Littérature scientifique sur le sujet « Wide Angle Reflection »
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Articles de revues sur le sujet "Wide Angle Reflection"
Shiraishi, Kazuya, Gou Fujie, Takeshi Sato, Susumu Abe, Eiichi Asakawa et Shuichi Kodaira. « Interferometric OBS imaging for wide-angle seismic data ». GEOPHYSICS 82, no 5 (1 septembre 2017) : Q39—Q51. http://dx.doi.org/10.1190/geo2016-0482.1.
Texte intégralZhu, Xinfa, et George A. McMechan. « Amplitude and phase versus angle for elastic wide-angle reflections in the τ‐p domain ». GEOPHYSICS 80, no 1 (1 janvier 2015) : N1—N9. http://dx.doi.org/10.1190/geo2013-0191.1.
Texte intégralRendleman, C. A., et F. K. Levin. « Reflection maxima for reflections from single interfaces ». GEOPHYSICS 53, no 2 (février 1988) : 271–75. http://dx.doi.org/10.1190/1.1442462.
Texte intégralChang, Ya-Chun, Wei-Feng Xu, Meng-Chieh Wu, Cyun-Tai Hong et Chen-Kuan Kuo. « P‐29 : Wide Visual Angle Anti‐Reflection Film ». SID Symposium Digest of Technical Papers 51, no 1 (août 2020) : 1442–44. http://dx.doi.org/10.1002/sdtp.14159.
Texte intégralSava, Paul, et Ioan Vlad. « Wide-azimuth angle gathers for wave-equation migration ». GEOPHYSICS 76, no 3 (mai 2011) : S131—S141. http://dx.doi.org/10.1190/1.3560519.
Texte intégralKhalaj-Amirhosseini, Mohammad, et Sayed Mohammad Javad Razavi. « WIDE-ANGLE REFLECTION WAVE POLARIZERS USING INHOMOGENEOUS PLANAR LAYERS ». Progress In Electromagnetics Research M 9 (2009) : 9–20. http://dx.doi.org/10.2528/pierm09070301.
Texte intégralEstakhri, Nasim Mohammadi, Verena Neder, Mark W. Knight, Albert Polman et Andrea Alù. « Visible Light, Wide-Angle Graded Metasurface for Back Reflection ». ACS Photonics 4, no 2 (3 février 2017) : 228–35. http://dx.doi.org/10.1021/acsphotonics.6b00965.
Texte intégralGoldman, Ph.D., Laine. « Appreciative Reflection : A Wide-Angle Lens for Changing Perception ». AI Practitioner 16, no 3 (1 août 2014) : 53–58. http://dx.doi.org/10.12781/978-1-907549-20-5-8.
Texte intégralChartas, George, et Sarah Strickland. « Wide-Angle Quasar Feedback ». Proceedings of the International Astronomical Union 11, S319 (août 2015) : 58. http://dx.doi.org/10.1017/s1743921315010145.
Texte intégralFruehn, Juergen, Moritz M. Fliedner et Robert S. White. « Integrated wide‐angle and near‐vertical subbasalt study using large‐aperture seismic data from the Faeroe—Shetland region ». GEOPHYSICS 66, no 5 (septembre 2001) : 1340–48. http://dx.doi.org/10.1190/1.1487079.
Texte intégralThèses sur le sujet "Wide Angle Reflection"
Harsha, Senusi Mohamed. « Interpretation of Southern Georgia coastal plain velocity structure using refraction and wide-angle reflection methods ». Thesis, Georgia Institute of Technology, 1988. http://hdl.handle.net/1853/25886.
Texte intégralHananto, Nugroho. « Architecture and Evolution of North Sumatra Subduction Zone based on long Offset Seismic Reflection and Wide Angle Seismic Refraction / Reflection Data ». Institut de physique du globe (Paris), 2011. http://www.theses.fr/2011GLOB1203.
Texte intégralOueity, Jounada. « Near-vertical and wide-angle seismic reflection studies of the Moho and sub-crustal lithosphere in NW Canada ». Thesis, University of British Columbia, 2010. http://hdl.handle.net/2429/28903.
