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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10115
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dc.contributor.authorallRoselli, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2015-08-17T07:12:44Zen
dc.date.available2015-08-17T07:12:44Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/10115en
dc.description.abstractArray seismology is an useful tool to perform a detailed investigation of the Earth’s interior. Seismic arrays by using the coherence properties of the wavefield are able to extract directivity information and to increase the ratio of the coherent signal amplitude relative to the amplitude of incoherent noise. The Double Beam Method (DBM), developed by Krüger et al. (1993, 1996), is one of the possible applications to perform a refined seismic investigation of the crust and mantle by using seismic arrays. The DBM is based on a combination of source and receiver arrays leading to a further improvement of the signal-to-noise ratio by reducing the error in the location of coherent phases. Previous DBM works have been performed for mantle and core/mantle resolution (Krüger et al., 1993; Scherbaum et al., 1997; Krüger et al., 2001). An implementation of the DBM has been presented at 2D large-scale (Italian data-set for Mw=9.3, Sumatra earthquake) and at 3D crustal-scale as proposed by Rietbrock & Scherbaum (1999), by applying the revised version of Source Scanning Algorithm (SSA; Kao & Shan, 2004). In the 2D application, the rupture front propagation in time has been computed. In 3D application, the study area (20x20x33 km3), the data-set and the source-receiver configurations are related to the KTB-1994 seismic experiment (Jost et al., 1998). We used 60 short-period seismic stations (200-Hz sampling rate, 1-Hz sensors) arranged in 9 small arrays deployed in 2 concentric rings about 1 km (A-arrays) and 5 km (B-array) radius. The coherence values of the scattering points have been computed in the crustal volume, for a finite time-window along all array stations given the hypothesized origin time and source location. The resulting images can be seen as a (relative) joint log-likelihood of any point in the subsurface that have contributed to the full set of observed seismograms.en
dc.description.sponsorshipUniversità di Bolognaen
dc.language.isoEnglishen
dc.subjectCrustal scattering, induced seismicityen
dc.titleImaging of crustal scatterers using multiple seismic arraysen
dc.typethesisen
dc.description.statusUnpublisheden
dc.subject.INGV05. General::05.02. Data dissemination::05.02.02. Seismological dataen
dc.relation.referencesAki K. & Richards P.G. (1980).”Quantitative Seismology, Theory and Methods”. I and II, W. H. Freeman, New York. Arlitt R., Kissling E., Ansorge J. and TOR Working Group (1999).”3-D crustal structure beneath the TOR array and effects on teleseismic wavefronts”. Tectonophysics, 314, 309–319. Baisch S., Bohnhoff M., Ceranna L., Yimin Tu, Harjes H.-P. (2002).” Probing the crust to 9 km depth: fluid-injection experiments and induced seismicity at the KTB superdeep drilling hole, Germany”. Bull. Seismol. Soc. Am., 92, 2369–2380, doi:10.1785/0120010236. Bastow I., Stuart G., Kendall J., Ebinger C. (2005).”Upper-mantle seismic structure in a region of incipient continental breakup: northern Ethiopian rift”. Geophys. J. Int., 162, 479–493. Birtill J.W. & Whiteway F.E. (1965).”The application of phased arrays to the analysis of seismic body waves”. Phil. Trans. Royal Soc. of London, Math. and Phys. Sciences A-258 (1091) 421-493. Whiteway F.E.