Academic literature on the topic 'Teleseismic data'

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Journal articles on the topic "Teleseismic data"

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Frederiksen, A. W. "Transfer functions between teleseismic data components." Geophysical Journal International 221, no. 2 (2020): 1248–63. http://dx.doi.org/10.1093/gji/ggaa085.

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SUMMARY Different data components of teleseismic waveforms are related by transfer functions that depend only on receiver-side structure. This is the common basis of a number of teleseismic techniques, including receiver functions and shear wave splitting analysis. Common trace misfits used in these analysis techniques are shown to be equivalent to band-limited comparisons of real and synthetic transfer functions. The data deconvolution used in receiver function analysis leads to reduced structural resolution compared to direct trace-based misfits such as cross-convolution, with direct transfe
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Short, Kevin M. "Detection of Teleseismic Events in Seismic Sensor Data Using Nonlinear Dynamic Forecasting." International Journal of Bifurcation and Chaos 07, no. 08 (1997): 1833–45. http://dx.doi.org/10.1142/s0218127497001400.

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In this paper we consider the use of nonlinear dynamic (NLD) forecasting as a signal processing tool for seismic applications. The specific problem considered here arises in monitoring nuclear tests and nuclear treaty compliance, where the presence of ubiquitous background noise obscures the seismic signals associated with the tests. The problem is that the signal from a distant teleseismic event can be attenuated so that it is lost in the background noise, and since the noise overlaps the frequency band occupied by the teleseisms, frequency-based techniques provide only marginal improvements
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Fan, Chengliang, Gary L. Pavlis, Arthur B. Weglein, and Bogdan G. Nita. "Removing free-surface multiples from teleseismic transmission and constructed reflection responses using reciprocity and the inverse scattering series." GEOPHYSICS 71, no. 4 (2006): SI71—SI78. http://dx.doi.org/10.1190/1.2217369.

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We develop a new way to remove free-surface multiples from teleseismic P- transmission and constructed reflection responses. We consider two types of teleseismic waves with the presence of the free surface: One is the recorded waves under the real transmission geometry; the other is the constructed waves under a virtual reflection geometry. The theory presented is limited to 1D plane wave acoustic media, but this approximation is reasonable for the teleseismic P-wave problem resulting from the steep emergence angle of the wavefield. Using one-way wavefield reciprocity, we show how the teleseis
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Zhang, Jia, and Charles A. Langston. "Separating the scattered wavefield from teleseismic P using curvelets on the long beach array data set." Geophysical Journal International 220, no. 2 (2019): 1112–27. http://dx.doi.org/10.1093/gji/ggz487.

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SUMMARY A dense seismic array, composed of over 5000 stations with an average spacing close to 120 m was deployed in Long Beach, CA, by NodalSeismic and Signal Hill Petroleum as part of a survey associated with the Long Beach oilfield. Among many interesting wave propagation effects that have been reported by others, we observe that the coda of teleseismic P waves display waves caused by obvious local scattering from the Signal Hill popup structure between strands of the Newport-Inglewood fault. The density of the seismic array allows space-based methods, such as the Curvelet transform, to be
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Lewis, Brian T. R., and LeRoy M. Dorman. "Recording teleseisms on the seafloor; an example from the Juan de Fuca plate." Bulletin of the Seismological Society of America 88, no. 1 (1998): 107–16. http://dx.doi.org/10.1785/bssa0880010107.

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Abstract In 1991, during an experiment to compare low-frequency seismic noise on a basaltic and a sediment covered seafloor (NOBS), we recorded teleseisms on the Juan de Fuca ridge, the Gorda ridge, and the adjacent Cascadia Basin with the SNAG ocean-bottom seismometers (OBS). These data provide an indication of the type of data that may be obtained from future experiments to record teleseisms and may be helpful in designing these experiments and analyzing the results. We found that although seafloor noise is dominated by microseisms in the band 0.1 to 0.3 Hz, there is a well-developed minimum
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Amukti, Rian, and Wiwit Suryanto. "Analisa Receiver Function Teleseismic untuk Mendeteksi Moho pada Stasiun Bkb Data Meramex." INDONESIAN JOURNAL OF APPLIED PHYSICS 3, no. 02 (2016): 195. http://dx.doi.org/10.13057/ijap.v3i02.1272.

