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Dissertations / Theses on the topic 'Geology – Alberta'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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1

Balzer, Solweig A. "Quaternary geology and dispersal patterns, Winagami region, Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ59928.pdf.

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2

Marquez, C. Xiomara M. (Marquez Ceballos). "Reservoir geology of upper Devonian Leduc buildups, deep Alberta basin." Thesis, McGill University, 1994. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=28487.

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Upper Devonian (Frasnian) stromatoporoid and coral buildups in the Alberta Basin are among the most important hydrocarbon reservoirs in Western Canada. In the deep basin ($>$4000 m), Strachan, Ricinus West and adjacent buildups have similar depositional facies, but have experienced different diagenetic processes that affected their reservoir characteristics. The most important diagenetic alteration is dolomitization that partially to completely replaced the original limestone buildups. Replacement dolomitization occurred at shallow depths near 500 m, indicated by petrographic and geologic rela

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3

Machel, Hans-G. (Hans-Gerhard). "Facies and diagenesis of the Upper Devonian Nisku formation in the subsurface of central Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=71974.

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The Nisku Formation in the Alberta subsurface consists of bank facies, reefal facies, and basinal/slope facies along the Outer Shelf. The bank facies was not previously recognized, and is here designated the Dismal Creek Member. Most buildups are coral-bearing mudmounds.<br>The Nisku Formation was affected by more than twenty diagenetic processes, most notably by dolomitization and anhydritization. The buildups were partially lithified in shallow phreatic environments, and some were subaerially exposed. Dolomitization took place at depths of about 300 to 1000 m by fluids that were derived main

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4

Stevenson, Patrick M. "Petroleum geology and geochemistry of the Manyberries oil field, southeastern Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ38614.pdf.

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5

Stevenson, Patrick M. "Petroleum geology and geochemistry of the Manyberries oil field, southeastern Alberta." Calgary, Alta. : University of Calgary, 1998. https://dspace.ucalgary.ca/handle/1880/26270.

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Thesis (M.Sc.) -- University of Calgary, 1998.<br>Three folded leaves and 3 1/2 in. computer disk in back pocket. 3 folded leaves and 3 1/2 in. computer disk in back pocket. Includes bibliographical references. Also available on microfiche. Available in PDF format via the World Wide Web.

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6

Teitz, Martin W. "Late proterozoic Yellowhead and Astoria Carbonate Platforms, southwest of Jasper, Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63371.

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7

Holme, Philip J. "Quarternary geology and stratigraphy of the Beaver Mines map area, southwest Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ39833.pdf.

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8

Drover, David Howard. "Regional and detailed structural geology of the Quirk Creek structure, S.W. Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0017/MQ55203.pdf.

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9

Chouinard, Hugo. "Lithofacies and diagenesis of the Cooking Lake platform : carbonates, Alberta Basin subsurface, Canada." Thesis, McGill University, 1993. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=69588.

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The Cooking Lake Formation in east-central Alberta is a widespread sheet-like carbonate unit that is up to 100 m thick.<br>The lithofacies of the Cooking Lake Formation platform are assigned to eight depositional environments: (1) deep subtidal argillaceous calcimudstones, (2) deep to shallow subtidal nodular wackestones, (3) intermediate subtidal skeletal lime wackestones, (4) intertidal stromatoporoid/coral floatstones to rudstones, (5) shallow subtidal to lagoonal Amphipora floatstones, (6) shallow-shoal grainstones, (7) semi-restricted shallow subtidal peloidal wackestones/packstones, and

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10

Nodwell, Byron J. "Sedimentology, stratigraphy and depositional history of the Falher F conglomerate trend, Alberta, Canada." Thesis, McGill University, 2004. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=81368.

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Detailed sequence stratigraphic analyses indicate that the lower Cretaceous Falher F unit is made up of 4 sandy/pebbly prograding parasequences labeled F1, F2, F3, and F4. Of the parasequences only F3 has a significant (>2m) thickness of conglomerate. Vertical lithological successions through a conglomeratic section suggest that the F3 pebbles were deposited on the upper shoreface and foreshore as part of a conformable, shoaling-upwards package of rocks. Detailed mapping, using core, well logs, production data and 3-D seismic, show that the conglomerates form a 4 km wide linear body dep

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11

Lebel, Daniel. "Geometry, kinematics, and computer simulations of thrust faulting, central Canadian Rocky Mountains, Alberta." Thesis, McGill University, 1993. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=41240.

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In the central Canadian Rocky Mountain thrust-fold belt, three types of first order decollements are outlined within or along the border of the present orogenic wedge: one basal decollement, three intermediate or internal decollements and one upper decollement. Structural relationships suggest that each internal decollement is the result of one of the successive forward shifts of early basal decollements to new positions within the stratigraphic pile.<br>Two computer programs have been developed to analyze the propagation of multiple thrust faults and their influence on the geometry of a thrus

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12

Duggan, James P. "Sedimentology and diagenesis of Swan Hills Simonette oil field, west-central Alberta basin." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/mq37116.pdf.

