Academic literature on the topic 'Wide Angle Reflection'

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Journal articles on the topic "Wide Angle Reflection"

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Shiraishi, Kazuya, Gou Fujie, Takeshi Sato, Susumu Abe, Eiichi Asakawa, and Shuichi Kodaira. "Interferometric OBS imaging for wide-angle seismic data." GEOPHYSICS 82, no. 5 (2017): Q39—Q51. http://dx.doi.org/10.1190/geo2016-0482.1.

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Marine wide-angle seismic data obtained using air guns and ocean-bottom seismographs (OBSs) are effective for determining large-scale subseafloor seismic velocities, but they are ineffective for imaging details of shallow seismic reflection structures because of poor illumination. Surface-related multiple reflections offer the potential to enlarge the OBS data illumination area. We have developed a new seismic imaging method for OBS surveys applying seismic interferometry, a technique that uses surface-related multiples similarly to mirror imaging. Seismic interferometry can use higher order m
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Zhu, Xinfa, та George A. McMechan. "Amplitude and phase versus angle for elastic wide-angle reflections in the τ‐p domain". GEOPHYSICS 80, № 1 (2015): N1—N9. http://dx.doi.org/10.1190/geo2013-0191.1.

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Near- and postcritical spherical-wave reflections contain amplitude and phase variations with incident angle that are not predicted by plane-wave solutions. However, if a spherical wavefield is decomposed into plane waves by a time-intercept-slowness ([Formula: see text]) transform, then plane-wave reflection coefficients (the Zoeppritz) can be used as the basis of amplitude/phase versus angle analysis. The spherical-wave effects on reflection coefficients near the critical angle (in the time-offset domain) were decomposed by [Formula: see text] transformation into plane waves. Kinematic ray t
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Rendleman, C. A., and F. K. Levin. "Reflection maxima for reflections from single interfaces." GEOPHYSICS 53, no. 2 (1988): 271–75. http://dx.doi.org/10.1190/1.1442462.

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At a workshop on refraction and wide‐angle reflections, Hilterman (1985) pointed out that, in contrast to the plane‐wave case, when there is a point source, a P-wave reflected from a plane interface attains its maximum amplitude at an offset greater than that corresponding to the critical angle (Figure 1). The same conclusion had been drawn earlier by Červený (1967). However, neither Červený’s results, which were based on very complicated mathematical expressions derived by Brekhovskikh (1960), nor Hilterman’s computer‐generated data shed light on the physics implied by the shifted maximum.
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Sava, Paul, and Ioan Vlad. "Wide-azimuth angle gathers for wave-equation migration." GEOPHYSICS 76, no. 3 (2011): S131—S141. http://dx.doi.org/10.1190/1.3560519.

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Extended common-image-point (CIP) gathers contain all of the necessary information for decomposition of reflectivity as a function of the reflection and azimuth angles at selected locations in the subsurface. This decomposition operates after the imaging condition applied to wavefields reconstructed by any type of wide-azimuth migration method, e.g., using downward continuation or time reversal. The reflection and azimuth angles are derived from the extended images using analytic relations between the space-lag and time-lag extensions. The transformation amounts to a linear Radon transform app
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Chang, Ya-Chun, Wei-Feng Xu, Meng-Chieh Wu, Cyun-Tai Hong, and Chen-Kuan Kuo. "P‐29: Wide Visual Angle Anti‐Reflection Film." SID Symposium Digest of Technical Papers 51, no. 1 (2020): 1442–44. http://dx.doi.org/10.1002/sdtp.14159.

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Fruehn, Juergen, Moritz M. Fliedner, and 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 (2001): 1340–48. http://dx.doi.org/10.1190/1.1487079.

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Acquiring large‐aperture seismic data (38 km maximum offset) along a profile crossing the Faeroe—Shetland basin in the North Atlantic enables us to use wide‐angle reflections and refractions, in addition to conventional streamer data (0–6 km), for subbasalt imaging. The wide‐angle results are complemented and confirmed by images obtained from the conventional near‐vertical‐offset range. Traveltime tomography applied to the wide‐angle data shows a low‐velocity layer (3.5–4.5 km/s) underneath southeastward‐thinning lava flows, suggesting a 2.5–3.0‐km‐thick sedimentary layer. The velocity model o
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Cao, Hao, Zhishuang Xue, Hongfeng Deng, Shuo Chen, Deming Wang, and Chengqun Gui. "Micromirror Array with Adjustable Reflection Characteristics Based on Different Microstructures and Its Application." Micromachines 15, no. 4 (2024): 506. http://dx.doi.org/10.3390/mi15040506.

