Relevant bibliographies by topics / Geological mapping

Contents

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

Academic literature on the topic 'Geological mapping'

Author: Grafiati
Published: 4 June 2021
Last updated: 11 June 2025

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Journal articles on the topic "Geological mapping"

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Griffiths, J. S. "Engineering geological mapping." Geological Society, London, Engineering Geology Special Publications 18, no. 1 (2001): 39–42. http://dx.doi.org/10.1144/gsl.eng.2001.018.01.06.

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Williams, D. A. "NASA’S PLANETARY GEOLOGIC MAPPING PROGRAM: OVERVIEW." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B4 (June 14, 2016): 519–20. http://dx.doi.org/10.5194/isprs-archives-xli-b4-519-2016.

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NASA’s Planetary Science Division supports the geologic mapping of planetary surfaces through a distinct organizational structure and a series of research and analysis (R&A) funding programs. Cartography and geologic mapping issues for NASA’s planetary science programs are overseen by the Mapping and Planetary Spatial Infrastructure Team (MAPSIT), which is an assessment group for cartography similar to the Mars Exploration Program Assessment Group (MEPAG) for Mars exploration. MAPSIT’s Steering Committee includes specialists in geological mapping, who make up the Geologic Mapping Subcommittee (GEMS). I am the GEMS Chair, and with a group of 3-4 community mappers we advise the U.S. Geological Survey Planetary Geologic Mapping Coordinator (Dr. James Skinner) and develop policy and procedures to aid the planetary geologic mapping community. GEMS meets twice a year, at the Annual Lunar and Planetary Science Conference in March, and at the Annual Planetary Mappers’ Meeting in June (attendance is required by all NASA-funded geologic mappers). Funding programs under NASA’s current R&A structure to propose geological mapping projects include Mars Data Analysis (Mars), Lunar Data Analysis (Moon), Discovery Data Analysis (Mercury, Vesta, Ceres), Cassini Data Analysis (Saturn moons), Solar System Workings (Venus or Jupiter moons), and the Planetary Data Archiving, Restoration, and Tools (PDART) program. Current NASA policy requires all funded geologic mapping projects to be done digitally using Geographic Information Systems (GIS) software. In this presentation we will discuss details on how geologic mapping is done consistent with current NASA policy and USGS guidelines.
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Dandar, Otgonbayar, Atsushi Okamoto, Masaoki Uno, Undarmaa Batsaikhan, Burenjargal Ulziiburen, and Noriyoshi Tsuchiya. "Drone brings new advance of geological mapping in Mongolia: Opportunities and challenges." Mongolian Geoscientist, no. 47 (December 31, 2018): 53–57. http://dx.doi.org/10.5564/mgs.v0i47.1063.

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Unmanned aerial vehicles (UAVs) or drones have revolutionized scientific research in multiple fields. Drones provide us multiple advantages over conventional geological mapping or high-altitude remote sensing methods, in which they allow us to acquire data more rapidly of inaccessible or risky outcrops, and can connect the spatial scale gap in mapping between manual field techniques and airborne, high-altitude remote sensing methods. Despite the decreased cost and technological developments of platforms, sensors and software, the use of drones for geological mapping in Mongolia has not yet been utilized. In this study, we present using of drone in two areas: the Chandman area in which eclogite is exposed and the Naran massif of the Khantaishir ophiolite in the Altai area. Drone yields images with high resolution that is reliable to use and reveals that it is possible to make better formulation of geological mapping. Our suggestion is that (1) Mongolian geoscientists are encouraged to add drones to their geologic toolboxes and (2) drone could open new advance of geological mapping in Mongolia in which geological map will be created in more effective and more detailed way combined with conventional geological survey on ground.
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Lemenkova, Polina. "Seismicity in the Afar Depression and Great Rift Valley, Ethiopia." Environmental Research, Engineering and Management 78, no. 1 (2022): 83–96. http://dx.doi.org/10.5755/j01.erem.78.1.29963.

