Relevant bibliographies by topics / Mapping geologic

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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 'Mapping geologic'

Author: Grafiati
Published: 4 June 2021
Last updated: 7 February 2022

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Journal articles on the topic "Mapping geologic"

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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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Saini-Eidukat, Bernhardt, Donald P. Schwert, and Brian M. Slator. "Geology explorer: virtual geologic mapping and interpretation." Computers & Geosciences 28, no. 10 (December 2002): 1167–76. http://dx.doi.org/10.1016/s0098-3004(02)00036-5.

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Yingst, R. A., S. C. Mest, D. C. Berman, W. B. Garry, D. A. Williams, D. Buczkowski, R. Jaumann, et al. "Geologic mapping of Vesta." Planetary and Space Science 103 (November 2014): 2–23. http://dx.doi.org/10.1016/j.pss.2013.12.014.

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Greeley, Ronald, Patricio H. Figueredo, David A. Williams, Frank C. Chuang, James E. Klemaszewski, Steven D. Kadel, Louise M. Prockter, et al. "Geologic mapping of Europa." Journal of Geophysical Research: Planets 105, E9 (September 1, 2000): 22559–78. http://dx.doi.org/10.1029/1999je001173.

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Bush, S. "Geologic mapping act supported." Eos, Transactions American Geophysical Union 72, no. 33 (1991): 347. http://dx.doi.org/10.1029/90eo00266.

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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 (May 1996): 253–58. http://dx.doi.org/10.5408/1089-9995-44.3.253.

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Gulbrandsen, Mats Lundh, Lyndsay B. Ball, Burke J. Minsley, and Thomas Mejer Hansen. "Automatic mapping of the base of aquifer — A case study from Morrill, Nebraska." Interpretation 5, no. 2 (May 31, 2017): T231—T241. http://dx.doi.org/10.1190/int-2016-0195.1.

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When a geologist sets up a geologic model, various types of disparate information may be available, such as exposures, boreholes, and (or) geophysical data. In recent years, the amount of geophysical data available has been increasing, a trend that is only expected to continue. It is nontrivial (and often, in practice, impossible) for the geologist to take all the details of the geophysical data into account when setting up a geologic model. We have developed an approach that allows for the objective quantification of information from geophysical data and borehole observations in a way that is easy to integrate in the geologic modeling process. This will allow the geologist to make a geologic interpretation that is consistent with the geophysical information at hand. We have determined that automated interpretation of geologic layer boundaries using information from boreholes and geophysical data alone can provide a good geologic layer model, even before manual interpretation has begun. The workflow is implemented on a set of boreholes and airborne electromagnetic (AEM) data from Morrill, Nebraska. From the borehole logs, information about the depth to the base of aquifer (BOA) is extracted and used together with the AEM data to map a surface that represents this geologic contact. Finally, a comparison between our automated approach and a previous manual mapping of the BOA in the region validates the quality of the proposed method and suggests that this workflow will allow a much faster and objective geologic modeling process that is consistent with the available data.
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Bailey, Christopher McNeill. "An Integrative Geologic Mapping Project for Structural-Geology Courses." Journal of Geoscience Education 46, no. 3 (May 1998): 245–51. http://dx.doi.org/10.5408/1089-9995-46.3.245.

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Hansen, V. "Geologic mapping of tectonic planets." Earth and Planetary Science Letters 176, no. 3-4 (March 30, 2000): 527–42. http://dx.doi.org/10.1016/s0012-821x(00)00017-0.

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Lisle, R. J., P. Brabham, and J. Barnes. "Basic Geologic Mapping, Fifth Edition." Environmental & Engineering Geoscience 19, no. 2 (May 1, 2013): 196–98. http://dx.doi.org/10.2113/gseegeosci.19.2.196.

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Dissertations / Theses on the topic "Mapping geologic"

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Jenett, Tilmann [Verfasser]. "Modern geologic mapping : The conceptual development and practical review of a digital geologic mapping approach / Tilmann Jenett." Berlin : Freie Universität Berlin, 2012. http://d-nb.info/1031421319/34.

