Relevant bibliographies by topics / Thin section (Geology)

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

Academic literature on the topic 'Thin section (Geology)'

Author: Grafiati
Published: 4 June 2021
Last updated: 17 February 2022

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Journal articles on the topic "Thin section (Geology)"

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Moxon, Terry. "Agate in Thin Section." Rocks & Minerals 89, no. 4 (2014): 328–39. http://dx.doi.org/10.1080/00357529.2014.904663.

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Nentwich, F. W., and R. W. Yole. "Polished thin section preparation of fine-grained siliciclastic rocks." Journal of Sedimentary Research 61, no. 4 (1991): 624–26. http://dx.doi.org/10.1306/d426778a-2b26-11d7-8648000102c1865d.

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Francus, P. "Quantification of Bioturbation in Hemipelagic Sediments Via Thin-Section Image Analysis." Journal of Sedimentary Research 71, no. 3 (2001): 501–7. http://dx.doi.org/10.1306/2dc4095a-0e47-11d7-8643000102c1865d.

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Smith, S. J., and R. S. Anderson. "A method for impregnating soft sediment cores for thin-section microscopy." Journal of Sedimentary Research 65, no. 3a (1995): 576–77. http://dx.doi.org/10.1306/d4268153-2b26-11d7-8648000102c1865d.

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Srisutthiyakorn, Nattavadee, Sander Hunter, Rituparna Sarker, Ronny Hofmann, and Irene Espejo. "Predicting elastic properties and permeability of rocks from 2D thin sections." Leading Edge 37, no. 6 (2018): 421–27. http://dx.doi.org/10.1190/tle37060421.1.

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Predicting rock elastic properties and permeability from high-resolution 2D thin sections has been a challenging problem in rock physics because the 2D thin sections reveal very little about how the microstructure connects in the third dimension. However, 2D thin sections are widely available and inexpensive because they are often produced as a part of the reservoir-quality workflow. Furthermore, they have much higher resolution and greater field of view than micro X-ray computed tomography images, which are commonly used for rock properties estimation. The 2D thin sections we studied are from
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Fei, Sun, Qiu Han Qin, Sheng Hao Zhou, and Li Peng. "Research on Reservoir Characteristics in San Zhao Peripheral Zone." Advanced Materials Research 986-987 (July 2014): 722–24. http://dx.doi.org/10.4028/www.scientific.net/amr.986-987.722.

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Using a large number of core, logging and seismic data, on the basis of sequence stratigraphy, reservoir geology, sedimentology, such as theory, the San Zhao peripheral zone were studied. FuYu reservoir is studied and Yang DaChengZi reservoir structure of reservoir. Based on coring well cores observation and rock thin section, casting thin sections and scanning electron microscopy (sem) analysis techniques, such as the SQ3–Y1 a sedimentary period main sedimentary, main lithological types, and different oil reservoir is studied.
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Tang, David G., Kitty L. Milliken, and Kyle T. Spikes. "Machine learning for point counting and segmentation of arenite in thin section." Marine and Petroleum Geology 120 (October 2020): 104518. http://dx.doi.org/10.1016/j.marpetgeo.2020.104518.

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Maithel, Sarah A., Leonard R. Brand, and John H. Whitmore. "A Methodology For Disaggregation and Textural Analysis of Quartz-cemented Sandstones." Journal of Sedimentary Research 89, no. 7 (2019): 599–609. http://dx.doi.org/10.2110/jsr.2019.35.

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AbstractSandstone textures provide critical information for reservoir modeling and interpreting depositional processes. While loose sand textures are easy to describe, various authors have developed thin-section and image-analysis techniques to characterize lithified deposits that were assumed impossible to disaggregate successfully. These methods are effective but tedious, and are generally not feasible for processing many samples. We present a new methodology for disaggregating quartz-dominated sandstones cemented by quartz overgrowths, with application to the Permian Coconino Sandstone of n
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Berthelon, Josselin, and William Sassi. "A discussion on the validation of structural interpretations based on the mechanics of sedimentary basins in the northwestern Mediterranean fold-and-thrust belts." Bulletin de la Société Géologique de France 187, no. 2 (2016): 83–104. http://dx.doi.org/10.2113/gssgfbull.187.2.83.

