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  • 1
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    In:  Tectonophys., Amsterdam, Elsevier Scientific Publishing Company, vol. 277, no. 1-3, pp. 41-55, pp. 1012, (ISSN: 1340-4202)
    Publication Date: 1997
    Keywords: Laboratory measurements ; cracks and fractures (.NE. fracturing) ; Physical properties of rocks ; Geothermics ; Geochemistry ; diagenesis
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  • 2
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    In:  J. Geophys. Res., Kobe, Dec. 6-11, 1993, The Local Organizing Committee for the CRCM '93, vol. 101, no. 19, pp. 13,919-13,932, pp. TC6001, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Seismology ; Source ; Friction ; JGR
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  • 3
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    In:  J. Geophys. Res., Taipei, Elsevier, vol. 101, no. 2, pp. 313-328, pp. RG2001, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Earthquake precursor: prediction research ; Earthquake precursor: electrical ; JGR
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  • 4
    Publication Date: 2008-01-04
    Description: It remains unknown how the small strains induced by seismic waves can trigger earthquakes at large distances, in some cases thousands of kilometres from the triggering earthquake, with failure often occurring long after the waves have passed. Earthquake nucleation is usually observed to take place at depths of 10-20 km, and so static overburden should be large enough to inhibit triggering by seismic-wave stress perturbations. To understand the physics of dynamic triggering better, as well as the influence of dynamic stressing on earthquake recurrence, we have conducted laboratory studies of stick-slip in granular media with and without applied acoustic vibration. Glass beads were used to simulate granular fault zone material, sheared under constant normal stress, and subject to transient or continuous perturbation by acoustic waves. Here we show that small-magnitude failure events, corresponding to triggered aftershocks, occur when applied sound-wave amplitudes exceed several microstrain. These events are frequently delayed or occur as part of a cascade of small events. Vibrations also cause large slip events to be disrupted in time relative to those without wave perturbation. The effects are observed for many large-event cycles after vibrations cease, indicating a strain memory in the granular material. Dynamic stressing of tectonic faults may play a similar role in determining the complexity of earthquake recurrence.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Johnson, Paul A -- Savage, Heather -- Knuth, Matt -- Gomberg, Joan -- Marone, Chris -- England -- Nature. 2008 Jan 3;451(7174):57-60. doi: 10.1038/nature06440.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Geophysics Group EES-11, Los Alamos National Laboratory of the University of California, MS D443, Los Alamos, New Mexico 87545, USA. paj@lanl.gov〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18172496" 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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  • 5
    Publication Date: 2009-12-18
    Description: Geological and geophysical evidence suggests that some crustal faults are weak compared to laboratory measurements of frictional strength. Explanations for fault weakness include the presence of weak minerals, high fluid pressures within the fault core and dynamic processes such as normal stress reduction, acoustic fluidization or extreme weakening at high slip velocity. Dynamic weakening mechanisms can explain some observations; however, creep and aseismic slip are thought to occur on weak faults, and quasi-static weakening mechanisms are required to initiate frictional slip on mis-oriented faults, at high angles to the tectonic stress field. Moreover, the maintenance of high fluid pressures requires specialized conditions and weak mineral phases are not present in sufficient abundance to satisfy weak fault models, so weak faults remain largely unexplained. Here we provide laboratory evidence for a brittle, frictional weakening mechanism based on common fault zone fabrics. We report on the frictional strength of intact fault rocks sheared in their in situ geometry. Samples with well-developed foliation are extremely weak compared to their powdered equivalents. Micro- and nano-structural studies show that frictional sliding occurs along very fine-grained foliations composed of phyllosilicates (talc and smectite). When the same rocks are powdered, frictional strength is high, consistent with cataclastic processes. Our data show that fault weakness can occur in cases where weak mineral phases constitute only a small percentage of the total fault rock and that low friction results from slip on a network of weak phyllosilicate-rich surfaces that define the rock fabric. The widespread documentation of foliated fault rocks along mature faults in different tectonic settings and from many different protoliths suggests that this mechanism could be a viable explanation for fault weakening in the brittle crust.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Collettini, Cristiano -- Niemeijer, Andre -- Viti, Cecilia -- Marone, Chris -- England -- Nature. 2009 Dec 17;462(7275):907-10. doi: 10.1038/nature08585.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Geologia Strutturale e Geofisica, Dipartimento di Scienze della Terra Universita degli Studi di Perugia, 06100, Perugia, Italy. colle@unipg.it〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20016599" 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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  • 6
    Publication Date: 2006-09-23
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Marone, Chris -- Richardson, Eliza -- New York, N.Y. -- Science. 2006 Sep 22;313(5794):1748-9.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geosciences, Pennsylvania State University, University Park, PA 16802, USA. cjm38@psu.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/16990540" 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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  • 7
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2008-01-12
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Richardson, Eliza -- Marone, Chris -- New York, N.Y. -- Science. 2008 Jan 11;319(5860):166-7. doi: 10.1126/science.1152877.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy, and the Department of Geosciences, Pennsylvania State University, University Park, PA 16802, USA. eliza@geosc.psu.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18187646" 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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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 53 (1997), S. 123-126 
    ISSN: 1432-1041
    Keywords: Key wordsCeftriaxone ; Haemodialysis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Abstract Objective: The purpose of the present study was to investigate whether the clearance of ceftriaxone during haemodialysis is influenced by the type of membrane used (cuprophane, haemophane or polysulphone). Methods: After administration of a single 2-g dose of ceftriaxone, the half-life of the drug during haemodialysis and the clearance of the dialyser were measured. Results: The mean dialysis clearance normalised for square metre of membrane surface was significantly different for the three dialysers (haemophane 24  ml · min−1 · m−2; cuprophane 32 ml · min−1 · m−2; polysul phone 42 ml · min−1· m−2). Conclusions: Polysulphone membranes are more permeable and increase the extraction of ceftriaxone more than the other dialysers studied (haemophane and cuprophane membranes). These results, taken together with previous data, show that an increase of the dose in dialysis patients treated with large surface (〉0.8 m2) and high permeability membranes might be necessary.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2008-12-10
    Print ISSN: 0031-9007
    Electronic ISSN: 1079-7114
    Topics: Physics
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  • 10
    Publication Date: 2007-03-16
    Print ISSN: 0278-7407
    Electronic ISSN: 1944-9194
    Topics: Geosciences
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