(1965).”The application of phased arrays to the analysis of seismic body waves”. Philos. Trans. R. Soc. London, Ser. A, 258, 421–493. Braun T., Schweitzer J., Azzara R.M., Piccinini D., Cocco M., Boschi E. (2004).”Results from the temporary installation of a small aperture seismic array in the Central Apennines and its merits for local event detection and location capabilities”. Annals of Geophys., 47 (5), 1557-1568. Braun T.; Dahm T.; Krüger F.; Ohrnberger M. & Scherbaum F. (2006).”Seismic array analysis of Tornillo-like signals recorded in Tuscany”. Atti 25° Convegno GNGTS. Braun T., Stammler K., Roselli P. (2007).”ELISA – Experimental Large Italian Seismic Array”. GNGTS Atti del 26° Convegno Nazionale-Riassunti estesi. Braun T. & Schweitzer J. (2008).” Spatial Noise-Field Characteristics of a Temporary Three- Component Small Aperture Array in Central Italy”. Bull. Seis. Soc. Am., 98, 1876–1886. Brudy M., Zoback M.D., Fuchs K., Rummel F. & Baumgärtner J. (1997).”Estimation of the complete stress tensor to 8 km depth in the KTB scientific drillholes implications for crustal strength”. J. Geophys. Res., 102, 18453-18475. Bondar I., North R., Beall G. (1999). Teleseismic slowness-azimuth station corrections for the international monitoring system seismic network. Bull Seismol Soc Am 89:989–1003. Büßelberg T., Harjes H.P., Knapmeyer M. (1995). “Source parameter of seismic events induced by fluid injection at 9 km depth in the KTB-borehole”. EOS, 76, no. 46/supplement, F559. Bungum H., Husebye E.S. & Ringdal F. (1971).”The NORSAR array and preliminary results of data analysis. Geoph. J. R. astr. Soc., 25, 115-126. Buttkus B. (1986).”Ten years of the Gräfenberg array: defining the frontiers of broadband seismology”. Geologisches Jahrbuch , E-35, Hannover, 135 pp. Capon J. (1969).”High-resolution frequency-wavenumber spectrum analysis”. Proc. IEEE, 57, 1408-1418.Castle J.C. and Creager K.C. (1999).”A steeply dipping discontinuity in the lower mantle beneath Izu-Bonin. J. Geophys. Res., 104, 7279–7292. Carpenter E. (1965).”A historical review of seismometer array development .Proc IEEE 53: 1816- 1821. Doi: 10.1109/PROC.1965.4452.Clouser R. & Langston C. (1995).”Modeling P-Rg conversions from isolated topographic features near the NORESS array”. Bull. Seismol. Soc. Am., 85,859–873. Crotwell H.P., Owens T.J., Ritsema J. (1999).”The TauP Toolkit: Flexible seismic travel-time and raypath utilities”. Seism. Res. Letters, 70, 154-170. Davies D., Kelly E., Filson J. (1971).”VESPA process for analysis of seismic signals”. Nat Phys. Sci. (Lond) 232, 8-13. Doornboos D.J. & Husebye E.S. (1972).”Array analysis of PKP phases and their precursors”. Phys. Earth Planet. Inter., 6, 387–399. Douglas A. (2002).”Seismometer arrays—Their use in earthquake and test ban seismology”. Handbook of Earthquake and Engineering Seismology, edited by P. Jennings, H. Kanamori, and W. Lee, 357–367, Academic, San Diego, Calif. Douglas A., Bowers D., Marshall P.D., Young J.B., Porter D., and Wallis N.J. (1999).”Putting nuclear-test monitoring to the test”. Nature, 398, 474–475. Douze E.J. & Laster S.J. (1979).”Statics of semblance”. Geophysics, 44, 1999-2003. Emmermann R. & Lauterjung J. (1997).”The German Continental Deep Drilling Program KTB: Overview and major results”. J. Geophys. Res., 102(B8), 18,179– 18,201. Friedrich A., Krüger F., Klinge K. (1998).”Ocean-generated microseismic noise located with the Grafenberg array”. J. Seismol., 2, 47–64. Frosch R.A. & Green