ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 1
    Publication Date: 2017-08-26
    Description: In this article, we evaluate the ground-motion prediction equations (GMPEs) described by Atkinson (2015) and Shahjouei and Pezeshk (2016) with ground-motion data collected from the central and eastern United States (CEUS). The former GMPE was developed for small-to-moderate events at short hypocentral distances with application to induced earthquakes in eastern North America, using the ground-motion database developed by the Next Generation Attenuation-West2 (NGA-West2) project ( Bozorgnia et al. , 2014 ). The latter GMPE was developed for the central and eastern North America for the NGA-East project ( Frankel, 2015 ). We compare spectral amplitudes from 46,178 ground-motion recordings at 1069 stations from 2873 earthquakes in the CEUS to the GMPEs. The ground-motion catalog is divided into potentially-induced and tectonic earthquakes using the classification scheme of Petersen et al. (2015) , and their differences in geometric spreading are observed. We observe that the Atkinson (2015) GMPE is a good fit for ground motions at hypocentral distances of less than 60 km, and that the Shahjouei and Pezeshk (2016) GMPE captures the geometric spreading of ground motions at larger distances, for both induced and tectonic earthquakes.
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 1997
    Keywords: Seismology ; Seismicity ; Fault zone ; Fluids ; 7230 ; Seismology ; Seismicity ; and ; seismotectonics ; 7205 ; Continental ; crust ; (1242) ; 8110 ; Tectonophysics ; Two-dimensional ; GRL ; Continental ; tectonics ; general ; (0905)
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    In:  Eos, Trans., Am. Geophys. Un., London, AGU, vol. 77, no. 6, pp. 45, 57, 58, pp. L10304, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Seismics (controlled source seismology) ; Fault zone ; Seismology ; Velocity depth profile
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    In:  Eos, Trans., Am. Geophys. Un., Zagreb, Conseil de l'Europe, vol. 75, no. 12, pp. 137, pp. B10401, (ISSN 0343-5164)
    Publication Date: 1994
    Keywords: Review article ; Borehole geophys. ; Project report/description
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    U. S. Geological Survey
    In:  Circular No. 1031, 34 pp., New Orleans, Louisiana, U. S. Geological Survey, vol. C 560, 183 pp., no. PNL-CC-1801 171, pp. 977-992, (ISBN 3-933346-037)
    Publication Date: 1989
    Keywords: Instruments ; Seismology ; Review article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2013-12-07
    Description: [1]  We perform a retrospective forecast test using Northern California seismicity for the period between 1980 and 2009. We compare 7 realizations of the short-term clustering epidemic-type aftershock sequence (ETAS) model, and 21 models combining Coulomb stress change calculations and rate/state theory (CRS) to forecast seismicity rates in 10-day time intervals. We employ a common learning phase (1974–1980) for CRS models to ensure consistency, and we evaluate the forecasts with log-likelihood statistics to detect any spatial inconsistency and compare the total numbers of forecast vs. observed events. We find that: (1) ETAS models are better forecasters of the spatial evolution in seismicity in the near-source region, (2) CRS models can compete with ETAS models away from the mainshock rupture, and for short periods after mainshocks, (3) CRS models with optimally oriented receiver fault planes perform better in the first few days after mainshocks, whereas mapped fault planes should be implemented for longer-term forecasting, and (4) CRS models based on shear stress change calculations have comparable performance with Coulomb stress change models, with the benefit of lesser parameters involved in stress calculations. We conclude that physics based and statistical forecast models are complimentary to each other, and that future forecasts should be based on statistical models for near-source regions, and physical models for longer periods and distances. However, the realization of the CRS models involves a number of critical parameters (reference seismicity rates, regional stress field, loading rates), which should be retrospectively tested to improve the predictive power of physics based models.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2009-06-19