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<span>It has been done a research to determine internal earth using receiver function teleseismic analysis <span>method. This method have been done by using MERAMEX (MErapi Amphibious Experiment) data from <span>broadband seismometer BKB. Event of teleseismic is chosen from Honshu Japan with radius 30<span>o <span>and <span>magnitude 7.2. This research begun by analysing radial and vertical characteristic of teleseismic event<br /><span>and using bandpass filter with range 0.003 Hz – 0.5 Hz. Then Iteractive Deconvolution is used to get <span&g
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Li, Yingping, William Prothero, Clifford Thurber, and Rhett Butler. "Observations of ambient noise and signal coherency on the Island of Hawaii for teleseismic studies." Bulletin of the Seismological Society of America 84, no. 4 (1994): 1229–42. http://dx.doi.org/10.1785/bssa0840041229.

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Abstract Ambient seismic noise conditions at several sites on the Island of Hawaii have been studied by analyzing noise power spectral density (PSD) and signal-to-noise ratio (SNR) of teleseisms. Broadband digital waveform data used in this study were collected during Project ALOHA. Direct comparison of noise PSD and SNR of teleseisms simultaneously recorded at stations on Hawaii and at station KIP on Oahu indicates that the stations on Hawaii are quieter than station KIP on Oahu in the frequency band of 0.1 to 1 Hz, suggesting that the Island of Hawaii can provide better noise conditions than
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Shimizu, Kousuke, Yuji Yagi, Ryo Okuwaki, and Yukitoshi Fukahata. "Development of an inversion method to extract information on fault geometry from teleseismic data." Geophysical Journal International 220, no. 2 (2019): 1055–65. http://dx.doi.org/10.1093/gji/ggz496.

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SUMMARY Teleseismic waveforms contain information on fault slip evolution during an earthquake, as well as on the fault geometry. A linear finite-fault inversion method is a tool for solving the slip-rate function distribution under an assumption of fault geometry as a single or multiple-fault-plane model. An inappropriate assumption of fault geometry would tend to distort the solution due to Green’s function modelling errors. We developed a new inversion method to extract information on fault geometry along with the slip-rate function from observed teleseismic waveforms. In this method, as in
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Shragge, J., B. Artman, and C. Wilson. "Teleseismic shot-profile migration." GEOPHYSICS 71, no. 4 (2006): SI221—SI229. http://dx.doi.org/10.1190/1.2208263.

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The shot-profile migration approach of wave-equation migration generates subsurface images using the interferometric principle of crosscorrelating two passive wavefields. These wavefields are typically a source wavefield containing energy from an excited source and a receiver wavefield comprised of scattered-source wavefield energy by the discontinuous earth structure. Shot-profile migration can be recast as a novel way of imaging the earth’s lithosphere using teleseismic wavefield data, where the source wavefield is the directly arriving wavefront and the receiver wavefield is the following w
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Campman, Xander, and Stephane Rondenay. "Multichannel near‐array corrections for short‐period teleseismic data." Journal of the Acoustical Society of America 119, no. 5 (2006): 3308. http://dx.doi.org/10.1121/1.4786295.

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Dissertations / Theses on the topic "Teleseismic data"

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Foley, John Edward. "Crustal structure from teleseismic bodywave data." Thesis, Massachusetts Institute of Technology, 1990. http://hdl.handle.net/1721.1/52914.

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Thesis (Sc.D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1990.<br>Includes bibliographical references (leaves 245-255).<br>by John Edward Foley.<br>Sc.D.
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Sargeant, Susanne. "Modelling shallow earthquakes with teleseismic broadband data." Thesis, University of East Anglia, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.251561.

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Fan, Chengliang. "Extracting P-primary transmission and reflection impulse responses from teleseismic data." [Bloomington, Ind.] : Indiana University, 2005. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:3199414.

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Thesis (Ph.D.)--Indiana University, Dept. of Geological Sciences, 2005.<br>Source: Dissertation Abstracts International, Volume: 66-11, Section: B, page: 5867. Adviser: Gary L. Pavlis. Title from dissertation home page (viewed Oct. 11, 2006).
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El-Haddadeh, B. R. H. "Seismological investigation of the crust and upper mantle structure of the British Isles using teleseismic travel time data." Thesis, University of Leeds, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.372598.

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Dewberry, Shawn Robert. "Crustal and upper mantle structure for the Pacific Northwest from an analysis of short-period teleseismic network data /." Thesis, Connect to this title online; UW restricted, 1996. http://hdl.handle.net/1773/6795.