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Decker, Megan Carolee. "Paterae on Io: Geologic Mapping of Tupan Patera and Experimental Models." BYU ScholarsArchive, 2014. https://scholarsarchive.byu.edu/etd/5306.

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Paterae cover approximately 2% of the surface of Io, Jupiter’s volcanically active moon. To understand the formation of these volcano-tectonic depressions we created a geologic map of a key region and compared this map with experimental models for Io paterae. Our mapping region is Tupan Patera, a patera that has experienced recent activity and is a detected hot spot. We identified four primary types of geologic materials: plains, patera floors, flows, and diffuse deposits. We constructed an experimental model to test previous suggestions that paterae may form as volatiles in the silicate crust are vaporized by rising magma, creating instability, and subsequent collapse. The apparatus is a scaled model that uses sand (silicate crust analog), ice or snow (volatile analog), a hotplate (magma chamber analog), and a moveable paddle (to simulate extension). Our experimental collapse features exhibit many characteristics of paterae on Io, such as “islands,” terraces, straight margins, and steep scarps. Our model suggests that the role of volatiles in Io’s crust is a significant part of paterae formation.Comparative studies between our map and model show it is possible Tupan is an emerging lava lake or one in a state of quiescence. Our studies have also culminated in the completion of a theoretical cross section for the geologic history of Tupan Patera. This cross section displays a sequence of events including the rise of magma as it preferentially volatilizes sulfurous layers in the crust, subsequent thinning, instability, and collapse, the likelihood of the patera floor sinking as a stoped block, and the more recent flow and diffuse deposits. This study gives some insight to the general formation of paterae on Io.
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Folfas, Andrew Paul. "Geologic Mapping of The Changgo Dome in Southern Tibet Using ASTER Imagery." Wright State University / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=wright1226357431.

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Poduska, Gabriel J. "Geologic Mapping of Ice Cave Peak Quadrangle, Uintah and Duchesne Counties, Utah with Implications from Mapping Laramide Faults." BYU ScholarsArchive, 2015. https://scholarsarchive.byu.edu/etd/5777.

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Geologic mapping (1:24,000 scale) of the Ice Cave Peak quadrangle, Uintah and Duchesne Counties, Utah has produced a better understanding of the geologic structures present in the quadrangle and has increased our understanding of faulting in northeastern Utah. Map units in the quadrangle range in age from late Neoproterozoic to Quaternary and include good exposures of Paleozoic rocks (Mississippian to Permian), limited exposures of Mesozoic rocks, and good exposures of Tertiary strata (Duchesne River Formation and Bishop Conglomerate) deposited during uplift of the Uinta Mountains. Lower Mississippian strata along the south flank of the Uinta Mountains have typically been mapped as Madison Limestone. Our preliminary mapping suggested that the Madison could perhaps be subdivided into an upper unit equivalent to the Deseret Limestone, and a lower unit separated by a phosphatic interval equivalent to the Delle Phosphatic Member of the Deseret Limestone found farther west. Upon further investigation, we propose not extending the use of Deseret Limestone, with the equivalent to the Delle Phosphatic Member at its base, into the south-central Uinta Mountains. Microprobe analysis revealed no phosphorus in thin sections of this unit. Instead, the unit is composed almost entirely of calcite and dolomite. A zone of northwest-trending faults, called the Deep Creek fault zone, occurs mainly east of the Ice Cave Peak quadrangle. However, our mapping shows that this fault zone extends into the quadrangle. These faults are both strike-slip and normal/oblique faults as documented by mapping and kinematic indicators and cut the folded hanging-wall sedimentary rocks above the Uinta Basin-Mountain boundary thrust fault. These faults may be part of an en echelon fault system that is rooted in the Neoproterozoic and reactivated during Laramide deformation above a possible transfer zone between segments of the buried boundary thrust.
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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 and thick Quaternary deposits unrelated to Pleistocene glaciation, burying drainages, and mantling hillslopes. The influence of bedrock on groundwater flow paths and stream baseflow is suggested by local anecdotal reports that high snowfall in the Deseret Peak region generates high discharge ten miles south in Clover Creek, though they are not in the same drainage basin.
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Patch, Nickolas Lee. "Geology of the Dyer Mountain quadrangle, Utah." Thesis, Manhattan, Kan. : Kansas State University, 2009. http://hdl.handle.net/2097/1452.

