Relevant bibliographies by topics / Radar geology

Contents

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

Academic literature on the topic 'Radar geology'

Author: Grafiati
Published: 4 June 2021
Last updated: 9 February 2022

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Journal articles on the topic "Radar geology"

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Budiono, Kris, and Godwin Latuputty. "SUBSURFACE GEOLOGICAL CONDITION OF SEVERAL LAND COASTAL ZONE IN INDONESIA BASED ON THE GSSI GROUND PROBING RADAR (GPR) RECORD INTERPRETATION." BULLETIN OF THE MARINE GEOLOGY 23, no. 1 (February 15, 2016): 9. http://dx.doi.org/10.32693/bomg.23.1.2008.6.

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The GSSI Ground Penetrating radar have been used to profile the shallow depth of subsurface geology of several area of Land Coastal zone in Indonesia Analysis of a large data base of GPR profile from natural subsurface geological condition along the land coast line have allowed identification of reflection configuration that characterize this type of sub surface geological environment. In many contamination problem, the geological information of coastal area is sparse and drill-core description only gives a limited picture of the geometry of inhomogeneties. The Ground-Probing Radar (GPR) method is a promising tool for resolving changes of physical properties in subsurface geological condition at the scale of natural inhomogeneties arising from changing lithology composition. The objective of present work are to examine whether and to what extent the characteristic lithofacies of subsurface lithology can be recognised as mapable reflection pattern on ground probing radar (GPR) reflection profiles in order to gain information about the subsurface geometry of subsurface geology in coastal area. Key word: Subsurface geology, coastal zone, Ground Probing Radar Ground probing radar produksi GSSI telah dipergunakan untuk membuat penampang geologi bawah permukaan dangkal di beberapa kawasan pantai Indonesia. Analisa data dasar penampang GPR dari geologi bawah permukaan di kawasan pantai dapat memperlihatkan konfigurasi reflector yang mencerminkan jenis lingkungan geologi bawah permukaan. Dalam masalah kontaminasi, informasi geologi di daerah pantai yang dihasilkan dari pemboran inti hanya dapat memperlihatkan gambaran yang sederhana tentang geometri ketidakseragaman. Metoda ground probing radar merupakan alat bantu yang menjanjikan untuk menanggulangi masalah sifat fisik kondisi geologi bawah permukaan pada skala ketidak seragaman yang sebenarnya dari perubahan komposisi litologi. Tujuan utama dari penelitian ini adalah untuk menguji sampai sejauh mana karakteristik litofasies dari litologi bawah permukaan dapat dilihat sebagai pola refleksi yang dapat dipetakan dalam penampang GPR dengan maksud untuk mendapatkan informasi geometri geologi bawah permukaan di daerah pantai. Kata kunci: Geologi bawah permukaan, zona pantai, “Ground probing radar”
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Budiono, Kris, and Yogi Noviadi. "INVESTIGATION OF GROUND PENETRATING RADAR FOR DETECTION OF ROAD SUBSIDENCE NORTHCOAST OF JAKARTA, INDONESIA." BULLETIN OF THE MARINE GEOLOGY 27, no. 2 (February 15, 2016): 87. http://dx.doi.org/10.32693/bomg.27.2.2012.48.