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Abstract Using the geologist’s interpretation of 6 published balanced cross-sections in the fold and thrust belts of the northwestern Mediterranean, a comparative analysis of the interpreted subsurface structural architecture is used to address the links between the structural style and the mechanics of fold and thrust emplacement. For each cross-section example, the geo-dataset and the methods used by the interpreters are different in quantity and quality. Here we have examined how useful is the content of information of each cross-section to constrain the structural evolution scenario. Each
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BURLEY, S. D., and J. D. KANTOROWICZ. "Thin section and S.E.M. textural criteria for the recognition of cement‐dissolution porosity in sandstones." Sedimentology 33, no. 4 (1986): 587–604. http://dx.doi.org/10.1111/j.1365-3091.1986.tb00763.x.

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Dissertations / Theses on the topic "Thin section (Geology)"

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Meyer, Petrus C. "Feasibility of thin seam coal mining at Dorstfontein Coal Mine." Pretoria : [s.n.], 2003. http://upetd.up.ac.za/thesis/available/etd-09072005-113231/.

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Meyer, Petrus Cornelius. "Feasibility of thin seam coal mining at Dorstfontein Coal Mine." Diss., University of Pretoria, 2003. http://hdl.handle.net/2263/27806.

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Miller, Steven B. "Application of complex trace attributes to reflection seismic data near Charleston, South Carolina." Thesis, Virginia Polytechnic Institute and State University, 1985. http://hdl.handle.net/10919/50058.

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Complex trace attribute analysis has been applied to 24-fold VIBROSEIS reflection data acquired on the Atlantic Coastal Plain near Charleston, S. C., to yield an expanded interpretation of a Mesozoic basin concealed beneath Coastal Plain sediments. Complex trace attributes express the seismic trace in terms of a complex variable and emphasize different components of the original seismogram. Attributes derived from synthetic seismograms of thin beds are used to interpret the patterns observed on the real data. Complex trace attributes derived from the original seismic trace complement the inter
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Grabow, Gerd. "Zum 175. Geburtstag Alfred Wilhelm Stelzners, eines verdienstvollen Wissenschaftlers auf dem Gebiet der Geologie und der Lagerstättenlehre." Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2016. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-210763.

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Grabow, Gerd. "Zum 175. Geburtstag Alfred Wilhelm Stelzners, eines verdienstvollen Wissenschaftlers auf dem Gebiet der Geologie und der Lagerstättenlehre." ACAMONTA 22(2015), 2015. https://tubaf.qucosa.de/id/qucosa%3A23082.

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Mouland, Darrell. "Semi-automated characterization of thin-section petrographic images /." 2005.

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Books on the topic "Thin section (Geology)"

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Dexter, Perkins. Minerals in thin section. Prentice Hall, 2000.

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R, Henke Kevin, ed. Minerals in thin section. 2nd ed. Prentice Hall, 2004.

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Rock forming minerals in thin section. Chapman & Hall, 1997.

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C, Guilford, ed. Atlas of rock-forming minerals in thin section. Longman, 1986.

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Lauretta, D. S. A color atlas of meteorites in thin section. Golden Retriever Publications, 2005.

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MacKenzie, W. S. A color atlas of rocks and minerals in thin section. Halsted Press, 1994.

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1946-, Vaughan David J., ed. Ore microscopy and ore petrography. 2nd ed. Wiley, 1994.

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1946-, Vaughan David J., ed. Ore microscopy and ore petrography. 2nd ed. Wiley, 1994.

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The preparation of thin sections of rocks, minerals, and ceramics. Oxford University Press, 1992.

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Atlas of selected oil and gas reservoir rocks from North America: A color guidebook to the petrology of selected oil and gas reservoir rocks from the United States and Canada. Wiley, 1986.