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Zoback, Mark D -- Ellsworth, William -- Hickman, Stephen -- England -- Nature. 2009 Jun 18;459(7249):909. doi: 10.1038/459909c.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19536240" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2013-11-23
    Description: We report on results of an all-sky search for high-energy neutrino events interacting within the IceCube neutrino detector conducted between May 2010 and May 2012. The search follows up on the previous detection of two PeV neutrino events, with improved sensitivity and extended energy coverage down to about 30 TeV. Twenty-six additional events were observed, substantially more than expected from atmospheric backgrounds. Combined, both searches reject a purely atmospheric origin for the 28 events at the 4sigma level. These 28 events, which include the highest energy neutrinos ever observed, have flavors, directions, and energies inconsistent with those expected from the atmospheric muon and neutrino backgrounds. These properties are, however, consistent with generic predictions for an additional component of extraterrestrial origin.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉IceCube Collaboration -- Aartsen, M G -- Abbasi, R -- Abdou, Y -- Ackermann, M -- Adams, J -- Aguilar, J A -- Ahlers, M -- Altmann, D -- Auffenberg, J -- Bai, X -- Baker, M -- Barwick, S W -- Baum, V -- Bay, R -- Beatty, J J -- Bechet, S -- Becker Tjus, J -- Becker, K-H -- Benabderrahmane, M L -- BenZvi, S -- Berghaus, P -- Berley, D -- Bernardini, E -- Bernhard, A -- Bertrand, D -- Besson, D Z -- Binder, G -- Bindig, D -- Bissok, M -- Blaufuss, E -- Blumenthal, J -- Boersma, D J -- Bohaichuk, S -- Bohm, C -- Bose, D -- Boser, S -- Botner, O -- Brayeur, L -- Bretz, H-P -- Brown, A M -- Bruijn, R -- Brunner, J -- Carson, M -- Casey, J -- Casier, M -- Chirkin, D -- Christov, A -- Christy, B -- Clark, K -- Clevermann, F -- Coenders, S -- Cohen, S -- Cowen, D F -- Cruz Silva, A H -- Danninger, M -- Daughhetee, J -- Davis, J C -- Day, M -- De Clercq, C -- De Ridder, S -- Desiati, P -- de Vries, K D -- de With, M -- DeYoung, T -- Diaz-Velez, J C -- Dunkman, M -- Eagan, R -- Eberhardt, B -- Eichmann, B -- Eisch, J -- Ellsworth, R W -- Euler, S -- Evenson, P A -- Fadiran, O -- Fazely, A R -- Fedynitch, A -- Feintzeig, J -- Feusels, T -- Filimonov, K -- Finley, C -- Fischer-Wasels, T -- Flis, S -- Franckowiak, A -- Frantzen, K -- Fuchs, T -- Gaisser, T K -- Gallagher, J -- Gerhardt, L -- Gladstone, L -- Glusenkamp, T -- Goldschmidt, A -- Golup, G -- Gonzalez, J G -- Goodman, J A -- Gora, D -- Grandmont, D T -- Grant, D -- Gross, A -- Ha, C -- Haj Ismail, A -- Hallen, P -- Hallgren, A -- Halzen, F -- Hanson, K -- Heereman, D -- Heinen, D -- Helbing, K -- Hellauer, R -- Hickford, S -- Hill, G C -- Hoffman, K D -- Hoffmann, R -- Homeier, A -- Hoshina, K -- Huelsnitz, W -- Hulth, P O -- Hultqvist, K -- Hussain, S -- Ishihara, A -- Jacobi, E -- Jacobsen, J -- Jagielski, K -- Japaridze, G S -- Jero, K -- Jlelati, O -- Kaminsky, B -- Kappes, A -- Karg, T -- Karle, A -- Kelley, J L -- Kiryluk, J -- Klas, J -- Klein, S R -- Kohne, J-H -- Kohnen, G -- Kolanoski, H -- Kopke, L -- Kopper, C -- Kopper, S -- Koskinen, D J -- Kowalski, M -- Krasberg, M -- Krings, K -- Kroll, G -- Kunnen, J -- Kurahashi, N -- Kuwabara, T -- Labare, M -- Landsman, H -- Larson, M J -- Lesiak-Bzdak, M -- Leuermann, M -- Leute, J -- Lunemann, J -- Madsen, J -- Maggi, G -- Maruyama, R -- Mase, K -- Matis, H S -- McNally, F -- Meagher, K -- Merck, M -- Meures, T -- Miarecki, S -- Middell, E -- Milke, N -- Miller, J -- Mohrmann, L -- Montaruli, T -- Morse, R -- Nahnhauer, R -- Naumann, U -- Niederhausen, H -- Nowicki, S C -- Nygren, D R -- Obertacke, A -- Odrowski, S -- Olivas, A -- O'Murchadha, A -- Paul, L -- Pepper, J A -- Perez de los Heros, C -- Pfendner, C -- Pieloth, D -- Pinat, E -- Posselt, J -- Price, P B -- Przybylski, G T -- Radel, L -- Rameez, M -- Rawlins, K -- Redl, P -- Reimann, R -- Resconi, E -- Rhode, W -- Ribordy, M -- Richman, M -- Riedel, B -- Rodrigues, J P -- Rott, C -- Ruhe, T -- Ruzybayev, B -- Ryckbosch, D -- Saba, S M -- Salameh, T -- Sander, H-G -- Santander, M -- Sarkar, S -- Schatto, K -- Scheriau, F -- Schmidt, T -- Schmitz, M -- Schoenen, S -- Schoneberg, S -- Schonwald, A -- Schukraft, A -- Schulte, L -- Schulz, O -- Seckel, D -- Sestayo, Y -- Seunarine, S -- Shanidze, R -- Sheremata, C -- Smith, M W E -- Soldin, D -- Spiczak, G M -- Spiering, C -- Stamatikos, M -- Stanev, T -- Stasik, A -- Stezelberger, T -- Stokstad, R G -- Stossl, A -- Strahler, E A -- Strom, R -- Sullivan, G W -- Taavola, H -- Taboada, I -- Tamburro, A -- Tepe, A -- Ter-Antonyan, S -- Tesic, G -- Tilav, S -- Toale, P A -- Toscano, S -- Unger, E -- Usner, M -- van Eijndhoven, N -- Van Overloop, A -- van Santen, J -- Vehring, M -- Voge, M -- Vraeghe, M -- Walck, C -- Waldenmaier, T -- Wallraff, M -- Weaver, Ch -- Wellons, M -- Wendt, C -- Westerhoff, S -- Whitehorn, N -- Wiebe, K -- Wiebusch, C H -- Williams, D R -- Wissing, H -- Wolf, M -- Wood, T R -- Woschnagg, K -- Xu, D L -- Xu, X W -- Yanez, J P -- Yodh, G -- Yoshida, S -- Zarzhitsky, P -- Ziemann, J -- Zierke, S -- Zoll, M -- New York, N.Y. -- Science. 2013 Nov 22;342(6161):1242856. doi: 10.1126/science.1242856.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24264993" 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
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2015-02-24
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉McGarr, A -- Bekins, B -- Burkardt, N -- Dewey, J -- Earle, P -- Ellsworth, W -- Ge, S -- Hickman, S -- Holland, A -- Majer, E -- Rubinstein, J -- Sheehan, A -- New York, N.Y. -- Science. 2015 Feb 20;347(6224):830-1. doi: 10.1126/science.aaa0494.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉U.S. Geological Survey (USGS), Earthquake Science Center, Menlo Park, CA 94025, USA. mcgarr@usgs.gov. ; USGS, National Water Quality Assessment Program, Menlo Park, CA 94025, USA. ; USGS, Powell Center, Fort Collins, CO 80526, USA. ; USGS, Geologic Hazards Center, Golden, CO 80225, USA. ; U.S. Geological Survey (USGS), Earthquake Science Center, Menlo Park, CA 94025, USA. ; University of Colorado at Boulder, Boulder, CO 80302, USA. ; Oklahoma Geological Survey, Norman, OK 73069, USA. ; Lawrence Berkeley National Laboratory, Berkeley, CA, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25700505" target="_blank"〉PubMed〈/a〉
    Keywords: Disasters/*prevention & control/*statistics & numerical data ; Earthquakes/*statistics & numerical data ; Proportional Hazards Models ; Safety Management/methods ; United States ; Waste Disposal, Fluid/*methods
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2017-04-04
    Description: Six moderate magnitude earthquakes (5 〈 Mw 〈 6) ruptured normal fault segments of the southern sector of the North Apennine belt (central Italy) in the 1997 Colfiorito earthquake sequence. We study the progressive activation of adjacent and nearby parallel faults of this complex normal fault system using1650 earthquake locations obtained by applying a double-difference location method, using travel time picks and waveform cross-correlation measurements. The lateral extent of the fault segments range from 5 to 10 km and make up a broad,45 km long, NW trending fault system. The geometry of each segment is quite simple and consists of planar faults gently dipping toward SW with an average dip of 40–45. The fault planes are not listric but maintain a constant dip through the entire seismogenic volume, down to 8 km depth. We observe the activation of faults on the hanging wall and the absence of seismicity in the footwall of the structure. The observed fault segmentation appears to be due to the lateral heterogeneity of the upper crust: preexisting thrusts inherited from Neogene’s compressional tectonic intersect the active normal faults and control their maximum length. The stress tensor obtained by inverting the six main shock focal mechanisms of the sequence is in agreement with the tectonic stress active in the inner chain of the Apennine, revealing a clear NE trending extension direction. Aftershock focal mechanisms show a consistent extensional kinematics, 70% of which are mechanically consistent with the main shock stress field.
    Description: Published
    Description: 2294,
    Description: 3.1. Fisica dei terremoti
    Description: JCR Journal
    Description: reserved
    Keywords: Normal faulting ; double-difference ; Umbria-Marche ; corss-correlation ; relative location ; 05. General::05.02. Data dissemination::05.02.02. Seismological data
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...