Academic literature on the topic 'Geology, Structural Geological mapping'

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Journal articles on the topic "Geology, Structural Geological mapping"

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Searight, Thomas Kay, and David Henry Malone. "A Geologic Mapping Problem for Structural Geology Class." Journal of Geoscience Education 44, no. 3 (1996): 253–58. http://dx.doi.org/10.5408/1089-9995-44.3.253.

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Battaglini, L., S. D′Angelo, and A. Fiorentino. "Mapping geological events in submerged areas." Quarterly Journal of Engineering Geology and Hydrogeology 54, no. 1 (2020): qjegh2020–031. http://dx.doi.org/10.1144/qjegh2020-031.

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EMODnet Geology Project work package 6 collects information regarding ‘Geological events and probabilities’, including submarine landslides, earthquakes, volcanic centres, tsunamis, fluid emissions and tectonics. The elaboration of guidelines to compile GIS layers was aimed at identifying parameters to be used to thoroughly characterize each event. Particular attention has been devoted to the definition of the ‘Attribute tables’ in order to achieve the best degree of harmonization and standardization complying with the European INSPIRE Directive. Due to the different geological settings of Eur
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Bailey, Christopher McNeill. "An Integrative Geologic Mapping Project for Structural-Geology Courses." Journal of Geoscience Education 46, no. 3 (1998): 245–51. http://dx.doi.org/10.5408/1089-9995-46.3.245.

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van Reed, E., S. Maclnnes, and M. Smith. "Case histories and modelling interpretation in CSAMT." Exploration Geophysics 20, no. 2 (1989): 121. http://dx.doi.org/10.1071/eg989121.

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Two CSAMT case history studies are presented in which modelling has been applied to data in order to produce geo-electric depth sections. These sections then assist in developing an idealized geologic model used as part of a geological exploration programme. At the geological planning level, one can define certain key geologic features which need to be identified as part of an exploration programme. Modelling may give some indication as to the success of a particular planned geophysical programme.At the interpretation level, modelling can be used to confirm or disprove geologic ideas previousl
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KOWALSKI, Aleksander. "LANDSLIDES AND THE INCORRECT INTERPRETATION OF GEOLOGICAL STRUCTURE – EXAMPLES FROM THE SUDETY MOUNTAINS." Biuletyn Państwowego Instytutu Geologicznego 473, no. 473 (2018): 27–48. http://dx.doi.org/10.5604/01.3001.0012.7708.

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Despite the relatively large number of individual landslides recognized and described over the last several years from the Sudety (Sudetes) Mountains (Lower Silesia, SW Poland), most of the papers focused on the geomorphological characterisation of these forms. This paper presents the results of geological and geomorphological mapping of individual landslides, recognized within three geological units: the Wleń Graben (Northsudetic Synclinorium), the Łączna Elevation (Intrasudetic Synclinorium) and the Glinno Graben (Sowie Mountains Block). Particular attention has been paid to the role of the
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Drury, S. A. "SPOT image data as an aid to structural mapping in the southern Aravalli Hills of Rajasthan, India." Geological Magazine 127, no. 3 (1990): 195–207. http://dx.doi.org/10.1017/s0016756800014485.

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AbstractThe 10 to 20 m resolution of SPOT image data, together with their potential for stereoscopic viewing, provides an excellent base for geological mapping inremote and rugged terrain that is akin to high-level aerial photographs. Their large format (60 × 60 km) also gives the advantage of synoptic coverage that ranks with images from the Landsat series of satellites. Use of stereo pairs of single-band SPOT images has enabled some revision of existing geological maps of the southern Aravalli Hills in Rajasthan at a scale of 1:100000, and has added significantly to knowledge of their comple
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Al-Nahmi, F., O. Saddiqi, A. Hilali, et al. "APPLICATION OF REMOTE SENSING IN GEOLOGICAL MAPPING, CASE STUDY Al MAGHRABAH AREA – HAJJAH REGION, YEMEN." ISPRS Annals of Photogrammetry, Remote Sensing and Spatial Information Sciences IV-4/W4 (November 13, 2017): 63–71. http://dx.doi.org/10.5194/isprs-annals-iv-4-w4-63-2017.