P.E. Jr. (1966).”The concept of a large aperture seismic array”. Proc. Royal Soc., A-290, 368-384. Goldstein P., Walter W.R., Zandt G. (1992).”Upper mantle structure beneath central Eurasia using a source array of nuclear explosions and waveforms at regional distances”. J. Geophys. Res., 97, 14,097–14,115. Haykin S. (1985).”Array signal processing”. Englewood Cliffs, NJ, Prentice-Hall, Inc., 493 pp, AA(McMaster University, Hamilton, Canada). Harjes H.P. & Henger M. (1973).”Array-Seismologie”. Z. Geophs., 39, 865-905. Harjes H.P. & Seidl D. (1978).”Digital recording and analysis of broad-band seismic data at the Gräfenberg (GRF-) array”. J. Geophys., 44, 511-523. Harjes H.P., et al. (1997).”Origin and nature of crustal reflections: Results from integrated seismic measurements at the KTB super-deep drilling site”. J. Geophys. Res., 102(B8), 18,267– 18,288. Haubrich R. (1968).”Array design”. Bull. Seismol. Soc. Am., 58, 977-991.Henyey T. (2000).”Earthscope: a look into our continent”. Geotimes, 45, 5. Herrmann R.B. (1975).”A student's guide to the use of P and S-wave data for focal mechanism determination”. Earthquake Notes, 46, 29-39. Hirschmann G. (1996).”KTB—The structure of a Variscan terrane boundary: Seismic investigation-drilling-models”. Tectonophysics, 264, 327 –339. Ishii M., Shearer P.M., Houston H., Vidale J.E. (2005).”Extent, duration and speed of the 2004 Sumatra-Andaman earthquake imaged by the Hi-Net array”. Nature, 435, 933-936. Huang B.S. (2001).” Evidence for azimuthal and temporal variations of the rupture propagation of the 1999 Chi‐Chi, Taiwan Earthquake from dense seismic array observations”. Geophys. Res. Lett., 28 (17), 3377-3380. Husebye E.S. & Ruud B.O. (1989).”Array seismology—Past, present and future developments. Observatory Seismology, edited by Litehiser J. J. , 123–153, Univ. of Calif. Press, Berkeley. Johnson D.H., Dudgeon D.E. (1992).”Array signal processing: concepts and techniques”. Simon & Schuster, New York. Jost M.L., Büsselberg T., Jost Ö., Harjes H.P. (1998).”Source Parameters of injection-induced microearthquakes at 9 km depth at the KTB deep drilling site, Germany”. Bull Seis. Soc. Am., 88(3), 815-832. Kao H. & Shan S.-J. (2004).”The Source-Scanning-Algorithm: mapping the distribution of seismic sources in time and space”. Geophys. J. Int., 157, 589-594. Kao H., Shan S.-J., Dragert H., Rogers G., Cassidy J.F., Ramachandran K. (2005).”A wide depth distribution of seismic tremors along the northern Cascadia margin”. Nature, 436, 841-844. Kao H., Shan S.-J., Dragert H., Rogers G., Cassidy J.F., Wang K., James T.S., Ramachandran K. (2006).”Spatial-temporal patterns of seismic tremors in northern Cascadia”. J. Geophys. Res., 111, B03309, doi:10.1029/2005JB003727. Kao H. & Shan S.-J. (2007).”Rapid identification of earthquake rupture plane using Source- Scanning Algorithm”. Geophys. J. Int., 168, 1011–1020. Kárason H. & van der Hilst R.D. (2001).”Tomographic imaging of the lowermost mantle with differential times of refracted and diffracted core phases (PKP, Pdiff)”. J. Geophys. Res., 106, 6569– 6587. Kennett B.L.N., Engdahl E.R., Buland R. (1995).”Constraints on seismic velocities in the Earth from travel times”. Geophys. J. Int., 122, 108-124. Kelly E.J. (1967).”Response of seismic signals to wide-band signals”. Lincoln Lab. Tech. Note 1967, 30, Lincoln Lab., Mass. Inst. of Technol., Lexington, Mass. Kito T. & Krüger F. (2001).”Heterogeneities in D” beneath the south-western Pacific inferred from scattered and reflected P-waves”. Geophys. Res. Lett., 28, 