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A survey of Ground Penetrating Radar (GPR) was conducted in the coastal zone of northern part of Jakarta, Indonesia. The purpose of this survey was to provide the subsurface of coastal Quaternary sedimentary features and stratigraphy disturbances associated with induce post road subsidence 2009. The possibility of subsurface lithology disturbance shown by the GPR record. This record resulted from GPR methods using SIR system 20 GSSI, 270 MHz and 400 MHz and MLF 3200 transducer. The method is a promising tool for resolving changes of physical properties in subsurface lithology condition at the natural scale due to composition changes of physical properties.The reflection data resulted that GPR can distinguish between image the basic geometry forms such as lithology , structure geology , soil and subsurface utilities condition Keywords: Quaternary geology, Jakarta subsidence northern road 2009, Ground Penetrating Radar Penyelidikan “Ground Penerating Radar” (GPR) telah dilaksanakan di kawasan pantai utara Jakarta Utara, Indonesia. Tujuan dari penyelidikan GPR ini adalah untuk melihat kondisi sedimen Kuarter bawah permukaan dan gangguan stratigrafi sehubungan dengan penurunan jalan raya pada tahun 2009. Kemungkinan gangguan terhadap litologi bawah permukaan terlihat pada rekaman GPR. Hasil rekaman metoda GPR mempergunakan model SIR 20 GSSI, transduser 270MHz, 400 MHz dan MLF 3200.Metoda GPR merupakan alat bantu yang cukup menjanjikan untuk melihat perubahan sifat fisik litologi bawah permukaan pada skala sebenarnya yang disebabkan oleh perubahan komposisi sifat fisiknya. Hasil refleksi data GPR dapat membedakan bentuk dasar geometri seperti litologi, struktur geologi, kondisi utilitas bawah permukaan. Kata kunci : Geologi Kuarter, Penurunan jalan utara Jakarta 2009, Ground Penetrating Radar
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Singhroy, Vernon H. "Radar geology: Techniques and results." Episodes 15, no. 1 (March 1, 1992): 15–20. http://dx.doi.org/10.18814/epiiugs/1992/v15i1/004.

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Singhroy, V., R. Slaney, P. Lowman, J. Harris, and W. Moon. "RADARSAT and Radar Geology in Canada." Canadian Journal of Remote Sensing 19, no. 4 (November 1993): 338–51. http://dx.doi.org/10.1080/07038992.1993.10874569.

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Ernst, Jacques R., Alan G. Green, Hansruedi Maurer, and Klaus Holliger. "Application of a new 2D time-domain full-waveform inversion scheme to crosshole radar data." GEOPHYSICS 72, no. 5 (September 2007): J53—J64. http://dx.doi.org/10.1190/1.2761848.

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Crosshole radar tomography is a useful tool in diverse investigations in geology, hydrogeology, and engineering. Conventional tomograms provided by standard ray-based techniques have limited resolution, primarily because only a fraction of the information contained in the radar data (i.e., the first-arrival times and maximum first-cycle amplitudes) is included in the inversion. To increase the resolution of radar tomograms, we have developed a versatile full-waveform inversion scheme that is based on a finite-difference time-domain solution of Maxwell’s equations. This scheme largely accounts for the 3D nature of radar-wave propagation and includes an efficient method for extracting the source wavelet from the radar data. After demonstrating the potential of the new scheme on two realistic synthetic data sets, we apply it to two crosshole field data sets acquired in very different geologic/hydrogeologic environments. These are the first applications of full-waveform tomography to observed crosshole radar data. The resolution of all full-waveform tomograms is shown to be markedly superior to that of the associated ray tomograms. Small subsurface features a fraction of the dominant radar wavelength and boundaries between distinct geological/hydrological units are sharply imaged in the full-waveform tomograms.
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Zhu, Chun Jie, Fei Liu, and Jun Dong. "Structure Detection and Evaluation of the Highway Tunnel." Advanced Materials Research 1020 (October 2014): 405–10. http://dx.doi.org/10.4028/www.scientific.net/amr.1020.405.

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Combined with a highway tunnel testing and assessment, through the discussing of technical problems existed in tunnel’s quality detecting by the using of geology radar, using gist of geology radar in tunnel’s quality detecting is grasped, the key technologies of survey line layout, acquisition parameters setting and on-site test in the process of geological radar application are concluded. Relying on the field test data, lining thickness and dense degree of the left and right of spandrel and arch crown being in the safe use of phase are more deeply researched. The studies show that geological radar detection technology for tunnel nondestructive testing and evaluation is a kind of effective method, correlation detection technique and analysis method has some reference value to the similar tunnel structure.
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Xiao, Qiao Lin, and Fen Lü. "Application Research of Geological Radar in Volcanic Lava in the Geological Survey." Applied Mechanics and Materials 226-228 (November 2012): 2093–97. http://dx.doi.org/10.4028/www.scientific.net/amm.226-228.2093.