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Remote sensing technology plays an important role today in the geological survey, mapping, analysis and interpretation, which provides a unique opportunity to investigate the geological characteristics of the remote areas of the earth's surface without the need to gain access to an area on the ground. The aim of this study is achievement a geological map of the study area. The data utilizes is Sentinel-2 imagery, the processes used in this study, the OIF Optimum Index Factor is a statistic value that can be used to select the optimum combination of three bands in a satellite image. It’s based
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Bessen, Ryan, Jennifer Gifford, Zack Ledbetter, Sean McGuire, Kyle True, and David Malone. "Geologic Map of the Park Reservoir Quadrangle, Sheridan County, Wyoming." Mountain Geologist 57, no. 4 (2020): 375–88. http://dx.doi.org/10.31582/rmag.mg.57.4.375.

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This project involved the construction of a detailed geologic map of the Park Reservoir, Wyoming 7.5-Minute Quadrangle (Scale 1:24,000). The Quadrangle occurs entirely in the Bighorn National Forest, which is a popular recreation site for thousands of people each year. This research advances the scientific understanding of the geology of the Bighorn Mountains and the Archean geology of the Wyoming Province. Traditional geologic mapping techniques were used in concert with isotopic age determinations. Our goal was to further subdivide the various phases of the 2.8–3.0 Ga Archean rocks based on
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Hollis, Julie A., Dirk Frei, Jeroen A. M. Van Gool, Adam A. Garde, and Mac Persson. "Using zircon geochronology to resolve the Archaean geology of southern West Greenland." Geological Survey of Denmark and Greenland (GEUS) Bulletin 10 (November 29, 2006): 49–52. http://dx.doi.org/10.34194/geusb.v10.4908.

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Until recently, in situ U-Pb zircon geochronology could be carried out only using ion microprobes, requiring lengthy analysis times of c. 20 minutes. However, new developments in laser ablation inductively coupled plasma mass spectrometer technologies have resulted in zircon geochronology techniques that are much faster, simpler, cheaper, and more precise than before (e.g. Frei et al. 2006, this volume). Analyses approaching the precision obtained via ion microprobe can now be undertaken in 2–4 minutes using instruments such as the 213 nm laser ablation (LA) system coupled with Element2 sector
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Gaich, Andreas, and Gerald Pischinger. "3D images for digital geological mapping." Geomechanics and Tunnelling 9, no. 1 (2016): 45–51. http://dx.doi.org/10.1002/geot.201500048.

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Dissertations / Theses on the topic "Geology, Structural Geological mapping"

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Centeno-García, Elena. "Tectonic evolution of the Guerrero terrane, western Mexico." Diss., The University of Arizona, 1994. http://hdl.handle.net/10150/186665.

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The Guerrero terrane of western Mexico is characterized by an Upper Jurassic-Lower Cretaceous volcanic-sedimentary sequence of arc affinity. The arc assemblage rests unconformably on partially metamorphosed rocks of possible Triassic-Jurassic age. These "basement units," the Arteaga and Placeres Complexes and the Zacatecas Formation, are composed of deformed turbidites, basalts, volcanic-derived graywackes, and blocks of chert and limestone. Sandstones from the basement units are mostly quartzitic and have a recycled orogen-subduction complex provenance. They have negative ᵋNdi (-5 to -7), mod
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Armstrong, Thomas Robert. "Structural and Petrologic Evolution of Acadian Dome Structures in Southern Vermont." Diss., Virginia Tech, 1995. http://hdl.handle.net/10919/37857.

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Petrologic and thermobarometric studies, coupled with geologic mapping and structural analysis, provide critical evaluation of several different models for Acadian (Late Silurian to Middle Devonian) dome evolution in southern Vermont. Previous models considered diapiric uprise and composite nappe-stage crustal thickening and subsequent diapirism as likely causes of dome formation. Both of these previous models result in symmetrical distribution of P-T values about the dome structures with corresponding coreward increases in temperature, and typically, coreward decrease in associated pressures.
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Copfer, Torrey J. "Geology of the Deseret Peak East 7.5' Quadrangle, Tooele County, Utah, and Impacts for Hydrology of the Region." DigitalCommons@USU, 2003. https://digitalcommons.usu.edu/etd/6723.