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The conventional reflective optical surface with adjustable reflection characteristics requires a complex external power source. The complicated structure and preparation process of the power system leads to the limited modulation of the reflective properties and difficulty of use in large-scale applications. Inspired by the biological compound eye, different microstructures are utilized to modulate the optical performance. Convex aspheric micromirror arrays (MMAs) can increase the luminance gain while expanding the field of view, with a luminance gain wide angle > 90° and a field-of-view w
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Khalaj-Amirhosseini, Mohammad, and 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.

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Estakhri, Nasim Mohammadi, Verena Neder, Mark W. Knight, Albert Polman, and Andrea Alù. "Visible Light, Wide-Angle Graded Metasurface for Back Reflection." ACS Photonics 4, no. 2 (2017): 228–35. http://dx.doi.org/10.1021/acsphotonics.6b00965.

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Goldman, Ph.D., Laine. "Appreciative Reflection: A Wide-Angle Lens for Changing Perception." AI Practitioner 16, no. 3 (2014): 53–58. http://dx.doi.org/10.12781/978-1-907549-20-5-8.

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Dissertations / Theses on the topic "Wide Angle Reflection"

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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.

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Hananto, 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.

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Oueity, 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.

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High quality, coincident near-vertical incidence (NVI) and refraction/wide-angle seismic reflection data (R/WAR) acquired along a profile in the Northwest Territories are used to study the nature of the Moho and subcrustal reflectors. First, we re-examine distinct subhorizontal reflections on NVI data in the uppermost mantle that were interpreted previously as a separate feature from a relict subducted slab. Using forward and inverse traveltime modeling of both data sets along the crooked line, we investigate the origin of the reflections. Our results demonstrate that the subhorizontal reflect
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Hughes, 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.

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The Ontario-New York-New England seismic refraction/wide-angle reflection profile was acquired to investigate the deep structural interrelationships between the southeastern Grenville province and the western New England Appalachians. The Grenville province is characterized by 45 km thick crust, with an average crustal seismic velocity of 6.6 km/s and a Poisson's ratio of 0.28+0.01. In the mid-crust a laminated dome-like body is inferred to be composed of mafic cumulate sills on the basis of its high velocity (7.1 km/s) and Poisson's ratio (0.27). The lower crust is characterized by a velocity
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Meléndez, 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.

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This dissertation is devoted to seismic tomography. I have implemented a new modelling tool for 3-D joint refraction and reflection travel-time tomography of wide-angle seismic data (TOMO3D). The reason behind this central objective is the evidence that the information based on 2-D seismic data does not allow to capture the structural complexity of many 3-D targets, and in particular that of the seismogenic zone in subduction margins. The scientific rationale for this statement, which justifies the central part of my thesis work, is based on the analysis of 2-D models obtained in the convergen
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Biari, Youssef. "Structure profonde de la marge Nord-Ouest Africaine." Thesis, Brest, 2015. http://www.theses.fr/2015BRES0080/document.

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La marge NE Américaine est une des marges les mieux étudiées au monde, elle a fait l’objet de plusieurs études géophysiques. En comparaison, la marge africaine reste peu étudiée car uniquement deux campagnes océanographiques y ont été menées : la campagne Sismar (2001) au large de la Meseta et la campagne Dakhla (2002) au large du Sahara. La structure profonde de la marge canadienne est connue grâce aux profils de sismique grand-angle SMART-1, 2 et 3. Le premier objectif du projet MIRROR était d’acquérir des profils combinant sismique grand-angle et sismique réflexion sur un segment homologue
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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.

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Dans ce travail de thèse, nous analysons la structure crustale de la marge est-algérienne et du bassin adjacent (région d’Annaba), à partir d’un ensemble de nouvelles données acquises durant la Campagne SPIRAL’2009 incluant un profil sismique terre-mer de ~240 km de long, des lignes sismiques réflexion pénétrante 360-traces, et des profils gravimétriques et magnétiques. Nous avons par ailleurs disposé pour cette étude de données complémentaires incluant notamment un ensemble de profils de sismique réflexion offrant des résolutions complémentaires. La structure crustale ainsi établie nous perme
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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.

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Dans les zones de subduction, la géométrie du slab est l'un des paramètres qui contrôle les déformations tectoniques de la marge, le couplage et le potentiel sismogénique. La subduction des Antilles résulte du chevauchement de la plaque Caraïbe vers le NE sur les plaques Amériques, à une vitesse de convergence de 2 cm/an. La sismicité est hétérogène et augmente localement sous la plateforme des Iles Vierges. D’une obliquité croissante vers le nord, cette zone est favorable à un partitionnement dont les déformations sont très peu observées. Ces travaux ont permis de confirmer un substratum d’un
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Brancatelli, Giuseppe. "Analisi di dati acquisiti con OBS." Doctoral thesis, Università degli studi di Trieste, 2010. http://hdl.handle.net/10077/3458.

