Relevant bibliographies by topics / Virtual reflection seismic profiling

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
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Academic literature on the topic 'Virtual reflection seismic profiling'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Virtual reflection seismic profiling"

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Poletto, Flavio, and Biancamaria Farina. "Synthesis and composition of virtual-reflector (VR) signals." GEOPHYSICS 75, no. 4 (July 2010): SA45—SA59. http://dx.doi.org/10.1190/1.3433311.

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The virtual-reflector (VR) method creates new seismic signals by processing seismic traces that have been produced by impulsive or transient sources. Under proper recording-coverage conditions, this technique allows a seismogram to be obtained as if there were an ideal reflector at the position of the receivers (or sources). Only the reflected signals from this reflector are synthesized. The algorithm is independent of the medium-velocity model and is based on convolution of the recorded traces and on subsequent integration of the crossconvolved signals in the receiver (or source) space. We use the VR method in combination with seismic interferometry (SI) by crosscorrelation to compose corresponding virtual-reflection events in seismic exploration. For that purpose, we use weighted-summation and data-crossfiltering approaches. In applying these combination methods, we assume common travel paths in the virtual signals, taking into account that VR and SI by crosscorrelation imply different stationary-phase conditions. We present applications in which we combine the SI-by-crosscorrelation and VR signals to (1) suppress unwanted effects, such as marine water-layer reflections in synthetic ocean-bottom-cable data, and (2) obtain virtual two-way traveltime seismograms with real borehole data from walkaway vertical seismic profiling (VSP). Analysis shows that time gating and selection of reflection events are critical steps in processing water-layer multiples.
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Finlay, Tori S., Lindsay L. Worthington, Brandon Schmandt, Nishath R. Ranasinghe, Susan L. Bilek, and Richard C. Aster. "Teleseismic Scattered‐Wave Imaging Using a Large‐N Array in the Albuquerque Basin, New Mexico." Seismological Research Letters 91, no. 1 (October 30, 2019): 287–303. http://dx.doi.org/10.1785/0220190146.

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Abstract The advent of low‐cost continuously recording cable‐free autonomous seismographs, commonly referred to as nodes, enables dense spatiotemporal sampling of seismic wavefields. We create virtual source reflection profiles using P waves from five teleseismic events recorded by the Sevilleta node array experiment in the southern Albuquerque basin. The basin geology records a structurally complex history, including multiple Phanerozoic orogenies, Rio Grande rift extension, and ongoing uplift from a midcrustal magma body. The Sevilleta experiment densified the long term, regionally sparse seismograph network with 801 single channel vertical‐component 10 Hz geophone nodes deployed at ∼300 m spacing for 14 days in February 2015. Results show sediment‐basement reflections at <5 km depth and numerous sub‐basin structures. Comparisons to legacy crustal‐scale reflection images from the Consortium for Continental Reflection Profiling show agreement with structural geometries in the rift basin and upper crust. Comparisons of the teleseismic virtual reflection profiles to synthetic tests using 2D finite‐difference elastic wave propagation show strong P‐to‐Rayleigh scattering from steep basin edges. These high‐amplitude conversions dominate the record sections near the western rift margin and originate at the Loma Pelada fault, which acts as the primary contact between rift‐bounding basement‐cored fault blocks and rift basin sediments. At near offsets, these signals may interfere with interpretation of upper crustal structure, but their relatively slow moveout compared to teleseismic P‐wave multiples provides clear temporal separation from sediment‐basement reflections across most of the array. The high‐signal‐to‐noise ratio of these converted Rayleigh‐wave signals suggests that they may be useful for constraining short‐period (∼1 Hz) dispersion with strong sensitivity in the uppermost ∼1 km of the rift basin sediments.
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Zhang, Kai, Hongyi Li, Xiaojiang Wang, and Kai Wang. "Retrieval of shallow S-wave profiles from seismic reflection surveying and traffic-induced noise." GEOPHYSICS 85, no. 6 (November 1, 2020): EN105—EN117. http://dx.doi.org/10.1190/geo2019-0845.1.