2545–2548. Kito T., Krüger F. Negishi H. (2004).”Seismic heterogeneous structure in the lowermost mantle beneath the southwestern Pacific”. J. Geophys. Res., 109 (B9), B09304.Krüger F., Weber M. (1992).”The effect of low-velocity sediments on the mislocation vectors of the GRF array”. Geophys. J. Int., 108, 387–393. Krüger F., Weber M., Scherbaum F. & Schlittenhardt J. (1993).”Double beam analysis of anomalies in the core-mantle boundary region”. Geoph. Res. Lett., 20, 1475-1478. Krüger F., Scherbaum F., Weber M., Schlittenhardt J. (1996).”Analysis of asymmetric multipathing with a generalization of the double-beam method”. Bull. Seismol. Soc. Am., 86, 737–749. Krüger F., Baumann M., Scherbaum F. and Weber M. (2001).”Mid mantle scatterers near the Mariana slab detected with a double array method”. Geophys. Res. Lett., 28, 667–670. Krüger F & Ohrnberger M. (2005).”Tracking the rupture of the Mw9.2 Sumatra earthquake over 1150 km at teleseismic distances”. Nature, 435, 937-939, doi: 10.1038/nature03696. Kværna T. & Doornbos D.J. (1986).”An integrated approach to slowness analysis with arrays and three-component stations”. In: NORSAR Semiannual Technical Summary, 1 October 1985 – 31 March 1986, Scientific Report 2-85/86, NORSAR, Kjeller, Norway, 60-69. Kværna T. & Ringda F. (1986).”Stability of various f-k estimation techniques”. In: NORSAR Semiannual Technical Summary, 1 April 1986 – 30 September 1986, Scientific Report 1- 86/87, NORSAR, Kjeller, Norway, 29-40. Kværna T. (1989).”On exploitation of small-aperture NORESS type arrays for enhanced P-wave detectability. Bull. Seism. Soc. Am., 79, 888–900. Martini N. & Stiller M. (1992). “Results of the ISO’89 experiment ‘Durchschallung’: recording of the vibrator sweeps of the 3D-seismics in the KTB borehole”. Niedersaechs. Landesamt Bodenforsch, Hannover, KTB-Report, 92 (5), 233–246. Mercier J., Bostock M., Audet P., Gaherty J., Garnero E., Revenaugh J. (2008).”The teleseismic signature of fossil subduction: northwestern Canada”. J. Geophys. Res., 113, B04308. Mykkeltveit S., Åstebøl K., Doornbos D.J. & Husebye E.S. (1983).”Seismic array configuration optimization”. Bull. Seism. Soc. Am. 73, 173-186. Mykkeltveit S., Fyen J., Ringdal F.& Kværna T. (1988).”Spatial characteristics of the NORESS noise field and implications for array detection processing”. Phys. Earth Planet. Inter., 63, 277-283. Neuberg J, Luckett R., Ripepe M. & Braun T. (1994).”Highlights from a seismic broadband array on Stromboli”. Geophys. Res. Lett., 21, 749-752 . Niazi M. (1969).”Use of source arrays in studies of regional structure”. Bull. Seismol. Soc. Am., 59,1631–1643. Oldenburg D.W. (1981).”A comprehensive solution to the linear deconvolution problem”. Geophys. J. R. Astron. Soc., 65, 331–357. Ohrnberger M., Bonnefoy-Claudet S., Cornou C., Guillier B., Kind F., Koehler A., Schissele-Rebel E., Savvaidiss A., Wathelet M. (2004).”User manual for software package CAP - a continuous array processing toolkit for ambient vibration array analysis”. SESAME deliverable D18.06, SESAME EVG1- CT-2000-00026 project (http://sesame-fp5.obs.ujf-grenoble.fr).