Texte intégralHughes, Stephen. « Crustal structure of northeastern North America : results from the Ontario-New York-New England seismic refraction/wide-angle reflection experiment ». Thesis, University of Leicester, 1992. http://hdl.handle.net/2381/35043.
Texte intégralMeléndez, i. Catalán Adrià. « Development of a New Parallel Code for 3-D Joint Refraction and Reflection Travel-Time Tomography of Wide-Angle Seismic Data. Synthetic and Real Data Applications to the Study of Subduction Zones ». Doctoral thesis, Universitat de Barcelona, 2014. http://hdl.handle.net/10803/289786.
Texte intégralAquesta tesi està dedicada a la tomografia sísmica. Concretament, he implementat una eina de modelització 3D per a la tomografia conjunta de temps de trajecte de refraccions i reflexions (TOMO3D). La raó darrere d'aquest objectiu és l'evidència de que la informació basada en dades sísmiques 2D no permet copsar la complexitat de gran part dels cossos geològics, i en particular de la zona sismogènica en marges de subducció. El desenvolupament del TOMO3D es basa en el TOMO2D, un codi d'avantguarda per a la tomografia conjunta de refraccions i reflexions en 2D. Els arxius de codi han estat reescrits, redefinint i introduint les funcions necessàries per dur a terme la inversió 3D. Els testos fets amb la versió seqüencial del codi posen de manifest la necessitat de paral·lelització ja que l'increment de la mida dels conjunts de dades així com la modelització de la dimensió espacial afegida fan que les inversions siguin computacionalment exigents. La versió paral·lelitzada del TOMO3D ha sigut aplicada a un cas sintètic complex que simula una zona de subducció. Aquesta primera aplicació 3D serveix per avaluar la correcció de la programació del codi, i com a descripció pas a pas del procediment de modelització. Els resultats demostren la capacitat del codi per recuperar acuradament la distribució de velocitat i la geometria dels dos reflectors. Finalment, el TOMO3D és aplicat a un conjunt 3D de dades de sísmica de gran angle adquirit al marge pacífic d'Equador i Colòmbia per extreure'n un model 3D de la velocitat de les plaques cavalcant i subduïda, que és comparat amb el resultat obtingut amb un codi 3D de tomografia de temps de trajecte de refraccions (FAST). La comparació indica que el TOMO3D és més acurat que el FAST però al mateix temps és computacionalment més exigent. Tot i així, la paral·lelització del TOMO3D permet utilitzar plataformes de supercomputació, a diferència del que passa amb el FAST i la majoria de codis existents.
Biari, Youssef. « Structure profonde de la marge Nord-Ouest Africaine ». Thesis, Brest, 2015. http://www.theses.fr/2015BRES0080/document.
Texte intégralThe NE American margin represents one of the best studied margins in the world, it was the subject of several scientific programs. In comparison, the conjugate NW African margin remains fairly unknown, only two deep seismic cruises were acquired: the SISMAR cruise (2001) offshore the Meseta and the DAKHLA cruise (2002) offshore the Sahara. The deep structure of the Canadian margin is known due to the SMART wide-angle seismic profiles 1, 2 and 3. The first objective of the MIRROR project was to acquire combined wide-angle and deep reflection seismic data offshore a segment conjugate to the SMART-1 profile. The comparison between the homologous segments of these two margins aimed to better understand the opening mechanism of the Central Atlantic Ocean. A comparison between Sismar, Dakhla and Mirror models shows that the continental crust is thicker in the north and thins toward the south. The width of the transition zone is narrower south and Sismar profiles are located on a sedimentary basin placed on a very thinned continental crust. Comparing the Mirror profile with that of the Canadian conjugate margin (Smart 1) shows that the thickness, the structure of the continental crust and the thinning is very similar. However, zones of exhumed and serpentinized mantle were imaged along the Canadian profile that have no conjugate on the African margin. Moreover, the thickness of the oceanic crust is variable with 8 km on the African side and only 3-4 km on the Canadian margin. Several hypotheses have been proposed to explain this difference (a) an age difference between the two types of crust (b) thickening associated with the passage of the Canary hotspot (c) an asymmetric accretion or (d) an accretion at slow to ultra-slow speading centers
Bouyahiaoui, Boualem. « Structure profonde et réactivation de la marge est-algérienne et du bassin adjacent (secteur d'Annaba), contraintes par sismique réflexion multitrace et grand-angle terre-mer ». Thesis, Nice, 2014. http://www.theses.fr/2014NICE4116/document.