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In urban subsurface exploration, seismic surveys are mostly conducted along roads where seismic vibrators can be extensively used to generate strong seismic energy due to economic and environmental constraints. Generally, Rayleigh waves also are excited by the compressional wave profiling process. Shear-wave (S-wave) velocities can be inferred using Rayleigh waves to complement near-surface characterization. Most vibrators cannot excite seismic energy at lower frequencies (<5 Hz) to map greater depths during surface-wave analysis in areas with low S-wave velocities, but low-frequency surface waves ([Formula: see text]) can be extracted from traffic-induced noise, which can be easily obtained at marginal additional cost. We have implemented synthetic tests to evaluate the velocity deviation caused by offline sources, finding a reasonably small relative bias of surface-wave dispersion curves due to vehicle sources on roads. Using a 2D reflection survey and traffic-induced noise from the central North China Plain, we apply seismic interferometry to a series of 10.0 s segments of passive data. Then, each segment is selectively stacked on the acausal-to-causal ratio of the mean signal-to-noise ratio to generate virtual shot gathers with better dispersion energy images. We next use the dispersion curves derived by combining controlled source surveying with vehicle noise to retrieve the shallow S-wave velocity structure. A maximum exploration depth of 90 m is achieved, and the inverted S-wave profile and interval S-wave velocity model obtained from reflection processing appear consistent. The data set demonstrates that using surface waves derived from seismic reflection surveying and traffic-induced noise provides an efficient supplementary technique for delineating shallow structures in areas featuring thick Quaternary overburden. Additionally, the field test indicates that traffic noise can be created using vehicles or vibrators to capture surface waves within a reliable frequency band of 2–25 Hz if no vehicles are moving along the survey line.
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Hurich, Charles, and Sharon Deemer. "Combined surface and borehole seismic imaging in a hard rock terrain: A field test of seismic interferometry." GEOPHYSICS 78, no. 3 (May 1, 2013): B103—B110. http://dx.doi.org/10.1190/geo2012-0325.1.

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Seismic images are inherently directionally biased by the source-receiver geometry. This directional bias is particularly problematic for seismic imaging in hard rock terrains where structural dips may have any orientation with respect to the surface. We tested a technique for partially mitigating directional bias by combining surface and borehole seismic data and evaluated the results of a first field test of the technique. In this technique, surface data acquired using standard 2D acquisition procedures were combined with borehole data derived from a walk-away vertical seismic profile (VSP). The VSP data were transformed into the borehole datum using seismic interferometry. The interferometry created virtual shot records comprising sources and receivers in the borehole. The virtual shot records were then processed, using standard common midpoint techniques, resulting in an image from the borehole datum. The combination of the surface and borehole data increased the range of illumination angles resulting in seismic images that included reflections from structures with a wider range of dips than is available to surface profiling alone. The field test demonstrated that the surface and borehole data provide complementary information, which is more than either data set alone can provide. The test also verified the robustness of the virtual source technique even when the original VSP data are highly contaminated by high-amplitude tube waves. These results demonstrated that the combined imaging approach has significant potential for application in the polydeformed hard rock domains often encountered in minerals exploration.
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White, Robert S. "Seismic reflection profiling comes of age." Geological Magazine 122, no. 2 (March 1985): 199–201. http://dx.doi.org/10.1017/s0016756800031149.

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Pugin, Andre J. M., Susan E. Pullan, and James A. Hunter. "Multicomponent high-resolution seismic reflection profiling." Leading Edge 28, no. 10 (October 2009): 1248–61. http://dx.doi.org/10.1190/1.3249782.

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ASANO, Shuzo, Tomohiko TSUNODA, Kunioki HIRAMA, Toru KUWAHARA, Yuzuru YASUI, Takeshi IKAWA, Tohru KURODA, Akihisa TAKAHASHI, Ikuhisa ADACHI, and Takao NIHEI. "Seismic Reflection Profiling in Kiyose, Tokyo Metropolis." Zisin (Journal of the Seismological Society of Japan. 2nd ser.) 44, no. 2 (1991): 131–43. http://dx.doi.org/10.4294/zisin1948.44.2_131.

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Wright, C., R. J. Korsch, D. M. Finlayson, and B. R. Goleby. "Deep seismic reflection profiling and continental evolution." Eos, Transactions American Geophysical Union 70, no. 23 (1989): 639. http://dx.doi.org/10.1029/89eo00187.

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Stadtlander, Ralf, and Larry Brown. "Turning waves and crustal reflection profiling." GEOPHYSICS 62, no. 1 (January 1997): 335–41. http://dx.doi.org/10.1190/1.1444135.