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Book chapters on the topic "Thin section (Geology)"

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Cremer, Michel, Laurence Droz, William R. Normark, et al. "Thin-Section Studies, Mississippi Fan." In Frontiers in Sedimentary Geology. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5114-9_45.

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Přikryl, Richard. "Fluorescent Microscopy of Stained Thin Sections: A Direct Tool for the Evaluation of Pore Space Characteristics in Porous Rocks." In Engineering Geology for Society and Territory - Volume 8. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09408-3_96.

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Wright, D., D. Stanley, H. C. Chen, A. W. Shultz, and J. H. Fang. "A Frame-Based Expert System to Identify Minerals in Thin Section." In Microcomputer Applications in Geology 2. Elsevier, 1990. http://dx.doi.org/10.1016/b978-0-08-040261-1.50030-1.

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Speed*, Robert C., and Hai Cheng†. "Geology of southeastern Barbados." In Emergence and Evolution of Barbados. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2549(03).

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ABSTRACT This chapter presents geological documentation of Quaternary (and perhaps older) event histories of southeastern Barbados. The Barbados Limestone is herein formally defined. A time-stratigraphic division of the Barbados Limestone in southeastern Barbados and the properties of the stratigraphic units are presented. A major finding of this study is that the marine terraces originated wholly by marine erosion, not by reef construction, and evolved in stages over a long duration. The hydrology and thickness data of the Barbados Limestone are discussed, and hypotheses on causes of thickness variations are given. The study domain is divided into seven areas that contain a continuous flight of nine marine terraces preserved in various partial sequences. Discussions of these key seven areas in southeastern Barbados are supported by geologic maps at large scale and cross sections. Sections with VE > 1 display limestone stratigraphy and facies over relatively large lengths. Sections with VE = 1 show true structural configurations over short lengths. Detailed observations and radio isotopic dating of the limestone units permit differentiation and correlation among them.
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Furbish, David Jon. "Appendixes." In Fluid Physics in Geology. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195077018.003.0021.

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Definitions and formulae used at various points in the text to manipulate vectors are listed below. Additional useful formulae, including geometrical and physical interpretations complementary to those provided in this text, can be found in standard texts on vector analysis and in mathematical handbooks. The Standard Mathematical Tables published by CRC Press (Boca Raton, Florida) is a particularly handy resource, and most college-level calculus texts cover introductory vector analysis as part of the material intended for a third-semester course. Appendix A in Bird, Stewart, and Lightfoot (1960) is a very good summary of vector and tensor notation presented in the context of fluid mechanics. Section 17.1.1 begins with several basic definitions of vector quantities that generally apply to any orthogonal coordinate system. The notation for unit vectors in Cartesian coordinates, i, j, and k, are used in this section, but it is understood that this notation may be directly replaced with symbols for unit vectors associated with other orthogonal coordinates. Section 17.1.2 then covers differential operations for Cartesian coordinates. Although the notation used for these differential operations in Cartesian coordinates is the same as that for other coordinate systems, the actual operations connoted by the notation are different, and must be defined separately (Appendix 17.2). Let S and T denote scalar functions, and let U, V, and W denote vectors. If U = 〈U1, U2, U3〉, then . . . U = U1i + U2j + U3k . . . . . . (17.1) . . .
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Maltman, Alex. "Epilogue." In Vineyards, Rocks, and Soils. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190863289.003.0017.

