Relevant bibliographies by topics / Geophysics Rocks Seismic reflection method

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Geophysics Rocks Seismic reflection method'

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Published: 4 June 2021
Last updated: 4 February 2022

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Journal articles on the topic "Geophysics Rocks Seismic reflection method"

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Heinonen, Suvi, Marcello Imaña, David B. Snyder, Ilmo T. Kukkonen, and Pekka J. Heikkinen. "Seismic reflection profiling of the Pyhäsalmi VHMS-deposit: A complementary approach to the deep base metal exploration in Finland." GEOPHYSICS 77, no. 5 (2012): WC15—WC23. http://dx.doi.org/10.1190/geo2011-0240.1.

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In the Pyhäsalmi case study, the seismic data is used in direct targeting of shallowly dipping mineralized zones in a massive sulfide ore system that was deformed in complex fold interference structures under high-grade metamorphic conditions. The Pyhäsalmi volcanic-hosted massive sulfide (VHMS) deposit ([Formula: see text]) is located in a Proterozoic volcanic belt in central Finland. Acoustic impedance of Pyhäsalmi ore ([Formula: see text]) is distinct from the host rocks ([Formula: see text]), enabling its detection with seismic reflection methods. Drill-hole logging further indicates that
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Kukkonen, I. T., S. Heinonen, P. Heikkinen, and P. Sorjonen-Ward. "Delineating ophiolite-derived host rocks of massive sulfide Cu-Co-Zn deposits with 2D high-resolution seismic reflection data in Outokumpu, Finland." GEOPHYSICS 77, no. 5 (2012): WC213—WC222. http://dx.doi.org/10.1190/geo2012-0029.1.

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Seismic reflection data was applied to a study of the upper crustal structures in the Outokumpu mining and exploration area in eastern Finland. The Cu-Co-Zn sulfide ore deposits of the Outokumpu area are hosted by Palaeoproterozoic ophiolite-derived altered ultrabasic rocks (serpentinite, skarn rock, and quartz rock) and black schist within turbiditic mica schist. Mining in the Outokumpu area has produced a total of 36 Mt of ore from three historical and one active mine. Seismic data comprises 2D vibroseis data surveyed along a network of local roads. The seismic sections provide a comprehensi
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Sexton, John L. "Seismic Reflection Expression of Reactivated Structures in the New Madrid Rift Complex." Seismological Research Letters 59, no. 4 (1988): 141–50. http://dx.doi.org/10.1785/gssrl.59.4.141.

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Abstract An important aspect of seismogenesis concerns the role of preexisting faults and other structural features as preferred zones of weakness in determining the pattern of strain accumulation and seismicity. Reactivation of zones of weakness by present day stress fields may be the cause of many intraplate earthquakes. To understand the relation between reactivated structures and seismicity, it is necessary to identify structures which are properly oriented with respect to the present-day stress field so that reactivation can occur. The seismic reflection method is very useful for identify
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Carcione, José M., Hans B. Helle, Nam H. Pham, and Tommy Toverud. "Pore pressure estimation in reservoir rocks from seismic reflection data." GEOPHYSICS 68, no. 5 (2003): 1569–79. http://dx.doi.org/10.1190/1.1620631.

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A method is used to obtain pore pressure in shaly sandstones based upon an acoustic model for seismic velocity versus clay content and effective pressure. Calibration of the model requires log data—porosity, clay content, and sonic velocities—to obtain the dry‐rock moduli and the effective stress coefficients as a function of depth and pore pressure. The seismic P‐wave velocity, derived from reflection tomography, is fitted to the theoretical velocity by using pore pressure as the fitting parameter. This approach, based on a rock‐physics model, is an improvement over existing pore‐pressure pre
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White, Don, David Boerner, Jianjun Wu, et al. "Mineral exploration in the Thompson nickel belt, Manitoba, Canada, using seismic and controlled‐source EM methods." GEOPHYSICS 65, no. 6 (2000): 1871–81. http://dx.doi.org/10.1190/1.1444871.