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Detailed geologic mapping of the Deseret Peak East 7.5' Quadrangle yields new interpretations regarding the stratigraphy of the Oquirrh Basin, fault and fold geometry, and structural evolution of the region. The Stansbury Range consists of the north-southtrending Deseret anticline. Basal Mississippian units rest unconformably on Cambrian beds in the central part of the range. Paleozoic uplift, Mesozoic contraction, and Cenozoic extension have created a series of broad folds, large thrust faults, and several normal faults. The area is dominated by bedrock springs, with the presence of abundant
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Foy, Travis A. "Quaternary faulting in Clayton Valley, Nevada: implications for distributed deformation in the Eastern California shear zone-walker lane." Thesis, Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/39561.

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The eastern California shear zone (ECSZ) and Walker Lane belt represent an important inland component of the Pacific-North America plate boundary. Current geodetic data indicate accumulation of transtensional shear at a rate of ~9.2 ± 0.3 mm/yr across the region, more than double the total geologic rate (<3.5 mm/yr) for faults in the northern ECSZ over the late Pleistocene [Bennett et al., 2003, Kirby et al., 2006, Lee et al., 2009, Frankel et al., 2007]. Unraveling the strain puzzle of the Walker Lane is therefore essential to understanding both how deformation is distributed through the lit
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Surtees, Grant Bradley. "The evolution of the Brosterlea Volcanic Complex, Eastern Cape, South Africa." Thesis, Rhodes University, 2000. http://hdl.handle.net/10962/d1005556.

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Detailed field mapping (Map, Appendix B) has been conducted in and around the boundaries of a 14x18km, volcanic complex 35km northeast of Molteno in the Eastern Cape Province, South Africa. The structure is interpreted as a subsidence structure, and is filled with two volcaniclastic breccias, numerous lava flows, a number of sedimentary facies, and lies on a base of Clarens Formation overlying Elliot Formation rocks. This is an important study because 'widespread, voluminous fields of basaltic breccias are very rare (see Hanson and Elliot, 1996) and this is the first time that this type of vol
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Haddox, David A. "Mapping and Kinematic Structural Analysis of the Deep Creek Fault Zone, South Flank of the Uinta Mountains, Near Vernal, Utah." Diss., CLICK HERE for online access, 2005. http://contentdm.lib.byu.edu/ETD/image/etd819.pdf.

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Rohrer, Lucas P. "BEDROCK GEOLOGIC MAPPING AND STRUCTURAL ANALYSIS OF THE WESTERN HALF OF THE PETERSHAM QUADRANGLE, CENTRAL MASSACHUSETTS: FURTHER TESTS OF THE MODEL FOR MIDDLE TO LATE PALEOZOIC DUCTILE TRANSPRESSION, VERTICAL EXTRUSION, AND LATERAL ESCAPE IN THE NORTHERN APPALACHIANS." UKnowledge, 2015. http://uknowledge.uky.edu/ees_etds/32.

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Bedrock mapping, structural analysis, and geochronology reveal the distribution of lithologies and timing of metamorphism and deformation in the western half of the Petersham 7.5’ quadrangle, western Massachusetts. Underlying lithologies are: (from west to east) the Ordovician Monson granitic orthogneiss, Silurian Rangeley migmatitic paragneiss, and Late Devonian (357 Ma) Hardwick tonalitic orthogneiss. Their tightly folded contacts strike north to south. The 361 Ma, unfoliated, strike-parallel Nichewaug quartz-diorite (10-100 m wide) intrusion spans the map area within the Rangeley. Evidence
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Liu, Yung-Chun. "Tectonics of Saturn's Moon Titan AND Tsunami Modeling of the 1629 Mega-thrust Earthquake in Eastern Indonesia." BYU ScholarsArchive, 2014. https://scholarsarchive.byu.edu/etd/5731.

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Chapter 1-2:The Cassini RADAR mapper has imaged elevated blocks and mountains on Titan we term ‘ridges’. Two unresolved problems regarding Titan's surface are still debated: what is the origin of its ridges and was there tectonic activity on Titan? To understand the processes that produced the ridges, in this study, (1) we analyze the distribution and orientation of ridges through systematic geomorphologic mapping and (2) we compare the location of the ridges to a new global topographic map to explore the correlation between elevation and ridges and the implications for Titan's surface evoluti
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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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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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Books on the topic "Geology, Structural Geological mapping"

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Mikhaĭlov, A. E. Structural geology and geological mapping. Mir Publishers, 1987.