Texte intégralIn this study, we determine the deep structure of the eastern Algerian basin and its southern margin in the Annaba region (easternmost Algeria), to better constrain the plate kinematic reconstruction in this region. This study is based on new geophysical data collected during the SPIRAL cruise in 2009 that included a wide-angle, 240-km-long, onshore-offshore seismic profile, multichannel seismic reflection lines, and gravity and magnetic data, which was complemented by the available geophysical data for the study area. The analysis and modeling of the wide-angle seismic data using travel-times and amplitudes, and integrated with the multichannel seismic lines, reveal the detailed structure of an ocean-to-continent transition. In the deep basin, there is an ~5.5-km-thick oceanic crust that is composed of two layers. The upper layer of the crust is defined by a high velocity gradient and P-wave velocities between 4.8 km/s and 6.0 km/s from the top to the bottom. The lower crust is defined by a lower velocity gradient and P-wave velocity between 6.0 km/s and 7.1 km/s. The Poisson ratio in the lower crust deduced from S-wave modeling is 0.28, which indicates that the lower crust is composed mainly of gabbros. Below the continental edge, a typical continental crust with P-wave velocities between 5.2 km/s and 7.0 km/s from the top to the bottom shows a gradual seaward thinning of ~15 km over an ~35-km distance
Laurencin, Muriel. « Etude de la géométrie, de la nature et des déformations de la zone de subduction des Petites Antilles du Nord ». Thesis, Brest, 2017. http://www.theses.fr/2017BRES0096/document.
Texte intégralIn subduction zones, the 3D geometry of the plate interface is one of the key parameters that controls margin tectonic deformation, interplate coupling and seismogenic behavior. The North American plate subducts below the Caribbean plate with a convergence rate of 20 mm/y. The seismic activity is heterogeneous and increases locally under the Virgin Islands platform. The northward increasing convergence obliquity is favorable in partitioning which deformations were not really observed. This PhD confirms that the forearc crust is a crust of oceanic affinity thickened by hotspot magmatism and poorly affected by subduction magmatism. Two structures accommodating the partitioning of the deformation were identified. The Bunce Fault is a 850-kmlength sinistral strike-slip fault extending from Hispaniola to the east of Barbuda decoupling the accretionary prism from the Caribbean substratum. The Anegada Passage, whose extension towards the NE is highlighted, entailed deeply the forearc. The structures are reactivated in sinistral strike-slip faults compatible with the partitioning of the deformation after formation in extension due to the collision of the Bahamas Bank with the northern margin. We image for the first time the characteristics of a slow ridge formation (partly complex core and partly oceanic grain) entering in subduction. It affects the morphology of the accretion prism and probably the seismogenic potential of the subduction interface. We have highlighted a shallower slab which is located under the NE Anegada Passage and where earthquakes and partitioning deformations increase locally. Thus, the shallowing slab might results in a local greater interplate coupling favoring seismic activity and tectonic partitioning beneath the Anegada Passage
Brancatelli, Giuseppe. « Analisi di dati acquisiti con OBS ». Doctoral thesis, Università degli studi di Trieste, 2010. http://hdl.handle.net/10077/3458.