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In the past, steeply dipping features were often recognized on seismic reflection profiles only from indirect evidence such as vertical offsets of cross‐cutting structures. New imaging algorithms, as for example, turning wave migration have had dramatic success in delineating steep, even‐overturned reflectors in sedimentary environments. Evaluation of the applicability of this technology to deep seismic recordings indicates that steep‐dip and turning wave migration will have limited practicality, generally, in the imaging of basement features because of the weak velocity gradients involved and the corollary requirement for large recording offsets. A potential exception arises when the basement structures to be imaged lie beneath a significant thickness of relatively young (i.e., steep velocity gradient) sedimentary cover.
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Vejmelek, Libor, and Scott B. Smithson. "Seismic reflection profiling in the Boulder batholith, Montana." Geology 23, no. 9 (1995): 811. http://dx.doi.org/10.1130/0091-7613(1995)023<0811:srpitb>2.3.co;2.

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Dissertations / Theses on the topic "Virtual reflection seismic profiling"

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Stoch, Agnieszka. "Analysis of Seismic Data Acquired in the Hverahlíð Geothermal Area." Thesis, Uppsala universitet, Geofysik, 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-413199.

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Volcanic rifting environments, such as in Iceland, are challenging for conventional seismic reflection methods using active surface seismic sources. This study demonstrates the potential of a novel technique, called Virtual Reflection Seismic Profiling (VRSP) for imaging reflections in geothermal regions, like Hverahlíð, where a dense seismic array recorded a number of local microearthquakes for cross-correlation. Uppsala University, in collaboration with Reykjavik Energy, recorded seismicity in Hverahlíð using both seismometers and geophones. Acquired data were processed using the VRSP method, which applies seismic interferometry only to selected events, in this thesis local microearthquakes. Cross-correlation of the signal from a microearthquake recorded at one of the stations, which acts as a virtual source, with a ghost reflection recorded by the remaining receivers, produces a virtual shot gather. Stacking each station’s result, for all available events, and following a conventional multichannel processing sequence resulted in two stacked seismic images. Potential reflections observed in the obtained sections could be associated with major feed zones identified in the area by the borehole measurements. Eight dynamite explosions were processed with a conventional seismic reflection method, as a complementary source to the microearthquakes. In the produced stacked seismic section two potential reflections could be observed. Results from both passive and active datasets were 3D visualised to verify whether the reflections correspond to each other between sections. Two horizons were traced throughout all three stacked sections. One more interface appeared on two images obtained from processing the passive data. This study shows promising results for using natural sources to image the subsurface in a challenging environment.
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Al-Rawahy, Salim Y. S. "Effects of mining subsidence observed by time-lapse seismic reflection profiling." Thesis, Durham University, 1995. http://etheses.dur.ac.uk/5125/.

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Extracting coal from underground mineworkings causes the overlying rocks to subside with associated changes in the stress regime. The aim of the study reported here was to apply the surface seismic reflection method to study the effect of subsidence on seismic velocity. Two sets of time-lapse surveys were carried out over two longwall mining panels in the Selby Coalfield. Seismic lines were profiled parallel and perpendicular to adjacent panels H45 and H46, respectively. A total of twenty-one repeated surveys were carried out along the two lines over a period of three years. The effect monitored was due to mining in the Bamsley Seam, at 550 m depth. As mining progressed, the traveltime of a strong reflection event from an anhydrite bed at 150 m depth was measured after processing the data with standard techniques. An overall increase in traveltime of about 4 % was observed. The progressive increase in traveltime over panel H45 correlated well with empirical calculations of differential subsidence between the surface and the anhydrite. However, the magnitude of the change must principally be accounted for by a decrease in seismic velocity, associated with a reduction in the vertical effective stress. Although the traveltime over panel H46 was also found to increase, and to correlate quite well with die expected differential subsidence, the agreement was less good along this transverse profile. This is attributed to asymmetric subsidence effects because the ground on the SW side of the panel had already been worked by panel H45, but the ground on the NE side was unworked. At the time of each seismic survey across panel H46, the profile was also levelled, and it was found that surface subsidence values along the profile increased towards panel H45. As most of the subsidence caused by mining panel H45 would have been completed by the time the H46 profile was surveyed, the effect must be at least partly attributed to asymmetric subsidence due to panel H46. Where the ground had been weakened by subsidence due to mining H45, near-total subsidence from mining H46 took place rapidly; but in the previously unworked ground on the NE side of panel H46, the residual subsidence was presumably delayed by competent strata in the overburden. Further work is needed to confirm whether this explanation is correct.
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Ward, Gavin Stuart. "Deep reflection seismics using S-waves on land." Thesis, University of Cambridge, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.387057.