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Aiming at the Hainan volcanic lava the geological characteristics, the application of geological radar detection technology in the geological environment of signal respond, combined with the added drilling data is compared, established the goal of geological radar image characteristics of geology, summarized the poor geological conditions in the area of geological radar signal response law. Field test shows that the radar reflected wave group of wave characteristic in volcanic lava can distinguish different geological layer reflection wave group, and via studying their relationship and change trend, to achieve the purpose of geological interpretation, and determine the adverse lava geology development stages , for design and construction to provide the reliable foundation material, effective use of survey for the design and construction of the guidance function.
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Krajewski, Witold F., Anton Kruger, Satpreet Singh, Bong-Chul Seo, and James A. Smith. "Hydro-NEXRAD-2: real-time access to customized radar-rainfall for hydrologic applications." Journal of Hydroinformatics 15, no. 2 (December 6, 2012): 580–90. http://dx.doi.org/10.2166/hydro.2012.227.

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Hydro-NEXRAD-2 (HNX2) is a prototype system that allows hydrologic users real-time access to NEXRAD radar data in support of a wide range of research. The system processes basic radar data (Level II) and delivers radar-rainfall products based on the user's custom selection of features such as spatial domain, rainfall product space and time resolution, and rainfall estimation algorithms. HNX2 collects real-time, unprocessed data from multiple NEXRAD radars as they become available, processes them through a user-configurable pipeline of data-processing modules, and publishes the processed data-products at regular intervals. Modules in the data-processing pipeline encapsulate algorithms such as non-meteorological echo detection, radar range correction, radar-reflectivity-rain rate (Z-R) conversion, echo advection correction, mosaicking of products from multiple radars, and grid projections and transformations. This paper describes the challenges involved in HNX2's development and implementation, which include real-time error-handling, time-synchronization of data from multiple asynchronous sources, generation of multiple-radar metadata products, and distribution of products to a user base with diverse needs and constraints. HNX2 publishes products through automation and allows multiple users access to published products. Currently, HNX2 is serving near real-time rain-rate maps for Iowa in the USA using data from seven radars covering the state. Hydrologic models operated by The University of Iowa's Iowa Flood Center use these products.
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Vivekanandan, J., W. C. Lee, E. Loew, J. L. Salazar, V. Grubišić, J. Moore, and P. Tsai. "The next generation airborne polarimetric Doppler weather radar." Geoscientific Instrumentation, Methods and Data Systems 3, no. 2 (July 21, 2014): 111–26. http://dx.doi.org/10.5194/gi-3-111-2014.

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Abstract. Results from airborne field deployments emphasized the need to obtain concurrently high temporal and spatial resolution measurements of 3-D winds and microphysics. A phased array radar on an airborne platform using dual-polarization antenna has the potential for retrieving high-resolution, collocated 3-D winds and microphysical measurements. Recently, ground-based phased array radar (PAR) has demonstrated the high time-resolution estimation of accurate Doppler velocity and reflectivity of precipitation and clouds when compared to mechanically scanning radar. PAR uses the electronic scanning (e-scan) to rapidly collect radar measurements. Since an airborne radar has a limited amount of time to collect measurements over a specified sample volume, the e-scan will significantly enhance temporal and spatial resolution of airborne radar observations. At present, airborne weather radars use mechanical scans, and they are not designed for collecting dual-polarization measurements to remotely estimate microphysics. This paper presents a possible configuration of a novel airborne phased array radar (APAR) to be installed on an aircraft for retrieving improved dynamical and microphysical scientific products. The proposed APAR would replace the aging, X-band Electra Doppler radar (ELDORA). The ELDORA X-band radar's penetration into precipitation is limited by attenuation. Since attenuation at C-band is lower than at X-band, the design specification of a C-band airborne phased array radar (APAR) and its measurement accuracies are presented. Preliminary design specifications suggest the proposed APAR will meet or exceed ELDORA's current sensitivity, spatial resolution and Doppler measurement accuracies of ELDORA and it will also acquire dual-polarization measurements.
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Witten, Alan, and John Lane. "Offset vertical radar profiling." Leading Edge 22, no. 11 (November 2003): 1070–76. http://dx.doi.org/10.1190/1.1634910.