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13

Becker, Sherry. "Depositional environments, provenance and sequence stratigraphy of the type Sassenach Formation, Jasper, Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0005/MQ44081.pdf.

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14

McCrimmon, G. Glen. "Sedimentology and sequence stratigraphy of the lower Cretaceous Clearwater Formation, Cold Lake, Alberta." Thesis, University of Ottawa (Canada), 1996. http://hdl.handle.net/10393/9765.

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The lower Cretaceous (Aptian to Albian) CLearwater Formation at Cold Lake, Alberta contains a complex assemblage of silicicastic strata. On the basis of detailed core analyses, Clearwater Formation strata have been subdivided into eight lithofacies and six recurring, facies associations. These facies associations are: (1) Tidal bar, (2) Sand flat, (3) Tidal-fluvial channel, (4) Fluvial channel, (5) Shoreface to foreshore, and (6) Offshore. Correlation of the facies associations and their bounding time-significant surfaces has led to the interpretation that Clearwater Formation strata are marin

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15

Qing, Hairuo. "Diagenesis and sedimentology of rainbow F and E buildups (Middle Devonian), northwestern Alberta." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65414.

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16

Molgat, Marianne Patricia. "Sedimentology, stratigraphy, and shallow burial alteration of the Upper Jurassic Swift Formation, southeastern Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0016/MQ57146.pdf.

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17

Boucher, Ryan James. "Mapping Sweetness of the Second White Speckled Shale S Member| Ricinus Area, Alberta, Canada." Thesis, University of Louisiana at Lafayette, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=10163266.

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<p> The Second White Speckled Shale Formation, located in the Western Canadian Sedimentary Basin is Late Cretaceous (Cenomanian-Turonian) in age, and consists of finely interbedded siltstone and mudstone. Since the 1960s, the formation has produced oil and gas in unpredictable quantities. Understanding the lateral heterogeneity of the formation’s characteristics such as thickness, hydrocarbon saturation, total porosity, brittleness, clay volume, and TOC could potentially help to uncover causes for production variations. In this study, well logs and core data from 25 different wells were

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18

Koladich, Andre Myles. "Sedimentology, sequence stratigraphy, and reservoir quality of the Lower Cretaceous Glauconitic Sandstone, southeastern Alberta." Thesis, University of Ottawa (Canada), 2004. http://hdl.handle.net/10393/26680.

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The Lower Cretaceous (Albian) Glauconitic Sandstone is the lowermost stratigraphic unit of the Upper Mannville interval in southern Alberta. It overlies calcareous and fossiliferous strata of the Ostracode Limestone and is unconformably overlain by feldspathic and lithic-rich fluvial sandstone of the undifferentiated Upper Mannville. In the study area, Glauconitic Sandstone strata comprise three facies associations consisting of prograding shoreface to shallow shelf (FA1I), upper estuary channel fill (FA2) and tidally-influenced abandoned channel fill/interchannel (FA3) deposits. The Jenner Up

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19

Mallamo, Mark P. "Paleoceanography of the upper Devonian Fairholme Carbonate Complex, Kananaskis-Banff area, Alberta." Thesis, McGill University, 1995. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=39958.

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The Fairholme Carbonate Complex is the southernmost and largest in an extensive stromatoporoid-dominated reef domain that developed in Alberta during Frasnian time. Its western margin is defined, and exhibits a major re-entrant 25 km wide named the Shark Embayment. A Devonian paleoclimatic model suggests that the western margin was subjected to seasonal oceanic upwelling of nutrient-rich and oxygen-poor waters that influenced the development of the carbonate buildups.<br>Lithostratigraphic units of the Fairholme Group are characterized in terms of a Rocky Mountain (RM) Conodont Zonation. In th

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20

Laflamme, Andre K. "Replacement dolomitization in the Upper Devonian Leduc and Swan Hills formations, Caroline area, Alberta, Canada." Thesis, McGill University, 1990. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59892.

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Replacement matrix dolomite (RMD) is present throughout the Leduc/Cooking Lake Formation, but is restricted to the bank margin in the Swan Hills Formation. RMD has an average crystal size of 140$ mu$m and fluoresces yellow in the Leduc/Cooking Lake Formation but has an average crystal size of 250$ mu$m and fluoresces green in the Swan Hills Formation. RMD formed before the onset of stylolitization. It has abundant inclusions, a homogeneous red cathodoluminescent response, and similar trace element concentrations in both formations. $ delta sp{18}$O values overlap for the most part, but some Sw

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21

James, D. P. "Stratigraphy, sedimentology and diagenesis of Upper Jurassic and Lower Cretaceous (Mannville) strata, Southwestern Alberta." Thesis, University of Oxford, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.371509.

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22

Drivet, Eva. "Diagenesis and reservoir characteristics of Upper Devonian Leduc dolostones, southern Rimbey-Meadowbrook reef trend, central Alberta." Thesis, McGill University, 1993. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=68172.