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2008/2009<br>Gli 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 o
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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.

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L'inversion des marges passives apparaît comme le premier stade vers l'initiation de nouvelles zones de subduction. Cette étape cruciale dans la tectonique des plaques soulève néanmoins encore de nombreuses questions. L'étude des marges actuellement réactivées en compression apparaît ainsi comme essentielle pour mieux comprendre ce processus. Ces marges sont peu nombreuses, situées dans des contextes géodynamiques variés, et les facteurs déterminant leur évolution mal contraints. Située au nord de l'Afrique, la marge algérienne fait partie de ces rares exemples potentiels à travers le monde. L
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Books on the topic "Wide Angle Reflection"

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J, Moses Michael, Tre hu Anne Martine, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Yosio, Nakamura, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Brocher, Thomas M. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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J, Moses Michael, Tréhu Anne Martine, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Yosio, Nakamura, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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J, Moses Michael, Tréhu Anne Martine, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Yosio, Nakamura, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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J, Moses Michael, Tréhu Anne Martine, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Yosio, Nakamura, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Yosio, Nakamura, and Geological Survey (U.S.), eds. Onshore-offshore wide-angle seismic recordings from central Oregon: The five-day recorder data. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Book chapters on the topic "Wide Angle Reflection"

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Braile, L. W., and C. S. Chiangl. "The continental Mohorovičič Discontinuity: Results from near-vertical and wide-angle seismic reflection studies." In Reflection Seismology: A Global Perspective. American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0257.

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Mereu, Robert, Dapeng Wang, and Oliver Kuhn. "Evidence for an inactive rift in the Precambrian from a wide-angle reflection survey across the Ottawa-Bonnechere graben." In Reflection Seismology: The Continental Crust. American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd014p0127.

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Ansorge, J., K. Holliger, P. Valasek, et al. "Integrated analysis of seismic normal incidence and wide-angle reflection measurements across the eastern Swiss Alps." In Continental Lithosphere: Deep Seismic Reflections. American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0195.

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Mereu, Robert. "The Heterogeneity of the Crust and its Effect on Seismic Wide-Angle Reflection Fields." In Heterogeneity in the Crust and Upper Mantle. Springer US, 2003. http://dx.doi.org/10.1007/978-1-4615-0103-9_10.

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Thiyagesan, M., B. Irfan, Ramakrishnan Raman, N. Ponnarasi, P. Ramakrishnan, and G. A. Senthil. "5G geological data for seismic inversion data detection based on wide-angle reflection wave technology." In Artificial Intelligence, Blockchain, Computing and Security Volume 1. CRC Press, 2023. http://dx.doi.org/10.1201/9781003393580-96.

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Rumpel, Hanna-Maria, Claus Prodehl, Catherine M. Snelson, and G. Randy Keller. "Results of the CD-ROM project seismic refraction/wide-angle reflection experiment: The upper and middle crust." In The Rocky Mountain Region—An Evolving Lithosphere: Tectonics, Geochemistry, and Geophysics. American Geophysical Union, 2005. http://dx.doi.org/10.1029/154gm20.

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Vidal, N., J. Gallart, J. J. Dañobeitia, and J. Diaz. "Mapping the Moho in the Iberian Mediterranean Margin by Multicoverage Processing and Merging of Wide-Angle and Near-Vertical Reflection Data." In Rifted Ocean-Continent Boundaries. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0043-4_16.

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Snelson, Catherine M., G. Randy Keller, Kate C. Miller, Hanna-Maria Rumpel, and Claus Prodehl. "Regional crustal structure derived from the CD-ROM 99 seismic refraction/wide-angle reflection profile: The lower crust and upper mantle." In The Rocky Mountain Region—An Evolving Lithosphere: Tectonics, Geochemistry, and Geophysics. American Geophysical Union, 2005. http://dx.doi.org/10.1029/154gm21.

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Epili, Duryodhan, and 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." In Properties and Processes of Earth' Lower Crust. American Geophysical Union, 1989. http://dx.doi.org/10.1029/gm051p0093.

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Tabyrtsa, S. N., A. S. Zholondz, and V. V. Polovkov. "Joint Processing Technology of MCS Data (600 m Streamer) and Wide-Angle Reflection/refraction Seismic Sonobuoy Soundings Acquired in Ice Conditions During Expedition “ARCTIKA-2014”." In Springer Proceedings in Earth and Environmental Sciences. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-47851-2_42.