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Dissertations / Theses on the topic "Radar geology"

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Cross, Guy Matthew. "Radar imaging glacio-volcanic stratigraphy : Mt. Wrangell, Alaska." Thesis, University of British Columbia, 1987. http://hdl.handle.net/2429/26195.

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An airborne radar survey was conducted over the ice-filled volcanic caldera at Mt. Wrangell, Alaska. Research reported here involves computer processing and interpretation of radio-reflection data acquired over 21 traverses of the summit. In addition to describing useful data enhancement techniques, a dynamic programming approach is introduced for topographically controlled data positioning and spatial correction. Interpretation focusses upon a well defined radio-stratigraphy attributed to high acidity horizons deposited at the ice surface during periods of elevated volcanic activity. A comparative analysis of layer character indicates that echoes from the caldera floor are not continuously detected because of anomalously high signal absorption. Consequently, results impose a lower limit upon maximum ice thickness. A numerical interpretation scheme, incorporating both glaciological measurements and empirical relations governing the behaviour of firn and ice, is developed to aid interpretation of the glacio-volcanic stratigraphy. Preliminary modelling yields a speculative volcanic record that roughly matches the known eruption sequence at Mt. Wrangell and suggests a significant extension of the volcanic history.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
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Woods, Brian Keith. "Development of an active pulsed radar receiver for a mono-static borehole-radar tool." Thesis, Stellenbosch : University of Stellenbosch, 2003. http://hdl.handle.net/10019.1/2512.

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Via, Michelle Frances. "Atmospheric Effects on Radar/Ladar Detection of Seismic Activity." Wright State University / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=wright1440979742.

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Dena, Ornelas Oscar S. "Fast approximate migration of ground penetrating radar using Kalman estimators and determination of the lithospheric structure of Lake Baikal, Russia." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2008. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Van, Gestel Jean-Paul. "Structure and tectonics of the Puerto Rico-Virgin Islands platform and multi-confirguration ground penetrating radar data /." Digital version accessible at:, 2000. http://wwwlib.umi.com/cr/utexas/main.

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Voytenko, Denis. "Glaciological Applications of Terrestrial Radar Interferometry." Scholar Commons, 2015. http://scholarcommons.usf.edu/etd/5856.

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Terrestrial Radar Interferometry (TRI) is a relatively new ground-based technique that combines the precision and spatial resolution of satellite interferometry with the temporal resolution of GPS. Although TRI has been applied to a variety of fields including bridge and landslide monitoring, it is ideal for studies of the highly-dynamic terminal zones of marine-terminating glaciers, some of which are known to have variable velocities related to calving and/or ocean-forced melting. My TRI instrument is the Gamma Portable Radar Interferometer, which operates at 17.2 GHz (1.74 cm wavelength), has two receiving antennas for DEM (digital elevation model) generation, and images the scenes at minute-scale sampling rates. Most of this TRI work has focused on two glaciers: Breiðamerkurjökull in Iceland and Helheim in Greenland. Monitoring the displacement of stationary points suggests velocity measurement uncertainties related to the instrument and atmosphere of less than 0.05 m/d. I show that the rapid sampling rate of the TRI can be used to observe velocity variations at the glacier terminus and assess the impact and spatial distribution of tidal forcing. Additionally, iceberg tracking in the amplitude imagery may provide insight about ocean currents near the terminus.
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Manjunath, Deepak Gomez Francisco Gustavo. "Earthquake interaction along the Sultandagi-Aksehir fault based on InSar and coulomb stress modeling." Diss., Columbia, Mo. : University of Missouri-Columbia, 2008. http://hdl.handle.net/10355/5788.

