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  • 11
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    In:  Tectonophysics, Taipei, Elsevier, vol. 6, no. 1, pp. 93-102, pp. RG2001, (ISBN: 0-12-018847-3)
    Publication Date: 1968
    Keywords: Anisotropy ; Lithosphere
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  • 12
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    In:  Geol. Soc. Am. Bull., Taipei, Elsevier, vol. 86, no. 1, pp. 227-236, pp. RG2001, (ISBN: 0-12-018847-3)
    Publication Date: 1975
    Keywords: P-waves ; Earth model, also for more shallow analyses ! ; Physical properties of rocks ; Laboratory measurements ; GSA
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  • 13
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    In:  Geophys. J. R. astr. Soc., Taipei, Elsevier, vol. 76, no. 1, pp. 89-111, pp. RG2001, (ISBN: 0-12-018847-3)
    Publication Date: 1984
    Keywords: Anisotropy ; Physical properties of rocks ; Geol. aspects ; Mineralogy ; petrology ; GJRaS
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  • 14
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    AGU
    In:  Bull., Polar Proj. OP-O3A4, Composition, Structure and Dynamics of the Lithosphere-Asthenosphere System, Washington, D.C., AGU, vol. 16, no. Subvol. a, pp. 111-123, (ISBN 0080419208)
    Publication Date: 1987
    Keywords: Review article ; Anisotropy ; Physical properties of rocks
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  • 15
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    CRC Handbook Phys. Prop. Rocks
    In:  Bonn, CRC Handbook Phys. Prop. Rocks, vol. 2, no. 3, pp. 2-203, (ISBN 0-19-513895-3)
    Publication Date: 1982
    Keywords: P-waves ; Shear waves ; Handbook of geophysics ; Physical properties of rocks ; Velocity
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  • 16
    Publication Date: 2009-01-06
    Description: Water and hydrous minerals play a key part in geodynamic processes at subduction zones by weakening the plate boundary, aiding slip and permitting subduction-and indeed plate tectonics-to occur. The seismological signature of water within the forearc mantle wedge is evident in anomalies with low seismic shear velocity marking serpentinization. However, seismological observations bearing on the presence of water within the subducting plate itself are less well documented. Here we use converted teleseismic waves to obtain observations of anomalously high Poisson's ratios within the subducted oceanic crust from the Cascadia continental margin to its intersection with forearc mantle. On the basis of pressure, temperature and compositional considerations, the elevated Poisson's ratios indicate that water is pervasively present in fluid form at pore pressures near lithostatic values. Combined with observations of a strong negative velocity contrast at the top of the oceanic crust, our results imply that the megathrust is a low-permeability boundary. The transition from a low- to high-permeability plate interface downdip into the mantle wedge is explained by hydrofracturing of the seal by volume changes across the interface caused by the onset of crustal eclogitization and mantle serpentinization. These results may have important implications for our understanding of seismogenesis, subduction zone structure and the mechanism of episodic tremor and slip.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Audet, Pascal -- Bostock, Michael G -- Christensen, Nikolas I -- Peacock, Simon M -- England -- Nature. 2009 Jan 1;457(7225):76-8. doi: 10.1038/nature07650.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada. paudet@berkeley.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19122639" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 17
    Publication Date: 2012-08-07
    Description: Polarization and splitting analyses of minute-long windows of non-volcanic tremor at 3-component stations in the vicinity of southern Vancouver Island provide new evidence for the presence of anisotropy within the crustal portion of the North American plate beneath Cascadia. As reported previously, tremor particle motions are predominantly horizontal and inferred to manifest an upgoing wavefield composed primarily of S-waves. Under this assumption, estimates of incidence angle and back azimuth can be deduced from orientation of the smallest principle direction of motion. When subjected to standard S-wave splitting analysis, most stations yield systematic and reproducible fast polarization directions. Estimates of original polarization direction are more scattered and splitting times often exhibit multimodal distributions. Numerical simulations, wherein band-limited synthetic seismograms comprising contributions from multiple sources are analyzed for splitting, neatly reproduce these characteristics and thereby provide a framework for interpretation. A number of stations in our study sit astride the San Juan fault which, based on reflection studies, dips approximately 60 to 70° to the north. Underlying these stations is the Leech River Complex consisting of strongly foliated greenschist facies phyllites with steeply dipping foliations striking parallel to fast polarization directions of split S-waves. Detailed laboratory velocity measurements at elevated pressures show that as little as 2 to 3 km of vertically dipping Leech River phyllite are required to produce the observed splitting. These phyllites have some of the highest S-wave anisotropies measured to date and are part of a once continuous belt of anisotropic crust extending over 2000 km along the western North American coast from southern Vancouver Island to southwest Alaska.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 18
    Publication Date: 2017-01-12
    Description: We have recently suggested that the nearly constant duration of low frequency earthquakes (LFEs) (and, equivalently, the band-limitation of tectonic tremor) manifests a moment-duration scaling that is fundamentally different from regular earthquakes and is most easily explained as rupture on asperities of roughly constant dimension. In that work, we employed qualitative arguments against potential bias by attenuation. Here we examine the role of attenuation more quantitatively through an analysis that avoids specification of particular source ( e.g. , Brune) models and relies on the particle velocity spectral maximum as the definition of apparent corner frequency. The analysis leads to the formal definition of a saturation frequency as the limiting value of apparent corner frequency as the true corner frequency tends infinity. The saturation frequency, a formal equivalent to f m a x , can be used to set bounds on path-averaged quality factor Q . We apply these relations to deep crustal and intraslab earthquakes beneath Vancouver Island to estimate bulk crustal attenuation parameters that are subsequently used to correct apparent corner-frequency measurements of LFEs reported in our earlier work. The attenuation bias due to bulk crustal structure is shown to be small, with negligible effect on the principal conclusions of that study. However, a review of laboratory and seismic refraction measurements of attenuation in oceanic basalts and evidence for high P -to- S LFE corner frequency ratios raises the possibility that strong, highly localized, near-source attenuation accompanying high pore-fluid pressures could cause the bandlimited nature of LFEs through the depletion of high frequencies.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 19
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 237 (1972), S. 450-451 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Laboratory studies of seismic velocities in rocks7-8 show that many common crustal rocks are highly aniso^opic to compressional wave propagation, so it is plausible that in many regions the Earth's crust is anisotropic, and Dorman9 has recently presented seismic data which indicate anisotropy of ...
    Type of Medium: Electronic Resource
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  • 20
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 229 (1971), S. 549-550 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1 Oscilloscope traces for shear wave propagation through (a) slate from Poultney, Vermont, and (b) dunite from Twin Sisters Peaks, Washington. The transducers are oriented at 0 to receive the higher velocity shear wave. Rotation of the transducers through 90 emphasizes the first arrival of the ...
    Type of Medium: Electronic Resource
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