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Structural geology and geological mapping. Mir, 1987.

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Mikhailov, A. Ye. Structural Geology and geological Mapping. Mir, 1987.

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E, Bischke Richard, ed. Applied subsurface geological mapping: With structural methods. 2nd ed. Prentice Hall, 2003.

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McClay, K. R. The mapping of geological structures. Open University Press, 1987.

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McClay, K. R. The mapping of geological structures. John Wiley & Sons, 1997.

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The mapping of geological structures. Open University Press, 1987.

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Geological maps: An introduction. Van Nostrand Reinhold, 1990.

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Maltman, Alex. Geological maps: An introduction. Open University Press, 1990.

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Maltman, Alex. Geological maps: An introduction. 2nd ed. John Wiley, 1998.

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Book chapters on the topic "Geology, Structural Geological mapping"

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Shogenova, Alla. "Use of the Computer for the Structural Analysis of the Ordovician Sedimentary Basin in Estonia." In Geologic Modeling and Mapping. Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_10.

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Park, R. G. "Geological structure and plate tectonics." In Foundations of Structural Geology. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-011-6576-1_15.

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Groshong, Richard H. "Mapping Faults and Faulted Surfaces." In 3-D Structural Geology. Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-662-03912-0_6.

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Dowd, P. A. "Geological and Structural Control in Kriging." In Quantitative Geology and Geostatistics. Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1739-5_74.

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Groshong, Richard H. "Cross Sections, Data Projection and Dip-Domain Mapping." In 3-D Structural Geology. Springer Berlin Heidelberg, 2006. http://dx.doi.org/10.1007/978-3-540-31055-6_6.

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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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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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Osipov, Victor. "Large-Scale Thematic Geological Mapping of Moscow Area." In Engineering Geology for Society and Territory - Volume 5. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_2.

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Banerjee, Saikat, Narayan Bose, and Soumyajit Mukherjee. "Field Structural Geological Studies Around Kurseong, Darjeeling-Sikkim Himalaya, India." In Tectonics and Structural Geology: Indian Context. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_16.

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Pundalik, Ashwin, Shiba Nikalje, Arnav Samant, and Hrishikesh Samant. "Geological Field Guide: Malvan (Maharashtra, India)." In Structural Geology and Tectonics Field Guidebook — Volume 1. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60143-0_17.

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Conference papers on the topic "Geology, Structural Geological mapping"

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Clegg, Nigel Mark, Ana Beatriz Domingues, Rosamary Ameneiro Paredes, et al. "Mapping Complex Geological Surface Morphology During Landing Operations Using 3-D Inversion of Ultra-Deep Electromagnetic LWD Data." In Offshore Technology Conference. OTC, 2021. http://dx.doi.org/10.4043/31216-ms.

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Abstract Ultra-deep azimuthal electromagnetic (EM) logging-while-drilling (LWD) tools are frequently used during landing operations for early detection of the reservoir top. This enables alterations to the well plan before the reservoir is penetrated. To date, this approach has relied on one-dimensional (1-D) inversions that accounts only for changes in resistivity above or below the wellbore. When geology is complex, resulting in lateral changes in resistivity, 3-D inversion of EM data is required to provide increased reservoir understanding. This paper presents a case study from offshore Bra
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Mele, Maurizio, Filippo Chinellato, Andrea Leone, Francesca Arata, Caterina Cappannelli, and Matteo Medaglia. "MULTISCALE LOGGING WHILE DRILLING DATA INTEGRATION UNVEILED COMPLEX GEOLOGICAL SCENARIO WHILE GEOSTEERING." In 2021 SPWLA 62nd Annual Logging Symposium Online. Society of Petrophysicists and Well Log Analysts, 2021. http://dx.doi.org/10.30632/spwla-2021-0083.

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The first Eni geosteering operation in Mexico was executed during the global COVID-19 crisis. The complex geology and the uncertainty related to this undrilled portion of the reservoir determined the employment of advanced Logging While Drilling (LWD) technology for real-time geosteering and a comprehensive geological interpretation. The target is an oil bearing sandstone reservoir, represented by deltaic front sands bars within an anticline structure on a salt core with faults and lateral heterogeneity. A sedimentological conceptual model was used to feed the 3D geological model, supporting a
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Mering, Catherine, and Jean-Francois Parrot. "Filtering of radar images for geological structural mapping." In Satellite Remote Sensing, edited by Jacky Desachy. SPIE, 1994. http://dx.doi.org/10.1117/12.196773.