Texte intégralGli OBS (Ocean Bottom Seismometer) sono ampiamente utilizzati negli studi sismici crostali attraverso l’utilizzo delle registrazioni di onde rifratte e riflesse a grande offset (Wide Angle Reflection/Refraction, WAR/R). L'analisi di questi dati comporta, solitamente, l'impiego di modellistica diretta e/o inversa al fine di giungere alle velocità dei singoli strati e alle profondità delle interfacce. In questa tesi, invece, si presenta un approccio diverso che prevede: 1) costruzione di modelli di velocità dall’analisi dei segnali rifratti; 2) elaborazione dei dati OBS al fine di ottenere immagini sismiche a riflessione. In particolare, gli OBS e gli scoppi sono stati riportati ad uno stesso datum (superficie del mare), utilizzando il Wave Equation Datuming (WED). Dopo il WED è stato possibile applicare l'elaborazione tipica della sismica a riflessione. I profili OBS analizzati sono stati acquisiti nell'area dell'Arco Ellenico e, i risultati ottenuti, hanno permesso di riconoscere le strutture geologiche principali e i meccanismi dell’evoluzione tettonica. L'utilizzo del WED ha migliorato la risoluzione delle sezioni finali rispetto a quanto ottenibile con le correzioni statiche classiche. Per confronto è stata applicata la metodologia WED anche a dati simici ad alta risoluzione a terra, risolvendo problemi di correzioni statiche e di strutturazioni tettoniche apparenti nell'area della Bassa Pianura Friulana.
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Leprêtre, Angélique. « Contraintes par imagerie sismique pénétrante sur l'évolution d'une marge Cénozoïque réactivée en compression (cas de la marge algérienne, secteur de Tipaza) ». Thesis, Brest, 2012. http://www.theses.fr/2012BRES0079/document.
Texte intégralThe inversion of passive margins appears to be one of the first steps towards the initiation of new subduction zones. This crucial step in plate tectonics nevertheless still raises many questions. The study of margins currently reactivated by compressional tectonics is thus essential to better understand this process. These margins are uncommon, located in different geodynamic settings, and the factors determining their evolution are poorly constrained. The Algerian margin, located in North Africa, is one of handful of modern examples worldwide. The evolution of this margin, rifted during the Miocene, in a back-arc setting, is part ofthe complex puzzle of the western Mediterranean. Since a few million years, the margin has suffered inversion and compression in the framework of slow on going convergence between the European and African plates. This convergence generates moderate to strong earthquakes in North Algeria. The relatively young age of the Algerian basin, the large sediment load, and the compressive forces, constitute favorable conditions to the formation of a future subduction zone. Studies from the past ten years indicate, that themain unresolved questions are related to (1) the deep structure of the Algerian basin and its southern margin (the type of margin, the nature of the basement, the dimension and nature of the ocean-continent transition, the style and the distribution of the compressional deformation), and (2) the history of the kinematic and geodynamic evolution of the basin. All of these unknowns have prevented a complete and thorough analysis of modalities of the Algerian margin inversion. This study focuses on the Central Algerian margin, in the area of Tipaza (West of Algiers), a key region to understand the mechanism of the opening of the Algerian basin. Processing and analysis of a deep wide-angle and multichannel seismic new data set acquired in the context of the French-Algerian project SPIRAL (Sismique profonde et Investigation Régionales en Algérie, 2009)have enabled us to determine the crustal structure of the Algerian basin and its southern continental margin,as well as the pseudo-3D structure of a specific feature in the study area: the submarine topographic highformed by the Khayr-al-Din bank. The analysis of the deep structure of the margin reveals features inherited from its complex evolution: (1) a crust of continental nature of more than 15 km thick at the upper margin(Khayr-al-Din Bank), (2) a thin crust of oceanic nature, 5-6 thick in the deep basin, including slightly high velocities at its base (7.2 km/s - 7.3 km/s), (3) similarities with margins formed in context of transform deformation, (4) a progressive deepening of the whole sedimentary cover and the thickening of the Plio-Quaternary sediments, from the distal deep basin towards the margin foot, coeval with (5) a long wavelengthflexuration of the basement in the basin. Results from this study provide new constraints on (1) the geometryand nature of the margin and the basin, (2) the evolution of the margin, suggesting a multiphased history including a stage of rifting and/or oceanic spreading, a transcurrent episode due to the westward migration of the Alboran block, and a diffuse Plio-Quaternary compressional reactivation distributed from the deep basinto the upper margin; (3) the mechanisms of the reactivation marked by newly formed south-dipping blind-thrusts, especially at the foot of the Khayr-al-Din bank, and suggesting a Plio-Quaternary uplift of the bankof 0.2 mm/y to 0.75 mm/y and the early stages of imbricate thrusting of crustal scales
Livres sur le sujet "Wide Angle Reflection"
Yosio, Nakamura, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralYosio, Nakamura, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralYosio, Nakamura, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralYosio, Nakamura, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralYosio, Nakamura, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralBrocher, Thomas M. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralJ, Moses Michael, Tréhu Anne Martine et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralJ, Moses Michael, Tréhu Anne Martine et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralYosio, Nakamura, et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralJ, Moses Michael, Tréhu Anne Martine et Geological Survey (U.S.), dir. Onshore-offshore wide-angle seismic recordings from central Oregon : The five-day recorder data. Menlo Park, Calif : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralChapitres de livres sur le sujet "Wide Angle Reflection"
Braile, L. W., et C. S. Chiangl. « The continental Mohorovičič Discontinuity : Results from near-vertical and wide-angle seismic reflection studies ». Dans Reflection Seismology : A Global Perspective, 257–72. Washington, D. C. : American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0257.