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Thesis (M.S.)--University of Missouri-Columbia, 2008.
The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed on July 8, 2009) Includes bibliographical references.
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Jung, Hahn Chul. "Wetland Hydrodynamics Using Interferometric Synthetic Aperture Radar, Remote Sensing, and Modeling." The Ohio State University, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=osu1291661296.

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Northrup, Dustin Shawn. "A Geomorphological Study of Yardangs in China, the Altiplano/Puna of Argentina, and Iran as Analogs for Yardangs on Titan." BYU ScholarsArchive, 2018. https://scholarsarchive.byu.edu/etd/6781.

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Collections of straight, RADAR-bright, linear features, or BLFs, on Saturn's moon Titan are revealed in Cassini SAR (Synthetic Aperture RADAR) images. Most are widely distributed across the northern midlatitudes SAR on SAR swaths T18, T23, T30, T64, and T83 and in swath T56 in the southern midlatitudes. To understand the origin of these features, we compare them with terrestrial yardangs in Dunhuang, China, the Altiplano/Puna of Argentina, and the Lut Desert of Iran and with a similar morphological landform, linear dunes in the Namib Sand Sea, Namibia and on Titan. We apply a statistical classification model developed through random forests, a type of decision tree classification system, grown with terrestrial and titanian training data to the BLFs. To develop the classification, we measured sinuosity, width, spacing, and length for all of the BLFs and their possible terrestrial analogs. We interpret the features in T18, T64-1, and T83 as yardangs based upon morphological similarities between them and features in Iran and Argentina, such as overall SAR brightness, straightness, and lack of branching. Similarities exist between the BLFs and terrestrial yardangs in sinuosity and spacing—sinuosity values range from 1.00 to 1.04 for all the BLFs, and terrestrial yardangs in Iran range from 1.00 to 1.001. A generated statistical model classified a large number of yardangs in T18 and T64-1. In contrast, we interpret the BLFs in T23 and T30 as stabilized linear dunes due to similarities in sinuosity, spacing, and scale with linear dunes in the Namib Sand Sea and Titan swath T3. Stabilized linear dunes may be slightly brighter than the SAR-dark dunes due a change in dielectric constant from introduction of liquids and subsequent stabilization or from the formation of a crust over the top the feature. Sinuosities range from 1.00 to 1.37 in T23 and T30 whereas dunes in the Namib and in T3 range from 1.01 to 1.05. Branching behavior similar to dunes are also observed in BLFs in swaths T23 and T30. The BLF features in T56 in the southern hemisphere we interpret to be dune-related, likely SAR-bright (rough) inter-dune areas. We base this interpretation on the presence of SAR-dark lineations between the BLFs that may be linear dunes. The statistical model classifies few yardangs in T23, T30, and T56. We conclude that statistical classification of these features can be performed. We also show that yardang orientations may aid in the development of global climate and wind models as both current and paleo wind direction indicators.
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Neumann, William John III. "The use of ground penetrating radar to determine the presence, extent, and spatial variability of fire related hydrophobic soils in fire impacted watersheds in southern California." Diss., University of Iowa, 2016. https://ir.uiowa.edu/etd/2251.