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Kolb, Dakota James, and Jennifer N. Gifford. "DEVELOPMENT OF COMPARATIVE TECTONIC MODELS USING STRUCTURAL AND PETROGRAPHIC APPLICATIONS TO GEOLOGIC MAPPING." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285127.

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Beiranvand Pour, Amin, and Mazlan Hashim. "PALSAR remote sensing data for structural geology mapping in tropical environments." In 2015 International Conference on Space Science and Communication (IconSpace). IEEE, 2015. http://dx.doi.org/10.1109/iconspace.2015.7283777.

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Sparks, C. Renee, and Issac J. Jacques. "GEOLOGIC MAPPING AND LITHOSPHERIC DEFORMATION IN THE STRUCTURALLY COMPLEX REGION OF CENTRAL-WESTERN HONDURAS." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-326621.

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Mitchell, G. "Highly Accurate Stereo Satellite Elevation Mapping For Geomorphology, Structural Geology and Project Engineering." In Remote Sensing 2012. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143276.

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Rocca, Riccardo. "Low cost 3d mapping using a commercial drone/UAV: Application in structural geology." In International Conference and Exhibition, Barcelona, Spain, 3-6 April 2016. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2016. http://dx.doi.org/10.1190/ice2016-6462962.1.

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Barbosa da Silva, Fernando, and José Joaquim Gonçalves Rodrigues. "Surface Geological Mapping Using 3D Seismic Attributes As An Aid To Subsurface Geology Understanding: An Example." In 7th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.217.376.

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Logvin, V. M., and P. G. Pigulevskiy. "Investigation of the possibilities of potential fields structural transformations in geological mapping." In 16th International Conference on Geoinformatics - Theoretical and Applied Aspects. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701852.

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Reports on the topic "Geology, Structural Geological mapping"

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Behnia, P., J. R. Harris, C. Harrison, et al. Geo-mapping Frontiers: compilation and interpretation of geologic structures north of 60°, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292917.

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James, D. T. Geological Mapping of the Sleepy Dragon Complex and the Cameron River Metavolcanic Belt, Slave Province: Basement - Cover Stratigraphic and Structural Relations. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133327.

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Church, M., J. Y. Chagnon, E. A. Christiansen, S. B. McCann, H. W. Nasmith, and G. C. Topp. Mapping the landscape: report of the Canadian Geoscience Council Advisory Committee to the Geological Survey of Canada on outputs in Quaternary and engineering geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/125168.

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Herriott, T. M., M. A. Wartes, R. J. Gillis, et al. Detailed geologic mapping and overview of structural and stratigraphic studies in the east-central North Slope foothills, Alaska (poster): 3P Arctic, The Polar Petroleum Potential Conference, 30 August–2 September 2011, Halifax, Nova Scotia, Canada. Alaska Division of Geological & Geophysical Surveys, 2011. http://dx.doi.org/10.14509/27041.

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Herriott, T. M., M. A. Wartes, P. L. Decker, et al. Structural and stratigraphic implications of detailed geologic mapping of Ellesmerian and Brookian units in the Echooka and Ivishak rivers region, east-central North Slope, Alaska (poster): AAPG Pacific Section Meeting, Anchorage, AK, May 10, 2011. Alaska Division of Geological & Geophysical Surveys, 2011. http://dx.doi.org/10.14509/22802.

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Real Fernández, Elena. ¿PUEDE HABER 5 FASES DE DEFORMACIÓN HERCÍNICA EN LA ZONA DE VALDEMORILLO (MADRID)? Ilustre Colegio Oficial de Geólogos, 2020. http://dx.doi.org/10.21028/erf.2020.10.27.

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This work aims to understand the processes that have taken part in the deformation, both on a small and large scale, of metamorphic materials in Valdemorillo area, located in the west of the Community of Madrid and within the Spanish Central System. The objective is to understand the kinematic evolution and the specific mechanical behaviour of igneous-metamorphic materials from the area, deformed by certain efforts developed throughout the Hercynian Orogeny. Therefore, a structural analysis has been carried out throughout a geological mapping scaled 1: 25000 and the analysis of various petrogr
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