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Seismic reflection and electromagnetic (EM) data were acquired near Thompson, Manitoba, Canada, to map the subsurface extent of the Paleoproterozoic, nickel ore‐bearing Ospwagan Group. These data are supplemented by surface and borehole geology and by laboratory measurements of density, seismic velocity, and electrical conductivity, which indicate that Ospwagan Group rocks are generally more seismically reflective and electrically conductive than the Archean basement rocks that envelop them. The combined seismic/EM interpretation suggests that the Thompson Nappe (cored by Ospwagan Group rocks)
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Li, Tonglin, and David W. Eaton. "Delineating the Tuwu porphyry copper deposit at Xinjiang, China, with seismic-reflection profiling." GEOPHYSICS 70, no. 6 (2005): B53—B60. http://dx.doi.org/10.1190/1.2122409.

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The Tuwu deposit is one of a series of recently discovered porphyry copper deposits in the eastern Tian Shan range of Xinjiang, China. Since its discovery in 1997, more than ten boreholes have been drilled and a suite of geophysical surveys has been acquired to delineate the deposit. As part of the geophysical program, a set of eight seismic reflection profiles was acquired in 2000, followed by a physical rock-property study in 2001. The ores are characterized by slightly higher density (Δρ ∼ 0.1 g/cm[Formula: see text]) and significantly higher P-wave velocity ([Formula: see text] ∼ 1.0–1.5 k
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Louie, J. N., and J. E. Vidale. "Array analysis of reflector heterogeneity." GEOPHYSICS 56, no. 4 (1991): 565–71. http://dx.doi.org/10.1190/1.1443074.

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In deep crustal reflection study, as in conventional exploration seismology, it is important to determine the geometry of the physical contrasts between rocks that cause reflections, to make reliable geologic interpretations. Fundamentally different reflecting structures produce similar signatures in stacked seismic sections. We have developed a method that uses prestack records to differentiate lateral structural variations from lateral reflectivity variations and laterally homogeneous structures. Full‐wave acoustic multioffset synthetics of canonical 2-D reflector configurations, analyzed by
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Berryman, James G., Patricia A. Berge, and Brian P. Bonner. "Estimating rock porosity and fluid saturation using only seismic velocities." GEOPHYSICS 67, no. 2 (2002): 391–404. http://dx.doi.org/10.1190/1.1468599.

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Evaluation of the fluid content in deep earth reservoirs or fluid contaminants in shallow earth environments has required the use of geophysical imaging methods such as seismic reflection prospecting. Interpretation of seismic velocities and amplitudes is based on theories of fluid‐saturated and partially saturated rocks that have been available since the 1950s. Here we present a new synthesis of the same physical concepts that uses compressional‐wave velocities together with shear‐wave velocities in a scheme that is much simpler to understand and apply yet yields detailed information about po
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Hardage, Bob, Mike Graul, Tim Hall, et al. "Determining fast-S and slow-S propagation directions with SV-P data produced by buried explosives and recorded with vertical geophones." Interpretation 9, no. 2 (2021): T599—T609. http://dx.doi.org/10.1190/int-2020-0226.1.

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We have evaluated the concept of practicing S-wave reflection seismology with legacy 3D seismic data generated by a P-wave source and recorded with only vertical geophones. This type of S-wave imaging is based on the principle that seismic P-wave sources not only produce a downgoing illuminating P wavefield, but they also simultaneously produce a downgoing illuminating SV wavefield that, in almost all cases, is suitable for S-wave reflection imaging. The S-mode used in this study is the SV-P, or converted-P, mode. This mode involves a downgoing illuminating SV wavefield and an upgoing reflecte
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Mitchell, James F., and Richard J. Bolander. "Structural interpretation using refraction velocities from marine seismic surveys." GEOPHYSICS 51, no. 1 (1986): 12–19. http://dx.doi.org/10.1190/1.1442026.

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Subsurface structure can be mapped using refraction information from marine multichannel seismic data. The method uses velocities and thicknesses of shallow sedimentary rock layers computed from refraction first arrivals recorded along the streamer. A two‐step exploration scheme is described which can be set up on a personal computer and used routinely in any office. It is straightforward and requires only a basic understanding of refraction principles. Two case histories from offshore Peru exploration demonstrate the scheme. The basic scheme is: step (1) shallow sedimentary rock velocities ar
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Dissertations / Theses on the topic "Geophysics Rocks Seismic reflection method"

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Zaske, Jörg Helmut. "Identification and attenuation of multiple reflections using wavefront characteristics /." [Karlsruhe] : Die Universität, 2000. http://www.ubka.uni-karlsruhe.de/cgi-bin/psgunzip/2000/physik/1/1.pdf.