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We have seen in previous chapters how grapevines interact with rocks and soils, and in Chapter 10 I discussed the role of geology in terroir. But a question remains, one that is probably uppermost in the mind of many a wine lover: to what extent does geology affect the taste of the wine in your glass? I argued in Chapter 9 that the perception of a mineral taste in wine can’t have a literal meaning, but what about other tastes ascribed to geology? We might reasonably expect that the geological influences on vine growth have at least some role in wine flavor, but what? Many populist wine writings imply that the answers to such questions are clear-cut, but unfortunately they aren’t. Claims are routinely made in wine descriptions that sound fine but that don’t easily tally with scientific understanding. In other words, there’s some divergence between popular beliefs and scientific understanding of the geology—wine flavor connection. Part of the explanation may be that many of the populist assertions seem to be based on custom and on anecdote—narratives passed on enthusiastically but unquestioningly between wine fans. Two situations are common. First, a description of a wine casually mentions the kind of geology where it originated, implying a significance but without any justification or indication of how it might come about. I give illustrations of this in the following section. Second, some character of a wine is ascribed to particular rocks and soils but without providing any rationale. For example, a Riesling from Kamptal’s Gaisberg vineyard (Austria) is said to have “complexity because of the slaty para-gneiss, amphibolite, and mica” soils. But there’s no indication of how these two very specific rock types together with this particular mineral bring this complexity about.
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Cevikbilen, Gokhan. "Slope Stability of Soils." In Advances in Civil and Industrial Engineering. IGI Global, 2018. http://dx.doi.org/10.4018/978-1-5225-2709-1.ch011.

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Slope stability problems in soils underlie most of the landslides that cause losses of human and property in the world. The stability of natural or man-made slopes in soils is an important topic that requires great attention while site exploring, testing, modelling and analyzing. Engineering geology and geotechnical engineering interdisciplinary team work is essential to achieve a sufficient understanding of site geology and the behavior of soil. The developments of urban areas require new sites for settlement. Soil structure interaction in slopes requires more sophisticated numerical analysis methods to develop. This section particularly summarizes the factors cause a slope to fail. In addition, site exploration steps, in-situ and laboratory test methods were mentioned. Slope stability analysis methods such as LEM, FEM, DEM, BEM were discussed in details. The developments of empirical or statistical regional approaches were stated. Remediation techniques were discussed regarding the construction costs. Finally, the necessity of further studies in numerical modelling was emphasized.
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Medwedeff, Donald A. "Interaction of extensional, contractional, and strike-slip elements at Mount Diablo and the surrounding eastern Coast Ranges, San Francisco Bay area, California: A model-based analysis." In Regional Geology of Mount Diablo, California: Its Tectonic Evolution on the North America Plate Boundary. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.1217(08).

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ABSTRACT This study presents three regional cross sections, a structural map analysis, and a schematic map restoration. The sections are constrained by surface geology and petroleum wells and were developed using model-based methods to be consistent with the regional tectonic context and balancing concepts. Together, these products depict the geometry and kinematics of the major fault systems. Insights from this research include the following. Franciscan complex blueschist-facies rocks in the Mount Diablo region were unroofed west of their current location and subsequently thrust beneath the Great Valley sequence in the mid-Eocene. East Bay structures are complicated by overprinting of Neogene compression and dextral strike-slip motion on a Paleogene graben system. Net lateral displacement between the Hayward fault and the Central Valley varies from 26 km toward 341° to 29 km toward 010° in the southern and northern East Bay Hills, respectively. Uplift above a wedge thrust generates the principal Neogene structural high, which extends from Vallejo through Mount Diablo to the Altamont Ridge. Anomalous structural relief at Mount Diablo is due to strike-parallel thrusting on the crest of a fault-propagation fold formed on the west-verging roof thrust. Uplift that exposes the Coast Range ophiolite in the East Bay Hills is formed by oblique thrusting generated by slip transfer at the northern termination of the Calaveras fault. The Paleogene extensional fault system likely extends farther west than previously documented. An east-dipping branch of that system may underlie the Walnut Creek Valley. Three-dimensional restoration should be applied to constrain geologic frameworks to be used for seismic velocity modeling.
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"Benthic Habitats and the Effects of Fishing." In Benthic Habitats and the Effects of Fishing, edited by Peter W. Barnes, Guy W. Fleischer, James V. Gardner, and Kristen M. Lee. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569605.ch15.