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Ground Penetrating Radar (GPR) methods have been used to evaluate the presence, extent, and spatial variability of hydrophobic soils in Southern California Watersheds. It has been shown that high frequency ground penetrating radar equipment, under certain conditions, has the ability to determine the presence, depth, and persistence of post fire hydrophobic soils. As part of this study an extensive investigation was undertaken to not only evaluate the capability of this approach but also to understand under what conditions the method can be applied successfully and what are the limitations of the approach. The investigation includes use of computer simulations and modeling, laboratory investigations in sand boxes with native soils, and multiple field trials spanning a five year time period. Of particular significance is the finding that using GPR it is possible to: locate the interface between the uppermost burnt soil layer, and soil horizons below; quantify the depth at which the hydrophobic layer forms; and quantify the spatial extent of the layer. As part of this study best practice methods for both field and lab experimentation have also been developed and are presented in the body of the thesis. Based on this study it is concluded that the use of GPR can provide a much more accurate and comprehensive method of evaluating the nature of hydrophobic layers in such environments than the current point specific manual methods. As a result the use of GPR has significantly advanced our capacity to assess the potential for increased erosion and the generation of debris flows in such environments after rainfall events.
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Books on the topic "Radar geology"

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Fletcher, Karen. Spaceborne radar applications in geology: An introduction to imaging radar, and application examples of ERS SAR in geology and geomorphology. Edited by European Space Agency and European Space Research and Technology Centre. Noordwijk, The Netherlands: ESA Publications Division, ESTEC, 2005.

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Lawrence, G. M. Imaging radar for geology: A study of SIR-B and related data. Borehamwood: Hunting Geology and Geophysics, 1985.

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Finkelʹshteĭn, M. I. Primenenie radiolokat͡s︡ionnogo podpoverkhnostnogo zondirovanii͡a︡ v inzhenernoĭ geologii. Moskva: "Nedra", 1986.

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Ceng zhuang ti xi jie dian te xing fan yan li lun ji qi ying yong. Beijing: Ke xue chu ban she, 2011.

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Lamparski, Piotr. Formy i osady czwartorzędowe w świetle badań georadarowych. Warsawa: PAN IG i PZ, 2004.

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Venus Geoscience Tutorial and Venus Geologic Mapping Workshop (1989 Flagstaff, Ariz.). Abstracts for the Venus Geoscience Tutorial and Venus Geologic Mapping Workshop: Flagstaff, Arizona, June 12-15, 1989. [Houston, Tex: Lunar and Planetary Institute, 1989.

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Friedman, Jules D. Tectonic trends of the northern part of the Paradox Basin, southeastern Utah and southwestern Colorado, as derived from LANDSAT multispectral scanner imaging and geophysical and geologic mapping. Washington: U.S. G.P.O., 1994.

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Sutinen, Raimo. Glacial deposits, their electrical properties and surveying by image interpretation and ground penetrating radar. Espoo: Geologian tutkimuskeskus, 1992.

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Inc, Horler Information. Evaluation of Radarsat applications in geology and state of preparedness of Canadian users: Final report. Ottawa, Ont: Horler Information, 1992.

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Friedman, Jules D. Uncontrolled X-band radar mosaic of the western part of the Moab 1 ̕x 2 ̕quadrangle, southeastern Utah and southwestern Colorado. Washington: U.S. G.P.O., 1994.

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Book chapters on the topic "Radar geology"

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Blindow, Norbert, Dieter Eisenburger, Bernhard Illich, Hellfried Petzold, and Thomas Richter. "Ground Penetrating Radar." In Environmental Geology, 283–335. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-74671-3_10.

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Drury, S. A. "Radar remote sensing." In Image Interpretation in Geology, 165–94. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-010-9393-4_7.

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Duranthon, J. P., F. Lemaître, and M. A. Chanut. "Radar Evaluation Movements Structures and Field." In Engineering Geology for Society and Territory - Volume 2, 1403–7. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_248.

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Strozzi, Tazio, Hugo Raetzo, Urs Wegmüller, Jessica Papke, Rafael Caduff, Charles Werner, and Andreas Wiesmann. "Satellite and Terrestrial Radar Interferometry for the Measurement of Slope Deformation." In Engineering Geology for Society and Territory - Volume 5, 161–65. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_32.

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Tarpanelli, A., L. Brocca, S. Barbetta, T. Lacava, M. Faruolo, and T. Moramarco. "Integration of MODIS and Radar Altimetry Data for River Discharge Estimation from Space." In Engineering Geology for Society and Territory - Volume 3, 607–10. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09054-2_121.