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Integrated mapping is essential in geological studies to assess risks of earthquake hazards. Cartographic techniques have become a commonplace approach to visualizing data in the continuous geologic and geophysical fields. However, traditional GIS mapping is a manual process with a time-consuming workflow that can lead to mistakes and misinterpretation of data. This study applied two mapping approaches to address this problem: Generic Mapping Tools (GMT) used for automated cartographic workflow employing scripts and QGIS used for traditional geologic mapping. The study area includes Ethiopia, notable for its complex geologic setting. The study aimed to analyse the relationships between the geophysical, geological, topographic and seismic setting of the country by presenting six new thematic maps:1 topography based on the GEBCO/SRTM15+ high-resolution grid;2 geological units with consistent lithology and age from the USGS database;3 geological provinces with major Amhara Plateau and Somali Province using USGS data;4 geoid based on the Earth Gravitational Model 2008 (EGM-2008) grid;5 free-air gravity anomaly model using satellite-based remote sensing data;6 seismicity showing earthquakes and volcanos from 05/03/1990 to 27/11/2020.The comparison of the topography, seismicity, geophysics and surface geology of the Afar Depression and the Great Rift Valley was based partly on extant literature on the geologic setting of Ethiopia which primarily focuses upon discussing tectonic processes that took place in the East African Rift System in the past. The current study contributes to the previous research and increases cartographic data on the geology and geophysics of Ethiopia. The outcomes can be implemented in similar regional projects in Ethiopia for geophysical and geological monitoring.
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Dawes, P. R. "Geological mapping of Greenland." Rapport Grønlands Geologiske Undersøgelse 148 (January 1, 1990): 10–15. http://dx.doi.org/10.34194/rapggu.v148.8109.

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Geological maps provide an important means of documenting and advancing geological knowledge. As well as presenting detailed information in a practical way, geological maps are essential in assessing a region’s geological history; they are prerequisite for meaningful evaluation of mineral resources.
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Hillier, John. "Geological mapping in Australia." Cartography 16, sup1 (1987): 62–66. http://dx.doi.org/10.1080/00690805.1987.10438389.

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Kotsanis, D., P. Panagiotopoulos, D. Rozos, and C. Loupasakis. "Engineering geological mapping of the Pallini urban area." Bulletin of the Geological Society of Greece 47, no. 4 (2013): 1715. http://dx.doi.org/10.12681/bgsg.11036.

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Engineering geological thematic maps can provide substantial information for the development of cities, the land planning of future infrastructures and even more for the planning of the natural hazards prevention and/or mitigation. To this direction the engineering geological map of the Municipality of Pallini, at the Eastern Attica prefecture, at a scale of 1:20.000, was compiled. For that purpose, the following workflow was adopted: Firstly, a desk study helped in selecting the relevant topographic and geologic maps, which were digitized and introduced in a GIS environment. Secondly, the data coming from detailed geological mapping were elaborated to the same GIS environment. Thirdly, geotechnical data collected from borehole logs, such as lithostromatographic sequence, in situ tests and laboratory tests were introduced in geotechnical database. The statistical evaluation of this data provided estimates for numerous geotechnical parameters. Finally, the engineering geological map was compiled by merging the geological formations into lithologic units according to their origin, age, natural condition, and geotechnical characteristics.
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Lemenkova, Polina, and Olivier Debeir. "Seismotectonics of Shallow-Focus Earthquakes in Venezuela with Links to Gravity Anomalies and Geologic Heterogeneity Mapped by a GMT Scripting Language." Sustainability 14, no. 23 (2022): 15966. http://dx.doi.org/10.3390/su142315966.