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Williamson, P. R. "Tomographic inversion of traveltime data in reflection seismology." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383956.

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Peterman, David Joseph. "Seismic Reflection Profiling near Middletown, Ohio and Interpretation of Precambrian Deformational Settings." Wright State University / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=wright1463936515.

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Stäuble, Martin Peter. "Seismic reflection profiling from the molasse basin into the Alps of Eastern Switzerland : processing, interpretation and modeling /." [S.l : s.n.], 1990. http://www.ub.unibe.ch/content/bibliotheken_sammlungen/sondersammlungen/dissen_bestellformular/index_ger.html.

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Diss. Phil.-naturwiss. Fak. Bern, 1990.
Enth. Sonderabdrucke: Tectonics vol.9/6: 1327-1355 (1990), Annales tectonicae vol. V/1 3-17 (1991), Eclogae geologicae Helvetiae vol.84/1 151-175 (1991), und Tectonics vol.12 (1993).
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Steht, Markus von. "Imaging of vertical seismic profiling data using the common-reflection-surface stack Abbildungsverfahren für seismische Daten aus Bohrlochmessungen mit der Common-Reflection-Surface Stapelung /." [S.l. : s.n.], 2008. http://digbib.ubka.uni-karlsruhe.de/volltexte/1000007747.

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Frommel, Jamin C. "INTEGRATED GEOPHYSICAL INVESTIGATION OF KARST FEATURES – INNER BLUEGRASS REGION OF KENTUCKY." UKnowledge, 2012. http://uknowledge.uky.edu/ees_etds/5.

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High-resolution electrical-resistivity, seismic-refraction, and seismic-reflection surveys were performed at three locations in the Inner Bluegrass Region of Kentucky along coincident survey lines in order to correlate results and determine which method is most effective at locating karst features in this area. The first two survey locations at Slack’s Cave and the Kentucky Horse Park were chosen in order to investigate known karst features. High and low electrical-resistivity anomalies were correlated to air- and water-filled karst voids, respectively. Seismic velocity anomalies, including parabolic time suppressions, amplitude terminations, and surface-wave backscatters, were also observed and correlated to these karst voids. These findings were applied to a third location along Berea Road in order to investigate undiscovered karst voids. Three seismic targets were selected based on backscatter anomaly locations and were aligned in a northwest trend following the general bedrock dip, joint orientations, and suspected conduit orientation. Overall, the seismic-reflection method provided the highest resolution and least ambiguous results; however, integration of multiple methods was determined to help decrease ambiguities in interpretation created by the inherent non-uniqueness found in the results of each method.
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Wissinger, Eugene Scott. "Seismic profiling constraints on the evolution of the Brooks Range, Arctic Alaska from an integrated reflection/refraction survey." Thesis, 1996. http://hdl.handle.net/1911/19112.