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Antolini, Francesco, and Marco Barla. "Combining Finite-Discrete Numerical Modelling and Radar Interferometry for Rock Landslide Early Warning Systems." In Engineering Geology for Society and Territory - Volume 6, 705–8. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09060-3_126.

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Eriksen, H. Ø., T. R. Lauknes, Y. Larsen, J. F. Dehls, T. Grydeland, and H. Bunkholt. "Satellite and Ground-Based Interferometric Radar Observations of an Active Rockslide in Northern Norway." In Engineering Geology for Society and Territory - Volume 5, 167–70. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_33.

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Grégoire, Colette, John W. Lane, and Peter K. Joesten. "Application of Borehole Radar for Monitoring Steam-Enhanced Remediation of a Contaminated Site in Fractured Limestone, Maine, USA." In Engineering Geology for Infrastructure Planning in Europe, 385–92. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-39918-6_45.

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Corominas, Jordi, Rubén Iglesias, Albert Aguasca, Jordi J. Mallorquí, Xavier Fàbregas, Xavier Planas, and Josep A. Gili. "Comparing Satellite Based and Ground Based Radar Interferometry and Field Observations at the Canillo Landslide (Pyrenees)." In Engineering Geology for Society and Territory - Volume 2, 333–37. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_51.

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Raynaud, Felix, Valerie Borrell-Estupina, Alain Dezetter, Severin Pistre, Helene Mathieu-Subias, and Eric Servat. "Modelling Flash Floods in a Karstic Watershed Using an Original Semi-distributed Radar-Gauge Merging Method." In Engineering Geology for Society and Territory - Volume 3, 169–73. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09054-2_34.

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Conference papers on the topic "Radar geology"

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Fenning, P. J. "Radar, physics and geology." In IEE Colloquium on Radar and Microwave Techniques for Non-Destructive Evaluation. IEE, 1995. http://dx.doi.org/10.1049/ic:19951315.

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Huilian, Wang, Li Daxin, Qi Mingsong, and Deng Shikun. "Application of ground penetrating radar to engineering geology in China." In Fourth International Conference on Ground Penetrating Radar. European Association of Geoscientists & Engineers, 1992. http://dx.doi.org/10.3997/2214-4609-pdb.303.11.

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Funk, C. W., and M. van den Berghe. "Mapping Complex Geology with GPR in a Canadian Potash Mine." In 2018 17th International Conference on Ground Penetrating Radar (GPR). IEEE, 2018. http://dx.doi.org/10.1109/icgpr.2018.8441589.

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Maurya, D. M., Mamta Tiwari, A. S. Rajawat, H. Kumar, N. Khonde, and L. S. Chamyal. "Geomorphic Characterization of the Banni Plain, Kachchh, Using Orbital Imaging Radar (RISAT 1C) and Optical Remote Sensing Data." In Recent Studies on the Geology of Kachchh. Geological Society of India, 2016. http://dx.doi.org/10.17491/cgsi/2016/105419.

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Santos-Assuncao, Sonia, Vega Perez-Gracia, and Ramon Gonzalez-Drigo. "GPR backscattering applied to urban shallow geology: GPR application in seismic microzonation." In 2015 8th International Workshop on Advanced Ground Penetrating Radar (IWAGPR). IEEE, 2015. http://dx.doi.org/10.1109/iwagpr.2015.7292659.

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Nesbitt, Ian, Seth Campbell, Steven Arcone, and Sean M. Smith. "NEW ENGLAND LAKE BOTTOM GEOLOGY AND SEDIMENTATION RATES DERIVED FROM GROUND-PENETRATING RADAR." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306235.

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Gafarov, K., M. Ercoli, D. Cirillo, C. Pauselli, and F. Brozzetti. "Extending surface geology data through GPR prospections: Quaternary faulting signature from the Campotenese area (Calabria-Italy)." In 2018 17th International Conference on Ground Penetrating Radar (GPR). IEEE, 2018. http://dx.doi.org/10.1109/icgpr.2018.8441611.