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This paper presents a cartographic framework based on algorithms of GMT codes for mapping seismically active areas in Venezuela. The data included raster grids from GEBCO, EGM-2008, and vector geological layers from the USGS. The data were iteratively processed in the console of GMT, converted by GDAL, formatted, and mapped for geophysical data visualisation; the QGIS was applied for geological mapping. We analyzed 2000 samples of the earthquake events obtained from the IRIS seismic database with a 25-year time span (1997–2021) in order to map the seismicity. The approach to linking geological, topographic, and geophysical data using GMT scripts aimed to map correlations among the geophysical phenomena, tectonic processes, geological setting, seismicity, and earthquakes. The practical application of the GMT scripts consists in automated mapping for the visualization of geological risks and hazards in the mountainous region of the Venezuelan Andes. The proposed method integrates the approach of GMT scripts with state-of-the-art GIS techniques, which demonstrated its effectiveness as a tool for mapping spatial datasets and rapid data processing in an iterative regime. In this context, using GMT and GIS to find similarities between the regional earthquake distribution and the geological and topographic setting is essential for hazard risk assessment. This study can serve as a basis for predictive seismic analysis in geologically vulnerable regions of Venezuela. In addition to a technical demonstration of GMT algorithms, this study also contributes to geological and geophysical mapping and seismic hazard assessments in South America. We present the full scripts used for mapping in a GitHub repository.
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Sunuwar, S. C. "Geological mapping in the Nepal Himalaya: importance and challenges for underground structures." Journal of Nepal Geological Society 51 (December 31, 2016): 89–95. http://dx.doi.org/10.3126/jngs.v51i0.24096.

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Geological mapping is very important technique to predict geological condition for underground structures. It helps to construct geological model for site selection and designing of any underground structures. Geological uncertainty is directly proportional to the accuracy of geological mapping. More accurate geological mapping resulted fewer uncertainties. Precise delineation of faults, shear/weak zones and water bearing zones is important part of the geological mapping to predict uncertainties. Geological mapping to predict geological condition for underground structures is a challenge in the tectonically active Nepal Himalaya due to thrusting, faulting, folding and reverse metamorphism nature of rocks with difficult terrain and high overburden. The mapping for underground structures is mostly focus on rock mass properties, faults, weak/shear zones, fractured zone, joints, folds, weathering depth and ground water bearing zones. This paper highlights importance of geological mapping and challenges for underground structures with case studies of uncertainties faced due to poor geological mapping.
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Olsen, Paul E., Jacques Laskar, Dennis V. Kent, et al. "Mapping Solar System chaos with the Geological Orrery." Proceedings of the National Academy of Sciences 116, no. 22 (2019): 10664–73. http://dx.doi.org/10.1073/pnas.1813901116.

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The Geological Orrery is a network of geological records of orbitally paced climate designed to address the inherent limitations of solutions for planetary orbits beyond 60 million years ago due to the chaotic nature of Solar System motion. We use results from two scientific coring experiments in Early Mesozoic continental strata: the Newark Basin Coring Project and the Colorado Plateau Coring Project. We precisely and accurately resolve the secular fundamental frequencies of precession of perihelion of the inner planets and Jupiter for the Late Triassic and Early Jurassic epochs (223–199 million years ago) using the lacustrine record of orbital pacing tuned only to one frequency (1/405,000 years) as a geological interferometer. Excepting Jupiter’s, these frequencies differ significantly from present values as determined using three independent techniques yielding practically the same results. Estimates for the precession of perihelion of the inner planets are robust, reflecting a zircon U–Pb-based age model and internal checks based on the overdetermined origins of the geologically measured frequencies. Furthermore, although not indicative of a correct solution, one numerical solution closely matches the Geological Orrery, with a very low probability of being due to chance. To determine the secular fundamental frequencies of the precession of the nodes of the planets and the important secular resonances with the precession of perihelion, a contemporaneous high-latitude geological archive recording obliquity pacing of climate is needed. These results form a proof of concept of the Geological Orrery and lay out an empirical framework to map the chaotic evolution of the Solar System.
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Dissertations / Theses on the topic "Geological mapping"

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Akkok, Inci. "Geological Mapping Using Remote Sensing Technologies." Master's thesis, METU, 2009. http://etd.lib.metu.edu.tr/upload/3/12610626/index.pdf.