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Conference papers on the topic "Wide Angle Reflection"

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Zhong, Jia-Li, You-Feng Cheng, Ting Shi, Xin-Long Bian, and Cheng Liao. "Wide-Angle Scanning and Backward Scattering-Reduced Phased Array Composed of Dual Anti-Reflection-Phase Elements." In 2024 IEEE 7th International Conference on Electronic Information and Communication Technology (ICEICT). IEEE, 2024. http://dx.doi.org/10.1109/iceict61637.2024.10671065.

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Luo, Huiling, Yanzhao Wang, Huanhuan Gao, Yanzhang Shao, and He-Xiu Xu. "Wide-angle Meta-reflector Using a Non-periodic Metasurface." In 2024 Photonics & Electromagnetics Research Symposium (PIERS). IEEE, 2024. http://dx.doi.org/10.1109/piers62282.2024.10618178.

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Abdani, Simon, Rajour Tanyi Ako, Madhu Bhaskaran, and Sharath Sriram. "Deep learning enhanced optimization of a broadband and wide-angle reflective linear terahertz polarization converter." In Metamaterials, Metadevices, and Metasystems 2024, edited by Nader Engheta, Mikhail A. Noginov, and Nikolay I. Zheludev. SPIE, 2024. http://dx.doi.org/10.1117/12.3028074.

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Ye, Ming-Jyun, Satoshi Ishii, and Kuo-Ping Chen. "Revisable Tuning of Tamm Plasmon Polaritons." In JSAP-Optica Joint Symposia. Optica Publishing Group, 2024. https://doi.org/10.1364/jsapo.2024.19a_p08_6.

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Phase-change materials (PCMs) provide a specific combination of properties. The binary semiconducting chalcogenide Sb2S3 is consider one of the promising candidates, especially its intrinsic high refractive index, low loss and wide bandgap properties, in near infrared (NIR). Here, the Sb2S3 transformation from amorphous to crystal state embedded between the distribute Bragg reflector (DBR) and metal layer. At the interface between DBR and metal layer in specific parameter, Phase-change Tamm plasmon–polariton (PC-TPP) resonance could be produce. The PC-TPP resonance has a 70 nm modulation wavel
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Li, Yuan, and Jun hong Su. "Polarization-dependent, wide spectrum and wide-angle anti-reflection grating." In Micro/Nano Optics, edited by Xiaoliang Ma, Emmanuel Stratakis, Xiangang Luo, Minghui Hong, Mingbo Pu, and Xiong Li. SPIE, 2021. http://dx.doi.org/10.1117/12.2604494.

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Zhang, Chuansheng, Xue-Xia Yang, and Guannan Tan. "1bit Coding Reflection Metasurface with Wide Incident Angle." In 2023 16th UK-Europe-China Workshop on Millimetre Waves and Terahertz Technologies (UCMMT). IEEE, 2023. http://dx.doi.org/10.1109/ucmmt58116.2023.10310410.

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Wang, Dan Yang, and Wei Xiang Jiang. "Wideband and Wide-Angle Anti-Reflection Coatings Based on Dielectric Metamaterials." In 2022 IEEE 10th Asia-Pacific Conference on Antennas and Propagation (APCAP). IEEE, 2022. http://dx.doi.org/10.1109/apcap56600.2022.10069993.

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Bingyi Liu. "Wide-angle and full-angle negative reflection based on metasurfaces with specific surface phase gradient." In 2016 Progress in Electromagnetic Research Symposium (PIERS). IEEE, 2016. http://dx.doi.org/10.1109/piers.2016.7734962.

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Gu, Tieer, Yiwei Lu, Johnny Q. Zhong, et al. "Low-reflection high-transmission wide-viewing-angle TFT-LCDs for avionics applications." In Photonics China '98, edited by Shou-Qian Ding and Bao Gang Wu. SPIE, 1998. http://dx.doi.org/10.1117/12.319690.

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Yamamoto, Hirotsugu. "Glass-Free Non-Contact Augmented Reality Interface With Aerial Imaging by Retro-Reflection (AIRR)." In Digital Holography and Three-Dimensional Imaging. Optica Publishing Group, 2023. http://dx.doi.org/10.1364/dh.2023.hm2d.2.

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A floating screen that is visible without glasses can be formed by utilizing retro-reflector to converge light from a wide angle. This paper reviews developments of non-contact AR interfaces with aerial imaging by retro-reflection (AIRR).
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Reports on the topic "Wide Angle Reflection"

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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.

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