Ødegaard E., Dooornbos D.J. & Kværna T. (1990).”Surface Topographic effects at arrays and three-component stations”. Bull. Seism. Soc. Am., 80, 2214-2226. Poupinet G., Ellsworth W.L., Frechet J. (1984).”Monitoring velocity variations in the crust using earthquake doublets: An application to the Calaveras fault, California”. J. Geophys. Res., 89, 5719– 5731. Rabbel W., Beilecke T. Bohlen T., Fischer D., Frank A., Hasenclever J., Borm G.,2 Kück, Bram K., Druivenga G., Lüschen E., Gebrande H., Pujol J., Smithson S. (2004).” Superdeep vertical seismic profiling at the KTB deep drill hole (Germany): Seismic close-up view of a major thrust zone down to 8.5 km depth”. J. Geophys. Res., 109, B09309, doi:10.1029/2004JB002975. Reasoner C. & Revenaugh J. (1999).”Short-period P wave constraints on D” reflectivity”. J. Geophys. Res., 104, 955–961. Rentsch S., Buske S., Gutjahr S., Kummerow J., Shapiro S.A. (2010).”Migration-based location of seismicity recorded with an array installed in the main hole of the San Andreas Fault Observatory at Depth (SAFOD)”. Geophys. J. Int., 182, 477–492. Revenaugh J & Mendoza H. (1996).”Mapping shallow heterogeneity with teleseismic P to Rg scattered waves”. Bull. Seismol. Soc. Am. 86, 1194–1199. Rietbrock A. & Scherbaum F. (1999).”Crustal scattering at the KTB from a combined microearthquake and receiver analysis”. Geophys. J. Int., 136, 57-67. Ritter J.R.R., Jordan M., Christensen U. and Achauer U. (2001).”A mantle plume below the Eifel volcanic fields, Germany”. Earth Planet. Sci. Lett., 186, 7–14. Roecker S. (2001).”Constraints on the crust and upper mantle of the Kyrgyz Tien Shan from the preliminary analysis of GHENGIS broad-band seismic data”. Geologiya I Geofizika , 42, 1554–1565. Rost S. & Revenaugh J. (2001).”Seismic detection of rigid zones at the top of the core”. Science, 294, 1911–1914. Rost S. & Thomas C. (2002).”Array seismology: methods and applications”. Reviews of Geophysics, 40, 1008-1035. Rost S. & Garnero E. (2004).”Array seismology advances research into earth’s interior”. EOS 85(301), 305-306. Rost S. & Thomas C. (2009).”Improving Seismic Resolution Throught Array Processing Tecniques”. Surv. Geophys., 30, 271-299. Rost S. (2010).”Seismic constraints on Ear”. Astronomy & Geophysics, 51 (2), 2.26-2.32. Saccorotti G., Di Lieto B., Tronca F., Fischione C., Scarpa R., Muscente R. (2006).”Performances of the UNDERground SEISmic array for the analysis of seismicity in Central Italy”. Annals of Geophys, 49 (4/5), 1041-1057. Saccorotti G. & Del Pezzo E. (2002).”A probabilistic approach to the inversion of data from a seismic array and its application to volcanic signals”. Geophys. J. Int., 143, 249-261. Scarpa R., Muscente R., Tronca F., Fischione C., Rotella P., Abril M., Alguacil G., De Cesare W., Martini M. (2004).”UNDERSEIS: The underground seismic array”. Seismol. Res. Lett., 75, 493 504.Shelly D.R., Beroza G.C., Satoshi I. (2007).”Non-volcanic tremor and low-frequency earthquake swarms”. Nature, 446, 305-307. Scherbaum F., Gillard D., Deichmann N. (1991).”Slowness power spectrum analysis of the coda composition of 2 microearthquake clusters in northern Switzerland”. Earth Planet. Inter., 67, 137– 161. Scherbaum F., Krüger F., Weber M. (1997).”Double beam imaging: mapping lower mantle heterogeneities using combinations of source and receiver arrays”. J. Geophys. Res., 102, 507–522. Schweitzer J., Feyen J., Mykkeltveit S., Kværna T. (2002).”Seismic array: in new manual of seismological observatory practice – NMSOP”. IASPEI, 481-532. Snoke J.A., Munsey J.W., Teague A.G., Bollinger G.A. (1984).”A program for focal mechanism determination by combined use of polarity and SV-P amplitude ratio data”. Earthquake Notes, 55, no. 3, 15. Spudich P. & Cranswick E. (1984).”Direct observation of rupture propagation during the 1979 Imperial Valley earthquake using a short baseline accelerometer array”. Bull. Seism. Soc. Am.; 74 (6), 2083-2114. Spudich P. & Bostwick T. (1987).”Studies of