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Thesis (Doctoral)--Universität Karlsruhe, 2000.<br>Abstract in German. Includes bibliographical references (p. 107-111). Also available via the World Wide Web. Also available via the World Wide Web. http://www.ubka.uni-karlsruhe.de/cgi-bin/psview?document=2000/physik/1 http://www.ubka.uni-karlsruhe.de/cgi-bin/psview?document=/2000/physik/2
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Vieth, Kai-Uwe. "Kinematic wavefield attributes in seismic imaging /." [Karlsruhe] : Die Universität, 2001. http://www.ubka.uni-karlsruhe.de/vvv/2001/physik/2/2.pdf.

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Kirchner, Andreas. "Efficient repeat-modelling of time-lapse seismograms for reservoir monitoring /." [Karlsruhe] : Die Universität, 2001. http://www.ubka.uni-karlsruhe.de/vvv/2001/physik/2/2.pdf.

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Thesis (Doctoral)--Universität Karlsruhe, 2000.<br>Abstract in German. Hochschulschrift = Thèse/Mémoire. Also available via the World Wide Web. http://www.ubka.uni-karlsruhe.de/cgi-bin/psview?document=2001/physik/2
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Bergman, Björn. "High-Resolution Seismics Methods Applied to Till Covered Hard Rock Environments." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-4811.

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<p>Reflection seismic and seismic tomography methods can be used to image the upper kilometer of hard bedrock and the loose unconsolidated sediments covering it. Developments of these two methods and their application, as well as identifying issues concerning their usage, are the main focus of the thesis. Data used for this development were acquired at three different sites in Sweden, in Forsmark 140 km north of Stockholm, in the Oskarshamn area in southern Sweden, and in the northern part of the Siljan Ring impact crater area.</p><p>The reflection seismic data were acquired with long source-r
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Ecevitoglu, Berkan G. "Velocity and Q from reflection seismic data." Diss., Virginia Polytechnic Institute and State University, 1987. http://hdl.handle.net/10919/77793.

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This study has resulted in the discovery of an exact method for the theoretical formulation of the effects of intrinsic damping where the attenuation coefficient, a(v), is an arbitrary function of the frequency, v. Absorption-dispersion pairs are computed using numerical Hilbert transformation; approximate analytical expressions that require the selection of arbitrary constants and cutoff frequencies are no longer necessary. For constant Q, the dispersive body wave velocity, p(v), is found to be p(v) = (p(v<sub>N</sub>)/(1+(1/2Q H(-v)/v)) where H denotes numerical Hilbert transformation, p(
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Gamboa, Fernando, and Universidade Estadual de Campinas Faculdade de Engenharia Mecânica Programa de Pós-Graduação em Ciências e. Engenharia de Petróleo. "Aplicações do metodo de superficie comum de reflexão (CRS) ao processamento sísmico." [s.n.], 2007. http://repositorio.unicamp.br/jspui/handle/REPOSIP/265465.

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Orientador: Martin Tygel<br>Tese (doutorado) - Universidade Estadual de Campinas, Facudade de Engenharia Mecanica e Instituto de Geociencias<br>Made available in DSpace on 2018-08-12T05:48:28Z (GMT). No. of bitstreams: 1 UniversidadeEstadualdeCampinas.FaculdadedeEngenhariaMecanica.ProgramadePos-GraduacaoemCienciaseEngenhariadePetroleo_D.pdf: 5963808 bytes, checksum: 11070db7b13faf0139f14fda5d6a4fb6 (MD5) Previous issue date: 2007<br>Resumo: O método Common Reflection Surface (CRS) tem por objetivo a obtenção de seções empilhadas de qualidade e extração de parâmetros do campo de onda que cara
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Kamioka, Daniela Midori 1984. "Uma comparação entre semblances no método de ponto médio comum." [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/306034.

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Orientadores: Maria Amélia Novais Schleicher, Lúcio Tunes dos Santos<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Matemática Estatística e Computação Científica<br>Made available in DSpace on 2018-08-25T10:12:39Z (GMT). No. of bitstreams: 1 Kamioka_DanielaMidori_M.pdf: 9312784 bytes, checksum: cd5e7b440a4b44168749d7cc069f1ac0 (MD5) Previous issue date: 2014<br>Resumo: Uma das principais etapas do processamento sísmico é a análise de velocidade. Essa é uma das técnicas que utilizam dados sísmicos organizados em famílias de ponto médio comum (CMP ¿ Common Midpoin
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Rueda, Serrano Dany 1982. "Random noise reduction by smoothing of CRS attributes = Redução do ruído aleatório mediante a suavização dos atributos CRS." [s.n.], 2013. http://repositorio.unicamp.br/jspui/handle/REPOSIP/262949.