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Barone, P. M., T. Bellomo, E. Pettinelli, and C. Scarpati. "Applications of GPR to archaeology and geology: the example of the regio III in Pompeii (Naples, Italy)." In 2007 4th International Workshop on, Advanced Ground Penetrating Radar. IEEE, 2007. http://dx.doi.org/10.1109/agpr.2007.386526.

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Kosaroglu, Sinan. "GROUND PENETRATING RADAR (GPR) METHOD OF GEOLOGICAL PROPERTIES OF COAL SEAMS NEAR THE SURFACE." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b11/s5.062.

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Tanajewski, Dariusz. "GROUND PENETRATING RADAR DATA ACQUISITION AND ANALYSES AT THE MOST HOLY TRINITY CHURCH IN STEBARK, POLAND." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b11/s5.063.

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Reports on the topic "Radar geology"

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Card, K., P. Huppé, C. Bowie, and J. Harris. Bedrock geology/airborne radar, Sudbury. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194046.

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Card, K. D., B. V. Sanford, and A. Davidson. Airborne Synthetic Aperture Radar (SAR)/geology, Sudbury, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/193704.

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Dallimore, S. R., and J. L. Davis. Ground Probing Radar Investigations of Massive Ground Ice and near Surface Geology in Continuous Permafrost. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122561.

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Jackson, L. E., S. R. Morison, and K. McKenna. Surficial Geology, Rader Lake, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/194041.

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Simms, Janet, Benjamin Breland, and William Doll. Geophysical investigation to assess condition of grouted scour hole : Old River Control Complex—Low Sill Concordia Parish, Louisiana. Engineer Research and Development Center (U.S.), September 2021. http://dx.doi.org/10.21079/11681/41863.

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Abstract:
Geophysical surveys, both land-based and water-borne, were conducted at the Old River Control Complex‒Low Sill, Concordia Parish, LA. The purpose of the surveys was to assess the condition of the grout within the scour region resulting from the 1973 flood event, including identification of potential voids within the grout. Information from the ground studies will also be used for calibration of subsequent marine geophysical data and used in stability analysis studies. The water-borne survey consisted of towed low frequency (16-80 MHz) ground penetrating radar (GPR), whereas the land-based surveys used electrical resistivity and seismic refraction. The GPR survey was conducted in the Old River Channel on the upstream side of the Low Sill structure. The high electrical conductivity of the water (~50 mS/m) precluded penetration of the GPR signal; thus, no useful data were obtained. The land-based surveys were performed on both northeast and southeast sides of the Low Sill structure. Both resistivity and seismic surveys identify a layered subsurface stratigraphy that corresponds, in general, with available borehole data and constructed geologic profiles. In addition, an anomalous area on the southeast side was identified that warrants future investigation and monitoring.
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Geology, Mining and Reclamation at the Radar Hill Quarry, Citrus County, Florida. Florida Geological Survey, 1989. http://dx.doi.org/10.35256/ic105p2.

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Relations between Warm Springs and geology delineated by side-looking airborne-radar imagery in eastern West Virginia. US Geological Survey, 1991. http://dx.doi.org/10.3133/wri884096.

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Map showing surficial and generalized bedrock geology and accompanying side-looking airborne radar image of the Radford 30' x 60' Quadrangle, Virginia and West Virginia. US Geological Survey, 1991. http://dx.doi.org/10.3133/i2170a.

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Tectonic trends of the northern part of the Paradox Basin, southeastern Utah and southwestern Colorado, as derived from Landsat multispectral scanner imaging and geophysical and geologic mapping: Uncontrolled X-band radar mosaic of the western part of the Moab 1 degree x 2 degrees Quadrangle, southeastern Utah and southwestern Colorado. US Geological Survey, 1994. http://dx.doi.org/10.3133/b2000cd.

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