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Martin, Daniel Holt. "Geologic map of the Golden Throne Quadrangle, Wayne and Garfield Counties, Utah /." Diss., CLICK HERE for online access, 2005. http://contentdm.lib.byu.edu/ETD/image/etd1011.pdf.

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Driscoll, Nicholaus D. "Geologic Map of the Deer Point Quadrangle, Garfield County, Utah." BYU ScholarsArchive, 2012. https://scholarsarchive.byu.edu/etd/3276.

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A new geologic map of the Deer Point 7.5' quadrangle located in the southern region of Capitol Reef National Park in south-central Utah provides stratigraphic and structural detail not previously available. The Deer Point quadrangle was mapped at a scale of 1:24,000 and is the fourth geologic map completed at this scale in Capitol Reef National Park. Twelve Quaternary units and eighteen bedrock formations and members are exposed in the Deer Point quadrangle. Bedrock formations range in age from Triassic to Cretaceous. The details not available on previous geologic maps include: four alluvial terrace units, two lacustrine units, two mass movement units, and members of the Moenkopi, Chinle, and Carmel Formations. Historically the Page Sandstone has been mapped as part of the Navajo Sandstone or the Carmel Formation. This map identifies the Page Sandstone as a separate and independent unit. The Deer Point quadrangle is cross cut by a portion of a Laramide-age, basement cored, NNW-SSE trending asymmetrical anticline called the Waterpocket Fold. Strikes and dips measured throughout the Deer Point quadrangle identify the vergence of the anticline as eastward with a maximum dip of 49˚ on the forelimb and 7˚ on the backlimb. The maximum dip on the forelimb dramatically decreases in the southern quarter of the quadrangle to 15˚.The Utah Geological Survey is mapping the Hite Crossing 30' x 60' quadrangle at a scale of 1:62.500. The Deer Point quadrangle is one of 32 quadrangles that comprise the Hite Crossing quadrangle. The Utah Geological Survey is working to establish erosion rates on the Colorado Plateau. To do this, they are dating alluvial terrace deposits. Within the Deer Point quadrangle four new terrace levels have been identified that could help with this research. Additional research could use these terrace deposits to better understand erosion rates in the Deer Point quadrangle and the broader Colorado Plateau. Numerous mass movement deposits are found within the Deer Point quadrangle. The largest has been named the Red Slide. Several aspects of the Red Slide are identified including classification, breakaway zone, source, deposit size, composition, debris flow path and depositional history. The Red Slide has been classified as a debris flow. The breakaway zone is a concave cliff 1.5 miles (2.4 km) to the west of the debris flow's present location. The flow's scarp is no longer identifiable. The source of the debris flow material is the Chinle Formation and Wingate Sandstone. The Red Slide deposit covers an area of over 16.6 million ft2 (~1.5 million m2). The toe of the debris flow is 1 mile (1.6 km) wide. The estimated maximum thickness of the debris flow is sixty meters. The Red Slide is composed of fine-grained, clay- and silt- sized material, and a small amount of angular pebble- to cobble-sized limestone clasts from the Owl Rock Member of the Chinle Formation. Boulder- to sand-sized grains from the Wingate Sandstone are scattered throughout the deposit with the larger grains forming inversely grading packages. The Red Slide likely occurred as a series of large debris flows, not one catastrophic event, although they may have occurred at about the same time.
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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. Thermobarometric calculations made during this study demonstrate that both P and T increase eastward across the entire region and are not symmetrically distributed about dome axes. The P-T data coupled with petrographically derived relative age relationships and available geochronology also suggest that attainment of peak metamorphic conditions and concurrent dome-stage deformation are diachronous and young from west to east. These relationships are consistent with new geologic mapping and structural analysis which show that all of the domes in southern Vermont are low-amplitude fold interference structures. A current tectonic model indicates that Acadian Barrovian metamorphism in this region was a consequence of west-directed crustal thickening of an eastward dipping tectonic wedge, presumably from the Bronson Hill Terrane; an Ordovician arc sequence. The basal surface of this allochthonous mass projects above the present land surface within this area. Accretion of lower-plate rocks (of this study) into the thrust complex and continued west-directed thrusting of the accreted package over a seismically recognizable east dipping ramp structure provided the necessary geometry and mechanism for dome-stage fabric development, calculated uplift rates (1.2 to 1.7 km/m.y. and west to east younging of Acadian structural and metamorphic evolution. Thermobarometric and geochronologic estimates of metamorphic pressure - temperature (P-T) conditions and metamorphic cooling ages were used to constrain the required thermal and tectonic input parameters for use in one-dimensional thermal modeling of an Acadian (Silurian-Devonian} tectonotherma! regime within the pre-Silurian Taconide zone of southern Vermont. This regime includes: 1) garnet-grade rocks from the eastern flank of an Acadian composite dome structure (Sadawga Dome; the western domain); 2) staurolite/kyanite-grade rocks from the western flank of a second composite structure, the Athens dome (eastern domain). Results from thermal modeling include development of P-T paths, temperature-time (T-t) and pressure-time (P-t) curves, related values of maximum temperature and pressure, pressure conditions at maximum temperature, predicted closure ages for radiogenic phases, and integrated uplift and cooling rates. Thermal modeling results are remarkably similar to independently obtained data for Acadian regional metamorphism in western New England, and provide some important constraints on regional thermal evolution: 1) pressure values contemporaneous with peak temperature on P-T paths may be substantially lower than actual maximum pressure (> 2.5 kbars); 2) differences in peak temperature for rocks initially loaded to similar crustal depths (garnetgrade vs. staurolite-grade), differences in calculated uplift rates, and differences in Ar closure ages, are consequences of variations in durations of isobaric heating events (or "residence periods"), and differences in actual tectonic uplift rates. These modeling results are internally consistent with structural model that suggests west to east younging of specific Acadian deformations and resultant diachroneity of peak metamorphic and Ar closure ages. Regional variations in timing and conditions of metamorphism may be controlled by diachronous deformational events coupled with variations in crustal levels to which rocks were initially loaded during the ca. 400 Ma onset of Acadian orogenesis in western New England.
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Summa, Michelle Carlene. "Geologic Mapping, Alluvial Stratigraphy, and Optically Stimulated Luminescence Dating of the Kanab Creek Area, Southern Utah." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/506.