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Orientador: Martin Tygel<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Faculdade de Engenharia Mecânica e Instituto de Geociências<br>Made available in DSpace on 2018-08-23T04:02:48Z (GMT). No. of bitstreams: 1 RuedaSerrano_Dany_M.pdf: 36981147 bytes, checksum: 4818cdd1a4fd5bda74072b4e6d58a7ba (MD5) Previous issue date: 2013<br>Resumo: A razão sinal-ruído, geralmente abreviada por razão S/N (do Inglês signal-to-noise ratio) é bastante afetada por ruídos aleatórios, os quais degradam a continuidade e identificação de refletores, com prejuízos para interpretação geológica. Com
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Faccipieri, Junior Jorge Henrique 1983. "Separação e processamento de difrações em dados geofísicos de reflexão." [s.n.], 2012. http://repositorio.unicamp.br/jspui/handle/REPOSIP/262953.

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Orientador: Martin Tygel<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Faculdade de Engenharia Mecânica e Instituto de Geociências<br>Made available in DSpace on 2018-08-21T00:35:26Z (GMT). No. of bitstreams: 1 FaccipieriJunior_JorgeHenrique_M.pdf: 11845729 bytes, checksum: 1c69f6a509b40bc499fe38630fb28be9 (MD5) Previous issue date: 2012<br>Resumo: O método de empilhamento Common Reflection Surface (CRS) permite obter seções de afastamento nulo simuladas de maior qualidade e extrair um maior número de atributos que caracterizam o meio geológico que o tradicional método de em
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Kulkarni, Mandar S. "Multi-coefficient Dirichlet Neumann type elliptic inverse problems with application to reflection seismology." Birmingham, Ala. : University of Alabama at Birmingham, 2009. https://www.mhsl.uab.edu/dt/2010r/kulkarni.pdf.

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Thesis (Ph. D.)--University of Alabama at Birmingham, 2009.<br>Title from PDF t.p. (viewed July 21, 2010). Additional advisors: Thomas Jannett, Tsun-Zee Mai, S. S. Ravindran, Günter Stolz, Gilbert Weinstein. Includes bibliographical references (p. 59-64).
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Books on the topic "Geophysics Rocks Seismic reflection method"

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Baker, Gregory S. Processing near-surface seismic-reflection data: A primer / Gregory S. Baker. Society of Exploration Geophysicists, 1999.

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Gogonenkov, G. N. Seismic prospecting for sedimentary formations. A.A. Balkema, 1990.

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Seismic prospecting for sedimentary formations. Oxford & IBH Pub. Co., 1990.

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Imaging the earth's interior. Blackwell Scientific Publications, 1985.

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European Association of Exploration Geophysicists. Meeting. Technical programme and abstracts of papers (oral and poster presentations: 54th Meeting and Technical Exhibition, Paris, France, 1 - 5 June 1992. European Association of Exploration Geophysicists, 1992.

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European Association of Exploration Geophysicists. Meeting. Technical programme and abstracts of papers (oral and poster presentations: 53rd Meeting and Technical Exhibition, Florence, Italy, 26 May-30 May 1991. European Association of Exploration Geophysicists, 1991.

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European Association of Exploration Geophysicists. Meeting. Technical programme and abstracts of papers (oral and poster presentations: 54th Meeting and Technical Exhibition, Paris, France, 1 - 5 June 1992. European Association of Exploration Geophysicists, 1992.

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Gogonenkov, G. N. Izuchenie detalʹnogo stroenii͡a︡ osadochnykh tolshch seĭsmorazvedkoĭ. "Nedra", 1987.

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McGee, Thomas Martin. Single-channel marine seismic profiling and the analysis of reverberatory sequences =: Eén-kanaals marien seismisch onderzoek en de analyse van resonantie in tijdreeksen. Faculteit Aardwetenschappen der Rijksuniversiteit Utrecht, 1991.

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Juhlin, Christopher. Seismic attenuation, shear wave anisotropy and some aspects of fracturing in the crystalline rock of the Siljan Ring Area, Central Sweden. Academia Upsaliensis, 1990.