Texte intégralMereu, Robert, Dapeng Wang et Oliver Kuhn. « Evidence for an inactive rift in the Precambrian from a wide-angle reflection survey across the Ottawa-Bonnechere graben ». Dans Reflection Seismology : The Continental Crust, 127–34. Washington, D. C. : American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd014p0127.
Texte intégralAnsorge, J., K. Holliger, P. Valasek, S. Ye, P. Finckh, W. Frei, E. Kissling et al. « Integrated analysis of seismic normal incidence and wide-angle reflection measurements across the eastern Swiss Alps ». Dans Continental Lithosphere : Deep Seismic Reflections, 195–205. Washington, D. C. : American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0195.
Texte intégralMereu, Robert. « The Heterogeneity of the Crust and its Effect on Seismic Wide-Angle Reflection Fields ». Dans Heterogeneity in the Crust and Upper Mantle, 257–79. Boston, MA : Springer US, 2003. http://dx.doi.org/10.1007/978-1-4615-0103-9_10.
Texte intégralRumpel, Hanna-Maria, Claus Prodehl, Catherine M. Snelson et G. Randy Keller. « Results of the CD-ROM project seismic refraction/wide-angle reflection experiment : The upper and middle crust ». Dans The Rocky Mountain Region—An Evolving Lithosphere : Tectonics, Geochemistry, and Geophysics, 257–69. Washington, D. C. : American Geophysical Union, 2005. http://dx.doi.org/10.1029/154gm20.
Texte intégralVidal, N., J. Gallart, J. J. Dañobeitia et J. Diaz. « Mapping the Moho in the Iberian Mediterranean Margin by Multicoverage Processing and Merging of Wide-Angle and Near-Vertical Reflection Data ». Dans Rifted Ocean-Continent Boundaries, 291–308. Dordrecht : Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0043-4_16.
Texte intégralSnelson, Catherine M., G. Randy Keller, Kate C. Miller, Hanna-Maria Rumpel et Claus Prodehl. « Regional crustal structure derived from the CD-ROM 99 seismic refraction/wide-angle reflection profile : The lower crust and upper mantle ». Dans The Rocky Mountain Region—An Evolving Lithosphere : Tectonics, Geochemistry, and Geophysics, 271–91. Washington, D. C. : American Geophysical Union, 2005. http://dx.doi.org/10.1029/154gm21.
Texte intégralEpili, Duryodhan, et Robert F. Mereu. « The GLIMPCE seismic experiment : Onshore refraction and wide-angle reflection observations from a fan line over the Lake Superior Midcontinent Rift System ». Dans Properties and Processes of Earth' Lower Crust, 93–101. Washington, D. C. : American Geophysical Union, 1989. http://dx.doi.org/10.1029/gm051p0093.
Texte intégralJohnson, Roy A., et Kenneth A. Hartman. « Upper crustal poisson's ratios in the Colorado Plateau from multicomponent wide-angle seismic recording ». Dans Continental Lithosphere : Deep Seismic Reflections, 323–28. Washington, D. C. : American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0323.
Texte intégralGohl, Karsten, Scott B. Smithson et Yngve Kristoffersen. « The structure of the Archean crust in SW Greenland from seismic wide-angle data : A preliminary analysis ». Dans Continental Lithosphere : Deep Seismic Reflections, 53–57. Washington, D. C. : American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0053.