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At the turn of the century, Kanab Creek incised 30-meters into its alluvium, leaving behind fluvial terraces and thick basin fill sediments exposed along arroyo walls. Research objectives were to determine the timing and causes of past valley-filling and arroyo-cutting episodes along a 20 km-long reach of Kanab Creek in southern Utah. Fluvial deposits were mapped at the 1:12,000 scale and sediments were described and dated using Optically Stimulated Luminescence (OSL) and radiocarbon dating. The Kanab Creek valley can be divided into a narrow, upper terraced reach and a broad lower basin fill reach near Kanab, Utah. The most prominent terrace in the upper reach is Quaternary alluvial terrace 4 (Qat4), followed by Qat3, Qat2/3, and Qat2 map units. These are composed of tabular-bedded, fine-grained sand, silt, and clay layers. The Qat2/3 map unit is a both a fill and fill-cut terrace underlain by Qa4, Qa3, and Qa2 alluvium and is used when the Qat3 fill-cut (fill-strath) terrace can not be differentiated from the Qat2 fill terrace due to their similar geomorphic position. The Qat3 fill-cut terrace upstream correlates to ~8 meters of aggradation downstream. The youngest terrace, Qat1, is a minor terrace, composed of coarse-grained channel facies. More recent channel and floodplain deposits were deposited over the last century following arroyo cutting. OSL and radiocarbon results suggest at least four cycles of fluvial cutting and filling: >6-3.5ka (Qa4), ~3->1ka (Qa3), 0.7-0.12ka (Qa2), and post-1880 AD (Qa1). Correlation to regional climate records suggests major periods of aggradation correlate to regionally cooler and wetter climatic intervals. Periods of arroyo cutting occurred at >6ka, ~3ka, 1-0.7ka, and during historic arroyo cutting (1882-1914 AD), and correlate to regionally warmer, drier intervals. These periods of aggradation and incision are roughly contemporaneous with regional drainages, except for the large aggradation seen in Kanab Creek 6-3.5ka (Qa4). Analysis of terrace longitudinal profiles indicates Qat4 has the lowest concavity suggesting that Qat4 aggraded during a period of greater sediment supply and/or reduced flood regime. Although OSL samples exhibited some degree of incomplete zeroing, calculated ages using a minimum age model are consistent with radiocarbon results.
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Books on the topic "Mapping geologic"

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Förster, Andrea, and Daniel F. Merriam. Geologic Modeling and Mapping. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3.