the seismic coda using an earthquake cluster as deeply buried seismograph array”. J. Geophys. Res., 92, 10526-10546. Stammler K. (1993).” Seismichandler—Programmable multichannel data handler for interactive and automatic processing of seismological analyses”. Computers & Geosciences, 19 (2), 135-140. Stammler K.”Seismic Handler”. Seismic Handler version 2.4h (05-May-2007), Copyright (C) 2006 Klaus Stammler, Seismological Observatory Graefenberg (SZGRF) http://www.seismichandler. org/portal/wiki. Tarenghi M. (2008).”The Atacama large millimetre/submillimeter array: overview and status”. Astrophys. Space Sci., 313, 1-7. Thomas C., Weber M., Wicks C. and Scherbaum F. (1999).”Small scatterers in the lower mantle observed at German broadband arrays”. J. Geophys. Res., 104, 15,073–15,088. Thomas C., Kendall J.M., Weber M. (2002).”Images of D” beneath northern Asia, 1, Multi-azimuth studies of heterogeneity”. Geophys. J. Int., 151 (1), 279–295. Vidale J.E., Dodge D.A. and Earle P.S. (2000).”Slow differential rotation of the Earth’s inner core indicated by temporal changes in scattering”. Nature, 405, 445–448. Wagner G.A., Coyle D.A., Duyster J., Henjes-Kunst F., Peterek A., Schrrder B., Stöckhert B., Wemmer K., Zulauf G. Ahrendt H., Bischoff R., Hejl E., Jacobs J., Menzel D., Lal N., Van Den Hante P., Vercoutere C. & Welzet B. (1997).”Post-Variscan thermal and tectonic evolution of the KTB site and its surroundings”. J. Geophys. Res., 102, 18221-18232. Waldhauser F. & Ellsworth W.L. (2000).”A double-difference earthquake location algorithm: Method and application to the Northern Hayward Fault, California”. Bull. seism. Soc. Am., 90, 1353–1368.Wang R. (1999).”A simple orthonormalization method for stable and efficient computation of Green’s functions”. Bull. Seism. Soc. Am., 89 (3), 733–741. Weber M., Davis J.P., Thomas C., Krüger F., Scherbaum F., Schlittenhardt J. and Körnig M. (1996).”The structure of the lowermost mantle as determined from using seismic arrays. Seismic Modeling of the Earth’s Structure, edited by Boschi E., Ekström G. and Morelli A., 399–442, Instit. Naz. di Geophys., Rome. Wessel P. & Smith W.H.F. (1998).”New, improved version of the Generic Mapping Tools Released”. EOS Trans. AGU, 79, 579. Whiteway F. E. (1966).”The use of arrays for earthquake seismology”. Proc. R. Soc. London, Ser. A, 290, 328–342. Williams E., Maynard J., Skudrzyk E. (1980).”Sound source reconstructions using a microphone array”. J. Acoust. Soc. Am., 68, 340-344. Wright C. (1972).”Array studies of seismic waves arriving between P and PP in the distance range 90 to 115. Bull. Seismol. Soc. Am., 62, 385–400. Zoback M.D. & Harjes H.P. (1997).”Injection-induced earthquakes and crustal stress at 9 km depth at the KTB deep drilling site, Germany”. J. Geophys. Res., 102, 18,477-18,491. Zhou H.W. (1994).”Rapid three-dimensional hypocentral determination using a master station method”. J. Geophys. Res., 99, 15 439–15 455.en
dc.type.methodGeophysicsen
dc.description.obiettivoSpecifico6T. Sismicità indotta e caratterizzazione sismica dei sistemi naturalien
dc.description.fulltextopenen
dc.contributor.authorRoselli, P.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
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item.openairecristypehttp://purl.org/coar/resource_type/c_46ec-
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crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0003-3844-5059-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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