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In an area of interest- Sivas Basin, Turkey- where most of the units are sedimentary and show similar spectral characteristics, spectral settings of ASTER sensor may not be enough by itself. Therefore, considering other aspects, such as morphological variables, is reasonable in addition to spectral classifiers. The main objective of this study is to test usefulness of integration of spectral analysis and morphological information for geological mapping. Remotely sensed imagery obtained from ASTER sensor is used to classify different lithological units while DEM is used to characterize landforms related to these lithological units. Maximum Likelihood Classification (MLC) is used to integrate data streaming from different sources. The methodology involves integrating the surface properties of the classified geological units in addition to the spectral reflectances. Seven different classification trials were conducted: : 1. MLC using only nine ASTER bands, 2. MLC using ASTER bands and DEM, 3. MLC using ASTER bands and slope, 4. MLC using ASTER bands and plan curvature, 5. MLC using ASTER bands and profile curvature, 6. MLC using ASTER bands and drainage density and finally 7. MLC using ASTER bands and all ancillary data. The results revealed that integrating topographical parameters aid in improvement of classification where spectral information is not sufficient to discriminate between classes of interest. An increase of more than 5% is observed in overall accuracy for the all ancillary data integration case. Moreover more than 10% improvement for most of the classes was identified. However from the results it is evident that the areal extent of the classified units causes constraints on application of the methodology.
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Shearer, Andrew. "The application of ground based and airborne radiometric methods to aid geological mapping in the Olary Province, South Australia /." Title page, abstract and contents only, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbs539.pdf.

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Nygren, Michelle. "Geological Mapping of the Glenurquhart Complex near Loch Ness, Scotland." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-131062.

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Giacomini, Lorenza. "GEOLOGICAL MAPPING AND ANALYSIS OF DAEDALIA PLANUM LAVA FIELD (MARS)." Doctoral thesis, Università degli studi di Padova, 2010. http://hdl.handle.net/11577/3422244.

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Volcanism is the most important rock-forming processes of the planetary surfaces and represents one of the main clues to investigate the chemical composition of the interior and the thermal history of a planet. Our study has been focused on the Daedalia Planum volcanic region, located to south-west of Arsia Mons, where some of the longest lava flows on Mars were emplaced. THEMIS, MOC and HiRISE images were analyzed in order to perform a stratigraphic and morphological analysis of the area and realize a Daedalia Planum geological map where different flow units are represented. Several features observed on the flow surface have been interpreted as related to inflation processes on the basis of several similarities with the morfologies of the inflated terrestrial Payen Matru flows (Argentina). This suggests that inflation process is quite common for the Daedalia Planum field, implying that the inflation emplacement mechanism on Martian flows could be more frequent than previously supposed and, consequently, effusion rates and rheological properties of Martian lavas more variable. In addition, a comparative study performed between the mounds detected on Daedalia Planum and Elysium Planitia regions seems to further confirm the tumuli nature of the Daedalia Planum features and thus the presence of inflated flows in this volcanic field. The OMEGA data reveal that Daedalia Planum lavas have a spectral response coherent with a basaltic composition. In addition the Spectral Angle Mapper (SAM) classification obtained from the OMEGA data highlights that the flows are characterized by distinctive spectral responses, which should depend on non-compositional factors, like different surface textures of flows but also different mineralogy or rock texture, such as the presence of glass, crystal size or crystal isoorientation.<br>Il vulcanismo è uno dei più importanti processi che interessano la superficie di un pianeta e rappresenta una delle chiavi per investigare la composizione chimica del suo interno nonché la sua storia termica. Il nostro studio si è focalizzato sul campo vulcanico di Daedalia Planum, a sud ovest di Arsia Mons, dove si trovano alcune delle più lunghe colate conosciute su Marte. Varie immagini di THEMIS, MOC e HiRISE sono state analizzate con l'obiettivo di studiare questa regione sia dal punto di vista stratigrafico che morfologico e di creare una mappa geologica della regione. Da questa analisi sono state individuate varie forme interpretate come collegate al processo di inflation e il confronto con le colate inflate terrestri del Payen (Argentina) sembrano confermare tale ipotesi. Ciò suggerisce che l’inflation è piuttosto comune nel capo lavico di Daedalia Planum e che, in generale, questo processo interessi più colate di Marte di quanto supposto finora. Di conseguenza i tassi di eruzione e le proprietà reologiche delle lave su Marte potrebbero essere molto più variabili. Uno studio comparativo tra le forme a cupola individuate su Daedalia Planum ed Elysium Planitia confermerebbe ulteriormente che su Daedalia Planum vi è effettivamente la presenza di tumuli e, quindi, di colate laviche inflate. Infine, prendendo in considerazione i dati OMEGA della regione, si è appurato che le lave presenti su Daedalia Planum hanno una risposta spettrale coerente con una composizione basaltica. Le classificazioni SAM ottenute da dati OMEGA evidenziano, inoltre, come le colate della regione siano effettivamente caratterizzate da distinte risposte spettrali, verosimilmente attribuibili a fattori non composizionali quali la diversa tessitura superficiale o la differente mineralogia e tessitura della roccia, come la presenza di vetro, la dimensione dei cristalli o la loro isoorientazione.
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Wilson, Kenneth T. "Shoreface mapping and sand resource inventory North Topsail Beach and Surf City, North Carolina /." View electronic thesis (PDF), 2009. http://dl.uncw.edu/etd/2009-1/willsonk/kennethwillson.pdf.