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

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Harrison, Richard W. Midcontinent urban corridor geologic mapping project. [Washington, D.C.?]: U.S. Dept. of Interior, U.S. Geological Survey, 1997.

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Mapping, Illinois General Assembly Senate Working Committee on Geologic. Geologic mapping for the future of Illinois. Champaign, Ill: Illinois State Geological Survey, 1992.

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Survey, Illinois State Geological. Geologic mapping for the future of Illinois. Champaign, Ill. (615 E. Peabody Dr., Champaign 61820): Illinois State Geological Survey, 1992.

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US GOVERNMENT. National Geologic Mapping Reauthorization Act of 1999. [Washington, D.C: U.S. G.P.O., 1999.

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Thomas, William Andrew. Meeting challenges with geologic maps. Alexandria, Va: American Geological Institute, 2004.

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Morton, Douglas M. Geologic map of the Cucamonga Peak 7.5-minute quadrangle, San Bernardino County, California. Menlo Park, CA: U.S. Geological Survey, 1991.

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Bray, E. A. Du. Preliminary geologic map of Chiricahua National Monument, Cochise County, Arizona, with digital geologic map data. [Denver, CO]: U.S. Geological Survey, 1993.

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Galloway, John P. Status of geologic mapping in Alaska: Digital bibliography. [Menlo Park, CA]: U.S. Geological Survey, 1994.

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Book chapters on the topic "Mapping geologic"

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Hauber, Ernst, Andrea Naß, James A. Skinner, and Alexandra Huff. "Planetary Geologic Mapping." In Lecture Notes in Geoinformation and Cartography, 105–45. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-62849-3_5.

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Plansky, Lee, Keith Prisbey, Carl Glass, and Lee Barron. "An Intelligent Framework for Geologic Modeling Applications." In Geologic Modeling and Mapping, 301–22. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_15.

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Wendebourg, Johannes, and John W. Harbaugh. "Sedimentary Process Simulation: A New Approach for Describing Petrophysical Properties in Three Dimensions for Subsurface Flow Simulations." In Geologic Modeling and Mapping, 1–25. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_1.

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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, 199–214. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_10.

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Merriam, Daniel F., Ute C. Herzfeld, and Andrea Förster. "Pairwise Comparison of Spatial Map Data." In Geologic Modeling and Mapping, 215–28. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_11.

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Grunsky, E. C., Q. Cheng, and F. P. Agterberg. "Applications of Spatial Factor Analysis to Multivariate Geochemical Data." In Geologic Modeling and Mapping, 229–61. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_12.

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Harff, Jan, Ricardo A. Olea, John C. Davis, and Geoffrey C. Bohling. "Geostatistical Solution for the Classification Problem with an Application to Oil Prospecting." In Geologic Modeling and Mapping, 263–79. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_13.

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Luo, Junfeng. "Transition Probability Approach to Statistical Analysis of Spatial Qualitative Variables in Geology." In Geologic Modeling and Mapping, 281–99. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_14.

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Ondrak, Robert. "Modeling of Multicomponent Diagenetic Systems." In Geologic Modeling and Mapping, 27–41. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_2.

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Watney, W. Lynn, John A. French, and Willard J. Guy. "Modeling Petroleum Reservoirs in Pennsylvanian Strata of the MidContinent, USA." In Geologic Modeling and Mapping, 43–77. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4613-0363-3_3.

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Conference papers on the topic "Mapping geologic"

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Allmendinger, Richard W., and Paul Karabinos. "IMPROVING GEOLOGIC MAPPING WITH COMPUTATIONAL FIELD GEOLOGY." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334376.