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<strong><em>Abstract. </em></strong>As part of a strategy to reestablish native stocks of lake trout <em>Salvelinus namaycush</em>, six areas of offshore and coastal Lake Michigan benthic habitat were mapped with a bathymetric laser system. This allowed us to visualize and map morphologic detail by at least an order of magnitude over existing data. Decimeter elevation–bathymetric data, referenced to the International Great Lakes datum of 1985, were obtained on a 4-m grid over a total area of about 200 km<sup>2</sup> in water depths from 0 to 30 m. Based on the laser-derived morphology, regional geology and sparse samples, three geologic regimes were used for substrate–habitat classification: (1) bedrock carbonates of Silurian through Devonian age, indicated by bedding scarps and lineations at or near the surface at all of the mapped areas; (2) glacial deposits that appear as compacted clay till lineations and cobble and boulder moraines with outwash features; and (3) modern sand deposits seen in thin down-drift (to the east) bedforms, sand sheets, and depositional lobes. Preferred spawning substrate—clean cobble and gravel deposits with adjacent deep water—is present in sections of all mapped areas. However, laser data cannot discern cleanliness, and video data indicate the cleanliness on this substrate may be compromised by recent algal and mussel growth.
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Gill, D., and M. Levinger. "Information Management And Mapping System For Subsurface Stratigraphic Analysis." In Computers in Geology - 25 Years of Progress. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195085938.003.0014.

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An information management and mapping system combining a series of interactive computer programs for stratigraphic, lithofacies, paleogeographic, and structural analysis interfaced with a comprehensive database on subsurface geology produces contour maps of quantitative variables including structure maps, isopach maps, and maps of lithofacies parameters; detailed lithologic and stratigraphic logs; and printouts of lithofacies parameters for all levels of the lithostratigraphic subdivision. Users communicate by means of simple, on-screen, menu-driven dialogues controlled by FORTRAN programs. The system runs on DEC/Micro VAX II computers operating under VMS. This information management and mapping system for subsurface stratigraphic analysis is an integration of a comprehensive database on the subsurface geology of Israel and a series of computer programs for stratigraphic, lithofacies, paleogeographic, and structural analysis. Development of the system, referred to as "ATLAS -RELIANT," was sponsored by OEIL [Israel Oil Exploration (Investment) Ltd.). The system serves primarily as a storage and retrieval facility for information on the subsurface geology of Israel. Users can obtain printouts of lithologic and stratigraphic logs, contour maps, and value maps. The system originally was developed to run on a CDC machine under the NOS/BE operating system. Later OEIL expanded the database to include many additional items of information [inventory of cores and petrophysical logs, results of production tests, results of petrophysical analyses, geochemical analyses of recovered fluids (water samples and hydrocarbons), and results of quantitative analyses of petrophysical logs] and the system was modified to run on DEC/Micro VAX II computers under the VMS operating system (Shertok, 1969). Among other things, the ATLAS-RELIANT system was instrumental in the regional stratigraphic analysis of the subsurface geology of Israel performed by OEIL during 1968-1988 (OEIL, 1966; Cohen et al., 1990). The database, dubbed "ATLAS," is about 16 MB in size and contains information on 320 petroleum exploration and development boreholes, 50 deep water wells, and 100 columnar sections of outcrops.
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Conference papers on the topic "Thin section (Geology)"

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Kath, Randy, and Robert Henthorne. "GEOLOGIC LICENSURE: HOW THIS WILL IMPACT YOUR CAREER IN GEOSCIENCES." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-291698.

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Taylor, Kenneth B. "DETAILED GEOLOGIC MAPPING LEGACY OF DR. ROBERT D. HATCHER, JR. AND HIS STUDENTS: 50-YEARS OF GEOLOGIC MAPPING, ONE OUTCROP AT A TIME WITH MORE THAN 51 MASTER’S THESES AND MORE THAN 17 PH.D. DISSERTATIONS." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-313132.

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Wolak, Jeannette. "OUT OF THIS WORLD INQUIRY: TEACHING PLANETARY GEOLOGIC PROCESSES USING TERRESTRIAL ANALOGS." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344882.