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Kufner, Sofia-Katerina [Verfasser]. "Lithospheric structure and seismotectonic setting of the Hindu Kush, the Tajik-Afghan basin and the western Pamir from analysis of local- and teleseismic data / Sofia-Katerina Kufner." Berlin : Freie Universität Berlin, 2016. http://d-nb.info/1122438737/34.

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Santos, Rúben José Chaves Miguel dos. "Modelação de processos de rotura sísmica através de dados de observação da deformação superficial." Doctoral thesis, Universidade de Évora, 2013. http://hdl.handle.net/10174/11790.

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Nesta dissertação foi desenvolvida uma metodologia baseada no cruzamento de diferentes técnicas e de dados geodésicos e sísmicos, para estudar o processo de rotura de sismos. A metodologia consiste, numa primeira fase, em determinar o campo de deslocamento cossísmico produzido por um evento, através da técnica InSAR. Numa fase seguinte o modelo de deslocamentos cossísmicos é determinado através das equações de Okada utilizando o modelo de distribuição de deslizamentos obtido pela inversão das formas de onda registadas em estações de banda larga a distâncias telessísmicas. Para comparar o model
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Vanacore, Elizabeth A. "Determining the nature of middle and lower mantle heterogeneity using array analyses of teleseismic data." Thesis, 2008. http://hdl.handle.net/1911/22203.

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The structure of the Earth's lower mantle has key implications to the distribution of potential mantle reservoirs and the dynamics of mantle convection. To characterize the nature of mantle heterogeneity, three teleseismic studies are combined in this thesis to expand the observational knowledge of middle mantle and lower mantle features. Array stacking techniques (linear, phase weight, Nth root, common-conversion point) are applied to P-wave coda data from West Pacific and South American subduction zones to search for middle mantle discontinuities and scatterers using S to P converted wavefor
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Books on the topic "Teleseismic data"

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W, Dewey James, and Geological Survey (U.S.), eds. The Scotts Mills, Oregon, earthquake of March 25, 1993: Intensities, strong-motion data, and teleseismic data. U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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W, Dewey James, and Geological Survey (U.S.), eds. The Scotts Mills, Oregon, earthquake of March 25, 1993: Intensities, strong-motion data, and teleseismic data. U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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Park, Sam-Keun. Three-dimensional Upper Mantle structure beneath Northern California inferred from teleseismic P-Wave delay time data. 1994.

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Book chapters on the topic "Teleseismic data"

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Nolet, Guust, and Berend Scheffers. "Imaging with Teleseismic Data." In Digital Seismology and Fine Modeling of the Lithosphere. Springer US, 1989. http://dx.doi.org/10.1007/978-1-4899-6759-6_3.

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Kværna, Tormod, Frode Ringdal, Johannes Schweitzer, and Lyla Taylor. "Optimized Seismic Threshold Monitoring — Part 2: Teleseismic Processing." In Monitoring the Comprehensive Nuclear-Test-Ban Treaty: Data Processing and Infrasound. Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8144-9_5.

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Zeyen, H., and U. Achauer. "Joint Inversion of Teleseismic Delay Times and Gravity Anomaly Data for Regional Structures." In Upper Mantle Heterogeneities from Active and Passive Seismology. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-015-8979-6_15.

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Li, Jie, Gang Liu, Xuejun Qiao, et al. "Rupture Characteristics of the 25 November 2016 Aketao Earthquake (Mw 6.6) in Eastern Pamir Revealed by GPS and Teleseismic Data." In Pageoph Topical Volumes. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-92297-3_5.

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Beldjoudi, Hamoud, Bertrand Delouis, and Abdelkrim Yelles-Chaouche. "Reassessing the Rupture Process of the 2003 Boumerdes-Zemmouri Earthquake (Mw 6.8, Northern Algeria) Using Teleseismic, Strong Motion, InSAR, GPS, and Coastal Uplift Data." In On Significant Applications of Geophysical Methods. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01656-2_45.

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"Three-dimensional structure of lateral heterogeneities in p-velocities in the upper mantle of the southern margin of Siberia from teleseismic data." In Computerized Tomography. De Gruyter, 1995. http://dx.doi.org/10.1515/9783112314067-036.

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Tikoff, B., C. Siddoway, D. Sokoutis, and E. Willingshofer. "The lithospheric folding model applied to the Bighorn uplift during the Laramide orogeny." In Tectonic Evolution of the Sevier-Laramide Hinterland, Thrust Belt, and Foreland, and Postorogenic Slab Rollback (180–20 Ma). Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2555(08).

