a low-velocity zone in the upper mantle nor polarization anisotropy in the crust or upper mantle. Azimuthal variations of Rayleigh and Love wave group velocities in western Turkey are consistent with velocities predicted by an azimuthally anisotropic upper crust in which vertical cracks are orientated in an approximate E-W direction. This interpretation is consistent with geological information, fault-plane solutions, lineations mapped from satellite observations, and reported heat flow values, but the possibility that these variations are caused by lateral changes of velocity in the crust of western Turkey cannot be completely ruled out at the present time.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 116 (1994), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: A combined inversion/forward modelling procedure, in which the frequency dependence of shear-wave internal friction (Qμ-1) is allowed to vary with depth, was developed and applied to selected Rayleigh wave and Lg attenuation data in the Basin and Range Province of the south-western United States. Both Q and the frequency dependence of Lg waves were used to constrain the models. Many models can explain Rayleigh wave and Lg data sets within their uncertainties, but at 1 Hz most have low values of Qμ (50-80) in the upper 8 km of the crust, rapidly increasing values to about 1000 at mid-crustal depths, and decreasing values at greater depths. Models which include a layer of higher Q values (80-150) in the upper few kilometres of the crust, overlying a region of lower Q values, cannot be precluded by the attenuation data of this study. Assuming that Qμ varies with frequency as fζ, models for which the frequency dependence is low (ζ= 0.0-0.1) in the upper crust best explain the data of this study. In the lower crust that frequency dependence is not well determined, but the models which best explain both the fundamental-mode and Lg data and produce realistic models of Qμ are characterized at 1 Hz by high values of both Qμ and its frequency dependence. Because of that frequency dependence Qμ may be an order of magnitude lower at a period of 100 s (∼ 100) than it is at 1 s (∼ 1000). Investigations of the effects of changing crustal velocity on values for Lg Q and its frequency dependence indicate that realistic velocity changes cause only small changes in those values and thus are inconsequential to our results.The low Qμ values, and their constancy with frequency, in the uppermost crust can be explained by fluid flow in a network of cracks in brittle rock. Increasing Qμ with depth to 10-15 km can be explained by the closing of those cracks due to pressure and their enhanced healing with increasing temperature. Plastic flow at greater depths may contribute further to the dissipation of cracks and to further increases in Qμ. Decreasing Qμ values at greater depths can be explained as being the result of increasing temperature, increasing content of partial melt, enhanced dislocation motion or some combination of these effects.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Westerville, Ohio : American Ceramics Society
    Journal of the American Ceramic Society 85 (2002), S. 0 
    ISSN: 1551-2916
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Physics
    Notes: Mixed-conducting Sr-Fe-Co oxides have potential applications in dense ceramic membranes for high-purity oxygen separation and/or methane conversion to produce syngas (CO + H2), because of their combined high electronic/ionic conductivity and significant oxygen permeability. SrFeCo0.5Oy has been synthesized by the solid-state reaction method. Conductivities were measured at elevated temperatures in various gas environments and increased as temperature and oxygen partial pressure (pO2) increased in the surrounding environment. Neutron powder diffraction experiments revealed that in a high pO2 environment the SrFeCo0.5Oy material consists of three different phases. The relative concentration of each component phase is dependent on temperature and pO2 in the surrounding environment. In air, Sr2(Fe, Co)3Oy (236-phase) is the majority phase and consists of 〉75 wt% of the total, whereas the perovskite and rocksalt phases account for ∼20 and 〈5 wt%, respectively. However, in a reducing environment, the 236-phase decomposes and converts to perovskite and rocksalt phase at high temperature. In an environment of pO2 〈 10−12.2 atm, the 236-phase is completely converted into perovskite (brownmillerite) and rocksalt phases.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 123 (1985), S. 487-498 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 118 (1980), S. 831-845 
    ISSN: 1420-9136
    Keywords: Surface-wave seismology ; Attenuation of Rayleigh waves ; Eastern Pacific Ocean
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Seismograms recorded for five earthquakes on the east Pacific rise have been analyzed to obtain the attenuation coefficients of the fundamental Rayleigh mode for the eastern Pacific in the 15–110 second period range. The attenuation coefficients have been obtained using two new methods, a reference-station method, and an iterative method by which the seismic moment and regionalized attenuation coefficient values are obtained simultaneously after considering the effect of the source directivity and time-function. The reference-station method was applied to the entire eastern Pacific, excluding paths along the east Pacific rise. When using the iterative method we divided the eastern Pacific into three sub-regions, designated as the north-eastern Pacific, the Nazca plate and the east Pacific rise. Although much scatter is present, the data suggest that attenuation coefficients for the Nazca plate are higher than those for the northeastern Pacific, and both are substantially higher than average values obtained for the entire Pacific Ocean. Two paths that lie along or near the east Pacific rise are characterized by especially high attenuation coefficients. These values suggest that a low-Q zone exists beneath that narrow feature.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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