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An integrated vertical incidence to wide-angle seismic data set has been used to develop a consistent migrated seismic reflection image and seismic velocity model of the Brooks Range fold and thrust belt in north central Alaska. Common midpoint (CMP) reflection data image the principal structures comprising the Brooks Range: the Endicott Mountains allochthon (EMA), the crustal scale Doonerak duplex, the master detachment, a 1.0-1.5 sec thick zone of lower crustal reflectivity just above the crust-mantle boundary, and a complex crustal root. The master detachment separates the crust into units which have been uplifted and deformed in the fold and thrust belt from those which have not. Least squares inversion of both reflected and refracted travel time data produced a velocity model consistent with CMP images of the Brooks Range, Bouguer gravity data, and seismic velocities determined from petrophysical data. Maximum crustal thickness in the range is 49 km, in an asymmetric root located under the EMA. At the root, an offset in lower crustal reflectivity is observed along with two deep zones of reflections north of the root. These reflections are interpreted as a Moho offset of some 5 km, resulting from subduction of the Brooks Range lower crust northward beneath the North Slope. The seismic reflection data, velocity data, and surface geologic constraints are used to identify the boundaries of major structural assemblages in the Brooks Range and restore 3 interpretations of the range to their pre-Jurassic configurations. Minimum shortening estimates derived above the basal decollement for the 3 models approximate 500-600 km of Mesozoic-Recent shortening. The amount of sub-decollement shortening may be as little as that now observed, 50-65 km, or may be comparable to the 500-600 km observed for upper-intermediate crustal rocks. Proximity of the continental subduction zone to the crustal scale Doonerak duplex suggests that the development of the fold and thrust belt has been at least partially controlled by the lower crust/mantle subduction.
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Underwood, Deborah H. "Hydrostratigraphic characterization of a coastal aquifer system in northern Monterey County, California using high-resolution seismic and ground penetrating radar profiling." Diss., 1998. http://catalog.hathitrust.org/api/volumes/oclc/41383675.html.

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Books on the topic "Virtual reflection seismic profiling"

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Hardage, Bob Adrian. Vertical seismic profiling. 2nd ed. Oxford: Pergamon Press, 1991.

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Vertical seismic profiling: Principles. 3rd ed. Amsterdam: Pergamon, 2000.

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Peter, Kennett, ed. Vertical seismic profiling and its exploration potential. Dordrecht: D. Reidel, 1985.

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J, Miller John. Reprocessing of reflection seismic lines R111 and R102, Risha Gas Field, Hashemite Kingdom of Jordan. [Denver, CO]: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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Brocher, Thomas M. Wide-angle seismic recordings obtained during seismic reflection profiling by the S.P. Lee offshore the Loma Prieta epicenter. Menlo Park, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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Brocher, Thomas Mark. Wide-angle seismic recordings obtained during seismic reflection profiling by the S.P. Lee offshore the Loma Prieta epicenter. Menlo Park, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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Brocher, Thomas M. Wide-angle seismic recordings obtained during seismic reflection profiling by the S.P. Lee offshore the Loma Prieta epicenter. Menlo Park, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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Uenzelmann-Neben, Gabriele. Sedimentation und Tektonik im Gebiet des Agulhas Rückens und des Agulhas Plateaus ("SETARAP") =: Sedimentation and tectonics of Agulhas Ridge and Agulhas Plateau : report of the cruise with RV "Petr Kottsov", December 17, 1997 to January 28th, 1998. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1998.

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Sando, Steven Kent. Determination of sediment thickness and volume in Lake Byron, South Dakota, using continuous seismic-reflection methods, May 1992. Rapid City, S.D: U.S. Geological Survey, 1994.

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René, R. M. Reflection seismic profiling of the Wabash Valley fault system in the Illinois Basin. Washington: U.S. G.P.O., 1995.

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Book chapters on the topic "Virtual reflection seismic profiling"

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Brown, Larry D. "Aspects of COCORP deep seismic profiling." In Reflection Seismology: A Global Perspective, 209–22. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0209.

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Chowdhury, Kabir Roy. "Deep Seismic Reflection and Refraction Profiling." In Encyclopedia of Solid Earth Geophysics, 103–18. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_226.

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Roy Chowdhury, Kabir. "Deep Seismic Reflection and Refraction Profiling." In Encyclopedia of Solid Earth Geophysics, 1–18. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10475-7_226-1.

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Roy Chowdhury, Kabir. "Deep Seismic Reflection and Refraction Profiling." In Encyclopedia of Solid Earth Geophysics, 127–44. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_226.

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Warner, M. R. "Deep seismic reflection profiling the continental crust at sea." In Reflection Seismology: A Global Perspective, 281–86. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0281.

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Okaya, David A. "Seismic profiling of the lower crust: Dixie Valley, Nevada." In Reflection Seismology: The Continental Crust, 269–79. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd014p0269.

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Oliver, Jack, and Sidney Kaufman. "Complexities of the Deep Basement from Seismic Reflection Profiling." In Geophysical Monograph Series, 243–53. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm020p0243.

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Oliver, Jack. "A global perspective on seismic reflection profiling of the continental crust." In Reflection Seismology: A Global Perspective, 1–3. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0001.