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Book chapters on the topic "Geophysics Rocks Seismic reflection method"

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Baojun, Yang, Liu Cai, Han Liguo, Zhang Haijiang, and He Min. "A Study of Detachment Faults of the Upper Crust in Manzhouli-Suifenhe GGT by the Method of Vertical Seismic Reflection." In Geophysics. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070853-5.

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Conference papers on the topic "Geophysics Rocks Seismic reflection method"

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Osukuku, Godfred, Abiud Masinde, Bernard Adero, Edmond Wanjala, and John Ego. "Integrated Geophysical Interpretation of Kerio Valley Basin Stratigraphy, Kenya Rift." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2670415-ms.

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Abstract This research work attempts to map out the stratigraphic sequence of the Kerio Valley Basin using magnetic, gravity and seismic data sets. Regional gravity data consisting of isotactic, free-air and Bouguer anomaly grids were obtained from the International Gravity Bureau (BGI). Magnetic data sets were sourced from the Earth Magnetic Anomaly grid (EMAG2). The seismic reflection data was acquired in 1989 using a vibrating source shot into inline geophones. Gravity Isostacy data shows low gravity anomalies that depict a deeper basement. Magnetic tilt and seismic profiles show sediment t
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McClymont, Alastair, Erin Ernst, Paul Bauman, and Nicholas Payne. "Integrating Geophysical and Geotechnical Engineering Methods for Assessment of Pipeline Geohazards." In 2016 11th International Pipeline Conference. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/ipc2016-64222.

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Because pipelines can cover extensive distances through diverse terrain, they are subject to various geohazards, including slope failure and earthquake damage, which can have costly environmental and monetary impacts over their designed operational lifetime. Here, we show how geophysical investigative techniques can be used to complement other geotechnical investigation methods to provide a detailed understanding of site geology to best inform geohazard assessments. We pay particular attention to how multiple geophysical methods can be used to obtain spatially continuous measurements of subsur
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Gorelik, G., L. Budanov, D. Ryabchuk, V. Zhamoida, and I. Neevin. "Application of Cdp Seismic Reflection Method in Buried Paleo-Valley Study." In Engineering and Mining Geophysics 2019 15th Conference and Exhibition. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201901777.

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Turchkov, A. M., A. N. Oshkin, I. P. Korotkov, E. A. Keldyushova, and A. A. Vyaznikovcev. "Using Areal Common Depth-Point (CMP) Seismic Reflection Method for Additional Exploration of the Coal Field." In Engineering and Mining Geophysics 2020. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202051148.

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Chunlin, Xie, Gu Haiyan, Wang Zihe, Liu Weiwei, Hu Jiuzhan, and Li Yongyi. "Thin beds prediction method in the context of strong seismic reflection shielding." In SEG 2018 Workshop: Reservoir Geophysics, Daqing, China, 5-7 August 2018. Society of Exploration Geophysicists and the Chinese Geophysical Society, 2018. http://dx.doi.org/10.1190/rege2018-45.1.

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Scholtz, P., and G. Szőts. "Enhanced Q Estimation by Iterative Spectral Ratio Method for High Resolution Seismic Reflection Image." In 24th European Meeting of Environmental and Engineering Geophysics. EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201802565.

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Ito, Shunichiro, Takao Aizawa, Fumio Nakada, and Ryosuke Kitamura. "Detecting Abandoned Air‐Raid Shelter Using the S‐Wave Seismic Reflection Method." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2008. Environment and Engineering Geophysical Society, 2008. http://dx.doi.org/10.4133/1.2963219.

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Maraio, S., P. P. G. Bruno, and V. Picotti. "High Resolution Seismic Imaging in Alpine Environment by Common Reflection Surface Method." In Near Surface Geoscience 2015 - 21st European Meeting of Environmental and Engineering Geophysics. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413774.

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Ito, Shunichiro, Takao Aizawa, Fumio Nakada, and Ryosuke Kitamura. "Detecting Abandoned Air-Raid Shelter Using The S-Wave Seismic Reflection Method." In 21st EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.177.33.

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Zhong, Shihang. "A New Version of Seismic Wave Reflection Method Fit for Urban Exploration — Landsonar." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2011. Environment and Engineering Geophysical Society, 2011. http://dx.doi.org/10.4133/1.3614103.

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