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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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Tijerina, Geraldine, and Sarah N. Heinlein. "CONTEMPORARY TECHNIQUES IN GEOLOGIC MAPPING." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340615.

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Soller, David R., Nancy R. Stamm, Robert C. Wardwell, and Christopher P. Garrity. "THE NATIONAL GEOLOGIC MAP DATABASE -- A RESOURCE FOR GEOLOGIC MAPPING." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286795.

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Powell, Mark, Thomas Crockett, Khawaja Shams, and Jeffrey Norris. "Geologic Mapping in Mars Rover Operations." In SpaceOps 2010 Conference: Delivering on the Dream (Hosted by NASA Marshall Space Flight Center and Organized by AIAA). Reston, Virigina: American Institute of Aeronautics and Astronautics, 2010. http://dx.doi.org/10.2514/6.2010-1998.

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Collins, Edward W., Jeffrey G. Paine, Brent Elliott, C. M. Woodruff, and Lucie Costard. "STATEMAP PROGRAM GEOLOGIC MAPPING IN TEXAS." In 52nd Annual GSA South-Central Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018sc-309882.

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Child, Sarah F., John W. Dunham, and W. C. Johnson. "GEOLOGIC MAPPING OF RICE COUNTY, KANSAS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286776.

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Pitts, Alan, Giuseppina Kysar-Mattietti, Randolph A. McBride, Claudio Di Celma, and Emanuele Tondi. "GEOLOGY FIELD CAMP IN ITALY: A NEW INTERNATIONAL FIELD EXPERIENCE IN GEOLOGIC MAPPING AND GEOLOGIC HAZARDS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-308696.

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Wynn, Jeff, Sue Karl, Bruce Smith, and Anne McCafferty. "Developing Geophysical Signatures To Constrain Geologic Mapping." In 14th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.192.air_7.

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Wynn, Jeff, Sue Karl, Bruce Smith, and Anne McCafferty. "Developing Geophysical Signatures to Constrain Geologic Mapping." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2001. Environment and Engineering Geophysical Society, 2001. http://dx.doi.org/10.4133/1.2922849.

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Reports on the topic "Mapping geologic"

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Hess, R. H., G. L. Johnson, and C. M. dePolo. County digital geologic mapping. Final report. Office of Scientific and Technical Information (OSTI), December 1995. http://dx.doi.org/10.2172/216280.

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Wypych, Alicja, ed. Northeast Tanacross geologic mapping project, Alaska. Alaska Division of Geological & Geophysical Surveys, 2020. http://dx.doi.org/10.14509/30537.

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Lyttle, P. T. Societal drivers for geologic mapping and the value of 3-D mapping. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/299499.

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Keefer, D. A., E. D. McKay, and R. C. Berg. Evaluating uncertainty in geologic models from the IL29 geologic mapping project. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/299497.

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Wypych, Alicja. Introduction to the northeast Tanacross geologic mapping project. Alaska Division of Geological & Geophysical Surveys, 2020. http://dx.doi.org/10.14509/30538.

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Davis, George. Geologic and Geoarchaeological Mapping of the Sanctuary of Zeus, Peloponnesus, Greece. Geological Society of America, March 2018. http://dx.doi.org/10.1130/2018.dmch023.

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Dey, W. S., A. M. Davis, C. C. Abert, B. B. Curry, and J C Seiving. Three-dimensional geologic mapping of groundwater resources in Kane County, Illinois. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221881.

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Grunsky, E. C., D. Corrigan, U. Mueller, and G. F. Bonham-Carter. Predictive geologic mapping using lake sediment geochemistry in the Melville Peninsula. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/291901.

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Szumigala, D. J. Alaska GeoSurvey News - Mineral-oriented geologic mapping of the Fortymile mining district. Alaska Division of Geological & Geophysical Surveys, October 2000. http://dx.doi.org/10.14509/14585.

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Hendricks, M. D., P. G. Ekberg, J. E. Athey, W. C. Wyatt, A. L. Willingham, and T. J. Naibert. AK GeMS data dictionary: A description of the Alaska geologic mapping schema. Alaska Division of Geological & Geophysical Surveys, 2021. http://dx.doi.org/10.14509/30669.

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