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ABSTRACT The Bighorn uplift, Wyoming, developed in the Rocky Mountain foreland during the 75–55 Ma Laramide orogeny. It is one of many crystalline-cored uplifts that resulted from low-amplitude, large-wavelength folding of Phanerozoic strata and the basement nonconformity (Great Unconformity) across Wyoming and eastward into the High Plains region, where arch-like structures exist in the subsurface. Results of broadband and passive-active seismic studies by the Bighorn EarthScope project illuminated the deeper crustal structure. The seismic data show that there is substantial Moho relief benea
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Conference papers on the topic "Teleseismic data"

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Campman, X., S. Rondenay, G. Herman, and A. Verdel. "Multichannel Teleseismic Data Processing and Imaging." In 68th EAGE Conference and Exhibition - Workshop Package. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609.201405162.

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Driver, Damani. "TELESEISMIC DATA ACQUISITION ON THE COASTAL PLAIN OF NORTH CAROLINA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286830.

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L. Ronin, A., Y. P. Lukashin, V. P. Semenov, and R. Y. Tsukerman. "A New Technology for a Polarisation Processing of the Teleseismic Station Data." In 61st EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609.201407890.

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Pageot, D., S. Operto, M. Vallée, J. Virieux, and R. Brossier. "Lithospheric imaging from teleseismic data by frequency-domain elastic full-waveform tomography." In 72nd EAGE Conference and Exhibition - Workshops and Fieldtrips. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609.20149932.

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Beller, S., V. Monteiller, S. Operto, et al. "3D Elastic Full Waveform Inversion of Teleseismic Data for High-resolution Ospheric Imaging." In 77th EAGE Conference and Exhibition 2015. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413203.

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Pageot, D., S. Operto, M. Valle, R. Brossier, and J. Virieux. "Two-dimensional Elastic Full-waveform Inversion of Passive Teleseismic Data for Lithospheric Imaging." In 74th EAGE Conference and Exhibition incorporating EUROPEC 2012. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20148669.

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Mordvinova, V. V., and M. M. Kobelev. "Velocity Structure of the Crust and Upper Mantle in the Southern Siberian Craton and the Flanking Orogens, from Teleseismic Data." In GeoBaikal 2014. EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20141764.

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Giannopoulos, D., C. Orfanos, K. Leontarakis, et al. "Passive seismic data processing with no prior information: Estimating the crustal shear-wave velocity model of the South Lokichar Basin (Kenya) through integration of ambient seismic noise and teleseismic earthquake data." In SEG Technical Program Expanded Abstracts 2020. Society of Exploration Geophysicists, 2020. http://dx.doi.org/10.1190/segam2020-3427725.1.

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Wang, Herb, and Dante Fratta. "Fiber Optic Monitoring in Mines." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-1218.

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ABSTRACT: Fiber-optic cable can be deployed in underground mines over kilometers in distance. The sensing interrogator and data acquisition can be operated remotely using lead-in fiber. Fiber-optic sensors can be either discrete or distributed. Fiber-Bragg Grating (FBG) sensors were grouted into the walls and roof of a small alcove at a depth of 4100 ft (1250 m) to measure deformation while jacking the roof (Gage et al., 2014). The modulus as a function of depth showed the profile of the Excavation Damage Zone (EDZ). Although FBGs can be embedded into long runs of optical fiber to create a qua
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Reports on the topic "Teleseismic data"

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Asudeh, I. PRS4 recording of teleseismic data from the Deep-Probe Passive Survey near Grand Junction, Colorado. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207604.

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Snyder, D. B. Subcontinental mantle lithosphere study using teleseismic data for the east arm of Great Slave Lake. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292470.

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Barbara Romanowicz and Mark Panning. Calibration of 3D Upper Mantle Structure in Eurasia Using Regional and Teleseismic Full Waveform Seismic Data. Office of Scientific and Technical Information (OSTI), 2005. http://dx.doi.org/10.2172/838993.

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Barbara Romanowicz and Mark Panning. Calibration of 3D Upper Mantle Structure in Eurasia Using Regional and Teleseismic Full Waveform Seismic Data. Office of Scientific and Technical Information (OSTI), 2005. http://dx.doi.org/10.2172/838994.

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Davis, Paul M., Shangxing Gao, and Laura Borton. Analysis of Digital Teleseismic Array Data Collected in South Central Siberia and Northern Mongolia, GSN SKS Waves and S Waves from Lop Nor Nuclear Explosions. Defense Technical Information Center, 2001. http://dx.doi.org/10.21236/ada387203.

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