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Ho, Chiu-shek. "Stereographic projection and mapping of engineering geology case study near Jordan Valley, Hong Kong /." Click to view the E-thesis via HKUTO, 2007. http://sunzi.lib.hku.hk/hkuto/record/B38848673.

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McCracken, Janet Rae. "Phenomenographic instructional design : case studies in geological mapping and materials science." Thesis, Open University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.270015.

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McCracken, Janet. "Phenomenographic instructional design : case studies in geological mapping and materials science." n.p, 2001. http://ethos.bl.uk/.

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Guerrero, Francisco Jesus. "Death Valley reconstruction new piercingpoints in the Panamint Mountains and Resting Springs Range /." 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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Bargel, Terje H. "Quaternary geological Mapping of Fennoscandia and Nordland : Deglaciation, Deposits, Stratigraphy and Applications." Doctoral thesis, Norwegian University of Science and Technology, Faculty of Engineering Science and Technology, 2003. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-1803.

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<p>Quaternary geological mapping is performed by geological surveys in most countries. At the Geological Survey of Norway (NGU), mapping of the surficial deposits has been one of the main tasks from the establishment of the institution in 1858, in the beginning mainly as an aid for agriculture and forestry. During recent decades, society's needs for information on the Quaternary deposits has increased, particularly within the fields of environment and health, physical planning, economy and supply of natural resources.</p><p>Geological mapping is not looked upon as a science by everyone, but its results have often proved to be valuable in a scientific context as the extensive database the maps represent give valuable information, useful in, e.g. the study of regional trends. Geological mapping can, however, be regarded as a journey of discovery, which is the basis for most scientific research on the development of the earth's crust and which provides a framework with which all laboratory-based research must be compatible.</p><p>Much detail information is also recorded (analog or digital), for example the location of exposed sections in distant areas and details beyond the reach of aerial photo interpretation, e.g. in heavily forested areas or of objects too small to be identified on aerial photos or maps. In addition, much sedimentological and stratigraphical work has to be performed during the fieldwork in order to understand the genesis of the deposits. Creation of geological models of the areas is an important part of the mapping activity that is necessary for attainment of an understanding of the Quaternary geological history on a regional scale.</p><p>What could be criticized is the fact that the many mapping geologists involved have not used, or have had the opportunity to use, the enormous data at hand to do more science and to tell the layman what the results of the geological mapping mean.</p><p>This thesis is a contribution to understanding of the Quaternary geology of Central Fennoscandia with special emphasis on the Nordland area. The thesis has the following aims:</p><p>A. To compile four Quaternary geological maps of Central Fennoscandia (showing surficial deposits, geomorphology and paleohydrography, ice flow indicators and stratigraphy) and a Quaternary geological map of the surficial deposits of Nordland.</p><p>B. To create a link between the Quaternary geological maps, applications of the map-data and studies of Quaternary geological history (Part I).</p><p>C. To present a coordinated description of the five Quaternary geological maps and compile a review of the Late Weichselian and Early Holocene deglaciation history of the mapped area (Part II).</p><p>D. To identify areas for in-depth investigation of the deglaciation and to perform these studies (Part III).</p><p>A. COMPILATION OF QUATERNARY GEOLOGICAL MAPS</p><p>This thesis is based on the data included in five maps of Quaternary Geology (Fig. A1):</p><p>1. Quaternary Deposits of Central Fennoscandia (scale 1:1,000,000) (Fig. A2)</p><p>2. Glacial Geomorphology and Palaeohydrography of Central Fennoscandia (scale 1:1,000,000) (Fig. A3)</p><p>3. Ice-flow Indicators of Central Fennoscandia (scale 1:1,000,000) (Fig. A4)</p><p>4. Quaternary Stratigraphy of Central Fennoscandia (scale 1:2,000,000) (Fig. A4)</p><p>5. Quaternary Deposits in Nordland County (scale 1:400,000) (Fig. A5)</p><br>Due to copyright enclosures 1-5 are not included in the online version of this thesis, neither is the CD-ROM referred to in page 14.
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Books on the topic "Geological mapping"