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Manda, Alex K. "QUANTITATIVELY ASSESSING THE INFLUENCE OF THE ‘THINK-PAIR-SHARE’ ACTIVE LEARNING PEDAGOGICAL APPROACH ON CONTENT KNOWLEDGE AND SELF-CONFIDENCE OF STUDENTS IN AN INTRODUCTORY LEVEL GEOLOGY COURSE." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290398.

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Yu, Jingfeng, Diao Zhou, Bo Zhang, et al. "Horizontal Well Drilling and Geosteering Optimization with Integrated Innovation Technologies: Case Studies from the World Largest Conglomerate Reservoir in West China." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21482-ms.

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Abstract MH oilfield is a fan delta deposited unconventional tight oil reservoir with complex lithology of volcanic rocks, metamorphic rocks, conglomerate, and claystone. The drilling efficiency was optimized by using the first-generation boundary mapping technology with Rotary Steering System (RSS) during the first batch drilling campaign (H2-2016∼H1-2017), which was mentioned in IADC/SPE-190998-MS. But with the development going further, more and more wells drilled into shale interbed causing low pay zone exposure, long drilling duration, and numerous drilling hazards. The overall drilling p
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Granath, James, Rolf Rango, Pete Emmet, Colin Ford, Robert Lambert, and Michael Kasli. "New Viewpoint on the Geology and Hydrocarbon Prospectivity of the Seychelles Plateau." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2556681-ms.

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ABSTRACT We have reprocessed, re-imaged, and interpreted 10000+ km of legacy 2D seismic data in the Seychelles, particularly in the western part of the Plateau. Seychelles data have been difficult to image, particularly for the Mesozoic section: volcanics are a major attenuator of low frequency signal, and a hard water bottom contributes to signal problems. Enhanced low frequency techniques were applied to improve the signal fidelity in the 4 to 20 Hz range, and to remove spectral notches of shallow geologic origin. These efforts have allowed a reasonable view of the structure of the Plateau t
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Wu, Cailan, Weixiao Cui, Chengzhi Zhang, Huaijian Li, and Hongliang Yan. "Design and Construction Technologies." In 2010 Joint Rail Conference. ASMEDC, 2010. http://dx.doi.org/10.1115/jrc2010-36217.

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Combining with the actual situation of China’s railway construction, this paper introduces the key technologies of design and construction of high-speed railway, such as the scheme optimization of subgrade, bridge and tunnel, technical standard, deformation control, advance geology forecast and settlement observation, etc. It also discusses the design and construction problems on the slab layout and interface of CRTS II slab track on bridge section, switch area, subgrade area and the transition with different track structures.
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Espinola Gonzalez, Oswaldo, Laura Paola Vazquez Macedo, Julio Cesar Villanueva Alonso, and Julieta Alvarez Martinez. "Novel Approach to Enhance Field Development Plan Process and Reservoir Management to Maximize the Recovery Factor of Gas Condensate Reservoirs Through Integrated Asset Modeling." In SPE Trinidad and Tobago Section Energy Resources Conference. SPE, 2021. http://dx.doi.org/10.2118/200895-ms.

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Abstract The proper exploitation for a gas condensate reservoir requires an integrated collaboration and management strategy capable to provide detailed insight about future behavior of the reservoir. When a development plan is generated for a field, the reservoir management is not performed integrally, this is, different domains: geology, reservoir, drilling, production, economics, etc., work separately, and therefore, an adequate understanding of the main challenges, leading to issues such as an over dimensioning of surface facilities, excessive costs, among others. Through this paper, a met
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Jones, S. C., and L. E. Sobers. "Comparison of the Impact of Dip and Vertical Transmissibility on Oil Recovery and Carbon Storage Using Water over Gas Injection in the Forest Reserve Field, Trinidad." In SPE Energy Resources Conference. SPE, 2014. http://dx.doi.org/10.2118/spe-169961-ms.