Texte intégralActes de conférences sur le sujet "Wide Angle Reflection"
Li, Yuan, et Jun hong Su. « Polarization-dependent, wide spectrum and wide-angle anti-reflection grating ». Dans Micro/Nano Optics, sous la direction de Xiaoliang Ma, Emmanuel Stratakis, Xiangang Luo, Minghui Hong, Mingbo Pu et Xiong Li. SPIE, 2021. http://dx.doi.org/10.1117/12.2604494.
Texte intégralBingyi Liu. « Wide-angle and full-angle negative reflection based on metasurfaces with specific surface phase gradient ». Dans 2016 Progress in Electromagnetic Research Symposium (PIERS). IEEE, 2016. http://dx.doi.org/10.1109/piers.2016.7734962.
Texte intégralGu, Tieer, Yiwei Lu, Johnny Q. Zhong, Rick Brinkley, Gang Xu, Willem den Boer et Scott V. Thomsen. « Low-reflection high-transmission wide-viewing-angle TFT-LCDs for avionics applications ». Dans Photonics China '98, sous la direction de Shou-Qian Ding et Bao Gang Wu. SPIE, 1998. http://dx.doi.org/10.1117/12.319690.
Texte intégralMakris, J., R. Boyce, M. Krieger, R. Garret et J. Thomas. « Wide angle reflection seismic mapping and velocity tomography of the Takutu Basin, Guyana ». Dans 54th EAEG Meeting. European Association of Geoscientists & Engineers, 1992. http://dx.doi.org/10.3997/2214-4609.201410483.
Texte intégralSchneider, William A., David Hays et Paul Docherty. « Wide azimuth reflection response in 3‐D angle gathers from OBS node data ». Dans SEG Technical Program Expanded Abstracts 2011. Society of Exploration Geophysicists, 2011. http://dx.doi.org/10.1190/1.3627866.
Texte intégralA. Minshull, T., G. D. Spence et C. R. Fink. « A Seismic Reflection and Wide-Angle Study of Methane Gas Hydrates, Offshore Vancouver Island ». Dans 57th EAEG Meeting. Netherlands : EAGE Publications BV, 1995. http://dx.doi.org/10.3997/2214-4609.201409199.
Texte intégralBotelho, Marco A., Irshad R. Mufti et Vicente P. Neto. « Multishot prestack depth migration : An application on wide‐angle reflection and refraction GPR data ». Dans SEG Technical Program Expanded Abstracts 1998. Society of Exploration Geophysicists, 1998. http://dx.doi.org/10.1190/1.1820166.
Texte intégralGuohua, Wei, Kong Qingfeng et Zuo Jianjun. « Research and application of wavelet reshaping to wide‐angle reflection in cross‐well seismic ». Dans Beijing 2009 International Geophysical Conference and Exposition. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3603633.
Texte intégralMaruyama, Tamami, Tatsuo Furuno, Yasuhiro Oda, Jiyun Shen, Ngochao Tran et Hidetoshi Kayama. « Design of wide angle reflection reflectarray using multi-layer mushroom structure to improve propagation ». Dans 2011 XXXth URSI General Assembly and Scientific Symposium. IEEE, 2011. http://dx.doi.org/10.1109/ursigass.2011.6050537.
Texte intégralIno, Shota, Takahiro Murai, Kunio Sakakibara et Nobuyoshi Kikuma. « Design of Metasurface Loaded in Multilayer Dielectric Plate to Reduce Reflection over Wide Incident Angle ». Dans 2019 International Workshop on Electromagnetics : Applications and Student Innovation Competition (iWEM). IEEE, 2019. http://dx.doi.org/10.1109/iwem.2019.8887881.
Texte intégralRapports d'organisations sur le sujet "Wide Angle Reflection"
Keen, C. E. Conversion of seismic-reflection time to depth for the Labrador margin, Davis Strait, and Baffin Bay, offshore northern Canada and Greenland, using sonic logs, checkshot surveys, and wide-angle seismic velocities. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/315016.
Texte intégral