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  • 21
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    In:  J. Geophys. Res., Stockholm, Wissenschaftliche Buchgesellschaft, vol. 101, no. 8, pp. 17,771-17,794, pp. L11308, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Earth model, also for more shallow analyses ! ; Rheology ; Attenuation ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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  • 22
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    In:  Bull. Seism. Soc. Am., Stockholm, Wissenschaftliche Buchgesellschaft, vol. 82, no. 8, pp. 454-480, pp. L11308, (ISSN: 1340-4202)
    Publication Date: 1992
    Keywords: Modelling ; Rheology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Inelastic ; Earthquake ; BSSA
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  • 23
    Publication Date: 1998-01-22
    Description: Space geodetic data recorded rates and directions of motion across the convergent boundary zone between the oceanic Nazca and continental South American plates in Peru and Bolivia. Roughly half of the overall convergence, about 30 to 40 millimeters per year, accumulated on the locked plate interface and can be released in future earthquakes. About 10 to 15 millimeters per year of crustal shortening occurred inland at the sub-Andean foreland fold and thrust belt, indicating that the Andes are continuing to build. Little (5 to 10 millimeters per year) along-trench motion of coastal forearc slivers was observed, despite the oblique convergence.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Norabuena -- Leffler-Griffin -- Mao -- Dixon -- Stein -- Sacks -- Ocola -- Ellis -- New York, N.Y. -- Science. 1998 Jan 16;279(5349):358-62.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉E. Norabuena, Instituto Geofisico del Peru, Apartado 3747, Lima 100, Peru, and Rosenstiel School for Marine and Atmospheric Sciences, University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149, USA. L. Leffler-Griffin and S. Stein, Departme.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9430582" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 24
    Publication Date: 2009-06-12
    Description: The first reports on a slow earthquake were for an event in the Izu peninsula, Japan, on an intraplate, seismically active fault. Since then, many slow earthquakes have been detected. It has been suggested that the slow events may trigger ordinary earthquakes (in a context supported by numerical modelling), but their broader significance in terms of earthquake occurrence remains unclear. Triggering of earthquakes has received much attention: strain diffusion from large regional earthquakes has been shown to influence large earthquake activity, and earthquakes may be triggered during the passage of teleseismic waves, a phenomenon now recognized as being common. Here we show that, in eastern Taiwan, slow earthquakes can be triggered by typhoons. We model the largest of these earthquakes as repeated episodes of slow slip on a reverse fault just under land and dipping to the west; the characteristics of all events are sufficiently similar that they can be modelled with minor variations of the model parameters. Lower pressure results in a very small unclamping of the fault that must be close to the failure condition for the typhoon to act as a trigger. This area experiences very high compressional deformation but has a paucity of large earthquakes; repeating slow events may be segmenting the stressed area and thus inhibiting large earthquakes, which require a long, continuous seismic rupture.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Liu, ChiChing -- Linde, Alan T -- Sacks, I Selwyn -- England -- Nature. 2009 Jun 11;459(7248):833-6. doi: 10.1038/nature08042.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute for Earth Sciences, Academica Sinica, 128 Sinica Road, Sec. 2, Nankang, Taipei 115, Taiwan, China. liucc@sinica.edu.tw〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19516339" 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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  • 25
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 100 (1990), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: A significant correlation is found, in both space and time, between the intraplate (land) and interplate (sea, thrust zone only) earthquakes in Tohoku, NE Japan that has persisted since the times of reliably reported events in AD 1600. the correlation peaks at a land-lead of about 36 yr with an average correlation distance of 200km, with the implication of an average strain migration rate of 5.6 km yr-1. the correlation is highly significant (〉 99 per cent), both from formal statistics and from tests of random shuffles of the data. Additional analysis of the data, as a point process, confirms the results of the correlation analysis. the sharpness of the correlation peak, when compared to the individual times of occurrence of the land and sea events suggests a trigger mechanism.To explain the correlation, the general model ofsubduction-rupture-rebound is extended to include additional features; the buckling of the land plate from the force of the subducting slab, and the viscoelastic coupling of the plate to the underlying asthenosphere. A buckle produces a high-stress region in the continental plate where earthquakes are more prone to occur, thus producing the spatial correlation in the data. This may also explain the preferred location on land for the smaller modern-day seismic events in NE Japan. the viscoelastic coupling controls the interaction between the land and sea events, resulting in the temporal correlation in the data. Because of viscosity, the model equations are diffuse-like with strain pulses as solutions; thus from the inferred strain migration rate it is possible to estimate asthenospheric viscosity (η=7 × 1018Pa s) using this model. A large land shock generates a strain pulse that affects the locked fault at the thrust zone several decades later. As the continental plate tends to pull away from the subducting slab, the frictional force arising from the overburden pressure is reduced, thus unlocking the fault and triggering a sea earthquake.The viscoelastic model is also used to explain surface deformations measured by triangulation surveys in Japan in 1904 and 1964. Horizontal displacements, which we believe are surface manifestations of the strain pulse from the large 1896 Riku-U land shock (M= 7.5) in NE Japan, are fit well by the model and provide a viscosity estimate η= 13 × 1018 Pa s.
    Type of Medium: Electronic Resource
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  • 26
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 99 (1989), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Observations of underside P-wave reflections from discontinuities deep within the upper mantle which precede the P'P’ phase have provided important constraints on the existence and physical properties of these dynamically critical features. In this study, we extend earlier work by examining for the first time, broad-band recordings of those earthquakes for which one would expect to observe P'P’ and its associated precursors P'dP’. An exhaustive search of 20 yr of Carnegie data and 11 yr of Gräfenberg data uncovered a number of fine P‘P’ observations, but in only one or perhaps two instances are there evidence of a precursor from near 670 km depth. These null results are consistent with what has been reported in earlier studies and provide us with an opportunity to estimate the variability of P velocity near 670 km or, alternatively, the scale length of discontinuity topography which acts to defocus the precursor. This has been done by using the reflectivity and Gaussian beam methods to compute synthetic seismograms for a suite of 1-D and 2-D earth models which vary slightly from PREM. We find that the null data may be satisfied either by (i) reducing the PREM impedance jump at 670 km from 8.5 to 4-5 per cent; (ii) smoothing this 8.5 per cent jump linearly over a zone 15-30 km thick or (iii) imposing deformations in the 670 km discontinuity as small as 10 km in amplitude and 300 km in wavelength. For the one case of an observed precursor, the relative size of the underside reflection and main P‘P’ phase suggests that, in this instance, the precursor's amplitude is correctly predicted by PREM.
    Type of Medium: Electronic Resource
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  • 27
    Publication Date: 2013-04-09
    Electronic ISSN: 1683-1470
    Topics: Computer Science
    Published by Ubiquity Press
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  • 28
    Publication Date: 1979-11-10
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 29
    Publication Date: 1957-06-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 30
    Publication Date: 1977-05-10
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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