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Abstract A combination of geologic carbon dioxide (CO2) sequestration and CO2 enhanced oil recovery (CO2EOR) can address the two of Trinidad and Tobago's energy sector challenges: falling oil production and increasing CO2 emissions. Geologic storage of CO2 in heavy oil reservoirs can increase oil production while injected CO2 is effectively sequestered. Our investigations are based on 225 ft (~69 m) of the unconsolidated Lower Forest sand, average porosity and permeability of 32% and 125 md, respectively, found within the Forest reserve field, Trinidad. The middle section of this sand package
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Daramola, Babalola. "Maximising Infill Well Oil Recovery with 4D Seismic and Reservoir Simulation." In SPE Trinidad and Tobago Section Energy Resources Conference. SPE, 2021. http://dx.doi.org/10.2118/200969-ms.

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Abstract This publication presents how 4D seismic and reservoir simulation techniques were used to optimise the trajectory of an infill production well in a producing oil field. The A6 infill well target in Field X offshore Nigeria was planned as a 12000 feet horizontal drill well with a 4900 feet gravel pack completion in the reservoir formation. The initial well trajectory delivered early water breakthrough and low oil recovery. The well planning team resolved the issue by reconciling the well trajectory and completion data in the geologic and reservoir simulation models, and used 4D seismic
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Reports on the topic "Thin section (Geology)"

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Henderson, Tim, Mincent Santucci, Tim Connors, and Justin Tweet. National Park Service geologic type section inventory: Chihuahuan Desert Inventory & Monitoring Network. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2285306.

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Abstract:
A fundamental responsibility of the National Park Service is to ensure that park resources are preserved, protected, and managed in consideration of the resources themselves and for the benefit and enjoyment by the public. Through the inventory, monitoring, and study of park resources, we gain a greater understanding of the scope, significance, distribution, and management issues associated with these resources and their use. This baseline of natural resource information is available to inform park managers, scientists, stakeholders, and the public about the conditions of these resources and t
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2

Henderson, Tim, Vincent Santucci, Tim Connors, and Justin Tweet. National Park Service geologic type section inventory: Northern Colorado Plateau Inventory & Monitoring Network. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2285337.

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Abstract:
A fundamental responsibility of the National Park Service (NPS) is to ensure that park resources are preserved, protected, and managed in consideration of the resources themselves and for the benefit and enjoyment by the public. Through the inventory, monitoring, and study of park resources, we gain a greater understanding of the scope, significance, distribution, and management issues associated with these resources and their use. This baseline of natural resource information is available to inform park managers, scientists, stakeholders, and the public about the conditions of these resources
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3

Henderson, Tim, Vincent Santucci, Tim Connors, and Justin Tweet. National Park Service geologic type section inventory: Klamath Inventory & Monitoring Network. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2286915.

Full text
Abstract:
A fundamental responsibility of the National Park Service (NPS) is to ensure that park resources are preserved, protected, and managed in consideration of the resources themselves and for the benefit and enjoyment by the public. Through the inventory, monitoring, and study of park resources, we gain a greater understanding of the scope, significance, distribution, and management issues associated with these resources and their use. This baseline of natural resource information is available to inform park managers, scientists, stakeholders, and the public about the conditions of these resources
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4

Nelson, Margot, Michael Antonioni, Vincent Santucci, and Justin Tweet. Oxon Run Parkway: Paleontological resource inventory; supplement to the National Capital Parks-East paleontological resource inventory. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2287217.

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Abstract:
Oxon Run Parkway (OXRN) is a 51-hectare (126-acre) natural area within Washington, D.C. administered by the National Park Service under National Capital Parks East (NACE). The original plan called for a road, slated to follow Oxon Run stream, but this never came to fruition; despite this, the moniker stuck. The majority of the original Oxon Run Parkway is managed by the District of Columbia. The section of Oxon Run Parkway under NPS jurisdiction contains wetlands and forests, as well as the only McAteean magnolia bogs still remaining in the District. The lower Cretaceous Potomac Group, known a
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