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Bois, C., M. Cazes, B. Damotte, A. Galdéano, A. Hirn, A. Mascle, P. Matte, J. F. Raoult, and G. Torreilles. "Deep seismic profiling of the crust in northern France: The ECORS Project." In Reflection Seismology: A Global Perspective, 21–29. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013p0021.

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Heitzmann, Peter, Walter Frei, Peter Lehner, and Paul Valasek. "Crustal indentation in the Alps—An overview of reflection seismic profiling in Switzerland." In Continental Lithosphere: Deep Seismic Reflections, 161–76. Washington, D. C.: American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0161.

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Conference papers on the topic "Virtual reflection seismic profiling"

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Brown, L., and K. Attoh. "Deep Seismic Reflection Profiling in Africa." In 10th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609-pdb.146.5.3.

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Brown, L. D. "Frontiers of Deep Seismic Reflection Profiling." In 5th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.299.8.

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Fuller, Brian N., Jose M. Pujol, and Scott B. Smithson. "Seismic reflection profiling in the Columbia Plateau." In SEG Technical Program Expanded Abstracts 1988. Society of Exploration Geophysicists, 1988. http://dx.doi.org/10.1190/1.1892195.

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S. Haines, Seth, and Karl J. Ellefsen. "AQUIFER CHARACTERIZATION WITH SEISMIC SHEAR WAVE REFLECTION PROFILING." In 19th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609-pdb.181.98.

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Kaida, Y., M. Matsubara, R. Ghose, and T. Kanemori. "Very Shallow Seismic Reflection Profiling Using Portable Vibrator." In 8th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609-pdb.206.1995_060.

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Milkereit, Bernd, and Erick Adam. "Reflection seismic profiling across the Matagami mining camp." In SEG Technical Program Expanded Abstracts 1992. Society of Exploration Geophysicists, 1992. http://dx.doi.org/10.1190/1.1822065.

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Haines, Seth S., and Karl J. Ellefsen. "Aquifer Characterization with Seismic Shear Wave Reflection Profiling." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2006. Environment and Engineering Geophysical Society, 2006. http://dx.doi.org/10.4133/1.2923735.

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Kaida, Y., M. Matsubara, R. Ghose, and T. Kanemori. "Very Shallow Seismic Reflection Profiling Using Portable Vibrator." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 1995. Environment and Engineering Geophysical Society, 1995. http://dx.doi.org/10.4133/1.2922182.

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S. Baker, Gregory, Jeffrey C. Strasser, Edward B. Evenson, Daniel E. Lawson, Kendra Pyke, and Robert A. Bigl. "Near-Surface Seismic Reflection Profiling On An Active Glacier." In 15th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2002. http://dx.doi.org/10.3997/2214-4609-pdb.191.11eg5.

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Baker, Gregory S., Jeffrey C. Strasser, Edward B. Evenson, Daniel E. Lawson, Kendra Pyke, and Robert A. Bigl. "Near‐Surface Seismic Reflection Profiling on an Active Glacier." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2002. Environment and Engineering Geophysical Society, 2002. http://dx.doi.org/10.4133/1.2927083.

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Reports on the topic "Virtual reflection seismic profiling"

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Spencer, C. P., A. G. Green, R. M. Clowes, F. A. Cook, and P. Carroll. Lithoprobe Seismic Reflection Profiling, southern Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131230.

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Milkereit, B., L. Reed, and A. Cinq-mars. High Frequency Reflection Seismic Profiling At Les Mines Selbaie, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133576.

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Harris, J. B., R. A. Hillman, J. A. Hunter, and J. L. Luternauer. Seismic reflection profiling in support of a deep borehole, Fraser River delta, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209075.

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Daley, T. M., E. L. Majer, and E. Karageorgi. Combined analysis of surface reflection imaging and vertical seismic profiling at Yucca Mountain, Nevada. Office of Scientific and Technical Information (OSTI), August 1994. http://dx.doi.org/10.2172/60915.

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Overton, A., and A. F. Embry. Seismic Reflection Profiling From An Ice Island Along the Continental Shelf of the Canadian Arctic Archipelago. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127612.

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Continuous seismic reflection profiling of hydrogeologic features beneath New River, Camp Lejeune, North Carolina. US Geological Survey, 1990. http://dx.doi.org/10.3133/wri894195.

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