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Dearman, W. R. Engineering geological mapping. Butterworth-Heinemann, 1991.

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Barnes, J. W. Basic Geological Mapping. John Wiley & Sons, Ltd., 2004.

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Barnes, J. W. Basic geological mapping. 2nd ed. Open University Press, 1990.

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Basic geological mapping. 3rd ed. Wiley, 1995.

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Peter, Brabham, Barnes, J. W. (John Wykeham), 1921-, and Barnes, J. W. (John Wykeham), 1921-, eds. Basic geological mapping. 5th ed. Wiley, 2011.

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E, Bischke Richard, ed. Applied subsurface geological mapping. Prentice Hall, 1991.

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Andrea, Förster, Merriam Daniel Francis, and International Association for Mathematical Geology. 25th Anniversary Meeting, eds. Geologic modeling and mapping. Plenum Press, 1996.

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Geological Survey (U.S.), ed. National Geologic Mapping Program: Goals, objectives, and long-range plans. U.S. Geological Survey, Federal Center, 1987.

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Berg, Richard C. Stack-unit geologic mapping: Color-coded and computer-based methodology. Illinois State Geological Survey, 1993.

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Woodward, Nicholas B. Balanced geological cross-sections: An essential technique in geological research and exploration. American Geophysical Union, 1989.

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Book chapters on the topic "Geological mapping"

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Wang, Chengbin, and Xiaogang Ma. "Digital Geological Mapping." In Encyclopedia of Mathematical Geosciences. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-26050-7_88-1.

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Wang, Chengbin, and Xiaogang Ma. "Digital Geological Mapping." In Encyclopedia of Mathematical Geosciences. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-030-85040-1_88.

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Marjoribanks, Roger. "Geological Mapping in Exploration." In Geological Methods in Mineral Exploration and Mining. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-540-74375-0_2.

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Marjoribanks, Roger W. "Geological Mapping in Exploration." In Geological Methods in Mineral Exploration and Mining. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5822-0_2.

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Marjoribanks, Roger. "Mine Mapping." In Geological Methods in Mineral Exploration and Mining. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-540-74375-0_3.

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Marjoribanks, Roger W. "Mine Mapping." In Geological Methods in Mineral Exploration and Mining. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5822-0_3.

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Mironov, Oleg. "3-Dimensional Geological Mapping. Applications to Urban Geological Environment." In Engineering Geology for Society and Territory - Volume 5. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_180.

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Singhroy, Vernon H., and Mark Pilkington. "Geological Mapping Using Earth’s Magnetic Field." In Encyclopedia of Remote Sensing. Springer New York, 2014. http://dx.doi.org/10.1007/978-0-387-36699-9_38.

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Blatnik, Matej, David C. Culver, Franci Gabrovšek, et al. "Structural–Geological Mapping of Karst Areas." In Advances in Karst Science. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-26827-5_1.

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Lombardo, Vincenzo, Fabrizio Piana, Dario Mimmo, Enrico Mensa, and Daniele P. Radicioni. "Semantic Models for the Geological Mapping Process." In AI*IA 2017 Advances in Artificial Intelligence. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-70169-1_22.

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Conference papers on the topic "Geological mapping"

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Delattre, Marc P. "GEOLOGIC MAPPING ACTIVITIES AT THE CALIFORNIA GEOLOGICAL SURVEY." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274321.

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Bossum, W. "Geophysics in Geological Mapping." In 3rd International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609-pdb.324.487.

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Du, Ying. "Research on 3D geological modeling method of complex geological body and application of geological engineering combined fracturing." In Fourth International Conference on Geoscience and Remote Sensing Mapping (GRSM 2022), edited by Tarun Kumar Lohani. SPIE, 2023. http://dx.doi.org/10.1117/12.2668088.

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Laake, A., and M. Francis. "Geological Process Mapping from Seismic Data." In 77th EAGE Conference and Exhibition 2015. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201412608.

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Miecznik, J., and W. Klitynski. "Mapping geological structures with magnetotelluric method." In 58th EAEG Meeting. EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201408842.

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MacNae, J., and Y. P. Yang. "Geological Mapping Using Airborne EM Data." In 61st EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609.201407904.

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Thorleifson, Harvey. "ARRANGEMENTS FOR SEAMLESS 3D GEOLOGICAL MAPPING." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-352620.

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Weathers, Taylor Andrew, Roy B. Van Arsdale, and David Arellano. "GEOLOGICAL MAPPING IN LAKE COUNTY, TENNESSEE." In 52nd Annual GSA South-Central Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018sc-310003.

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Williams, David A., Jacob E. Bleacher, W. Brent Garry, and Kyle J. Mohr. "GEOLOGICAL MAPPING OF MARS' THARSIS VOLCANOES." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321048.

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Pendock, Neil. "Radio-wave tomography for geological mapping." In Optical Engineering and Photonics in Aerospace Sensing, edited by Nancy K. Del Grande, Ivan Cindrich, and Peter B. Johnson. SPIE, 1993. http://dx.doi.org/10.1117/12.160331.

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Reports on the topic "Geological mapping"

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Pugin, A. J. M., and T. H. Larson. Geological mapping using geophysics. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/299503.

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Palacky, G. J. Geological Background To Resistivity Mapping. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/122343.

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Russell, H. A. J., R. C. Berg, and L. H. Thorleifson. Introduction - three-dimensional geological mapping. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289610.

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Harris, J., E. M. Schetselaar, T. Lynds, and E. A. de Kemp. Remote predictive mapping: A strategy for geological mapping of Canada's north. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/226009.

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Russell, H. A. J., R. C. Berg, and L. H. Thorleifson. Three-dimensional geological mapping, workshop extended abstracts. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289609.

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McKean, Adam P., Zachary W. Anderson, Donald L. Clark, et al. Detrital Zircon U-Pb Geochronology Results for the Bountiful Peak, Coalville, James Peak, Mount Pisgah, Paradise, and Payson Lakes 7.5' Quadrangles, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ofr-743.

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Abstract:
This Open-File Report makes available raw analytical data from laboratory analysis of U-Pb ages of zircon grains from samples collected during geologic mapping funded by the U.S. Geological Survey (USGS) National Cooperative Geologic Mapping Program (STATEMAP) and the Utah Geological Survey (UGS). The references listed in table 1 provide additional information such as sample location, geologic setting, and interpretation of the samples in the context of the area where they were collected. The data were prepared by the University of Utah Earth Core Facility (Diego Fernandez, Director), under contract to the UGS. These data are highly technical in nature and proper interpretation requires considerable training in the applicable geochronologic techniques.
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Russell, H., L. H. Thorleifson, and R. C. Berg. Introduction - three-dimensional geological mapping for groundwater applications. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221843.

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Morris, W. A., H. Ugalde, H. Slavinski, and K. Markham. Case study 8. Geological mapping derived from topography. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/226027.

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Waanders, Gerald. Palynology Evaluation Results From the Duchesne 30' x 60' Quadrangle, Duchesne and Wasatch Counties, Utah. Utah Geological Survey, 2023. http://dx.doi.org/10.34191/ofr-750.

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This Open-File Report makes available data from palynology evaluations completed to determine the age and depositional environment of rock samples collected during geologic investigations funded or partially supported by the Utah Geological Survey (UGS) and the U.S. Geological Survey National Cooperative Geologic Mapping Program (STATEMAP). Table 1 provides the sample numbers and locations for the palynology data. The reference listed in table 1 provides additional information such as sample location, geologic setting, and interpretation of the samples in the context of the area where they were collected.
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Dodds, C. J. Geological mapping in Tatshenshini River map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122684.

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