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Dolomitization of Leduc Formation (Upper Devonian) along the southern part of the Rimbey-Meadowbrook trend in central Alberta occurred early by pervasive replacement, and later by minor cementation. Replacive dolomitization postdates submarine cementation and deposition of overlying shales, overlaps stylolitization, and produces $ delta sp{18}$O values indicating precipitation between 45 and 75$ sp circ$C. Therefore, this dolomitization likely originated at burial depths of more than 500 m. Strontium isotope ratios suggest that dolomitizing fluids were slightly more radiogenic than Upper Devon

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23

Walsh, Warren J. A. "Sedimentology and sequence stratigraphic framework of the Lower Cretaceous Bluesky Formation, Valhalla area, west-central Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0022/MQ52310.pdf.

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24

Venieri, Marco. "Reservoir characterization of the Cardium Formation in the Ferrier Oilfield, west-central Alberta, Canada." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amslaurea.unibo.it/10091/.

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This thesis has the main aim of defining the lithostratigraphy, depositional architecture, post-depositional modifications and reservoir characteristics of the Cardium Formation in the Ferrier Oilfield, and how these characteristics can have great impact over production rates, GOR and produced fluid discrimination. In the Ferrier area, the Cardium Formation is composed by a NE prograding clastic sequence made up of offshore to shoreface deposits sealed by marine shales. The main reservoir is composed by sandstones and conglomerates interpreted to have deposited in a shoreface depositional en

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25

Tan, Wenbin. "Origins of replacement dolomites, upper Devonian Leduc, Nisku and Wabamun formations, southeastern Alberta western Canada sedimentary basin." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0021/NQ44607.pdf.

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26

Hill, Robert E. (Robert Einar). "Stratigraphy and sedimentology of the Middle Proterozoic Waterton and Altyn Formations, Belt-Purcell Supergroup, southwest Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63330.

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27

Shiraki, Masahiro. "Upper Devonian sponge-algal mud mounds, southern flank of Miette reef complex, Jasper National Park, Alberta, Canada." Thesis, McGill University, 1996. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=27409.

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A series of small mud mounds are exposed in the McConnell and Miette thrust sheets on the southern flank of the Miette reef complex. They occur on the southeastward inclined carbonate clinoforms of the late Frasnian Arcs Member. These mounds are rooted on marine, argillaceous lime mudstones and are surrounded by lime mudstones of several prograding clinoforms of the upper Arcs Member or dolomitic siltstones of the lower Ronde Member.<br>Mounds are approximately 17 to 36 m high and 32 to 81 m wide and columnar to domal in shape. The lower part of the mounds consists of sponge-rich wackestones a

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28

Tawadros, Ezzat Edward. "Stratigraphy, sedimentology and petrology of the Cambrian rocks in the subsurface of Southern Alberta, Canada." Thesis, University of St Andrews, 1988. http://hdl.handle.net/10023/11694.

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The Cambrian section in the subsurface of southern Alberta has a maximum thickness of 1860'. It is composed of sandstones, shales, limestones, and dolomites. The grand cycles characteristic of the Cambrian Sections in the Foothills and Front Ranges can be traced to some distance in the subsurface. However, the section changes facies eastwards into clastics and the grand cycles become less defined. The present correlations indicate that the Waterfowl-Arctomys grand cycle extends to the subsurface but is restricted to the northwest corner of the study area. Two new stratigraphic units have been

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29

McCullagh, Timothy. "Investigating the controls on production from a basin-centered gas accumulation: lower cretaceous cadotte member, Deep Basin Alberta." Thesis, McGill University, 2008. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=18668.

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This thesis examines the controls on gas production from a Cretaceous sandstone deposit located within the Deep Basin of Alberta, Canada. By integrating core, wireline log, 3-D seismic, petrophysical, pressure and production data, we show that the best production comes from permeable chert-rich shoreface and beachface sandstones separated laterally and cyclically by tighter quartzose sandstones. The physical properties of the two lithologies are sufficiently different that they can be distinguished seismically; a map of seismic amplitudes for the Cadotte shows curvilinear high-amplitude anom

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30

Crerar, Erin Elizabeth. "Sedimentology and stratigraphic evolution of a tidally influenced marginal-marine complex: The Lower Cretaceous McMurray Formation, Athabasca oil sands deposit, northeastern Alberta." Thesis, University of Ottawa (Canada), 2003. http://hdl.handle.net/10393/26464.

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Within the Lewis study area, McMurray Formation strata comprise 4 facies associations that form a depositional continuum of braided-fluvial (FA1), tidally-influenced braided- to low-accommodation meandering-fluvial and meandering-tidal channel-fills (FA2), associated overbank (FA3), and open-estuarine tidal flat deposits (FA4). The primary reservoir occurs in transgressive FA2 deposits. Lower-FA2 channels incise older water-wet FA1sand and consist of medium to locally-coarse, bitumen-saturated sand with rare to locally common pin-stripe laminated and/or 1--5 cm thick mud beds. Channels were in

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31

Kahmann-Robinson, Julia A. Atchley Stacy C. "The sequence stratigraphic evolution of the Sturgeon Lake bank, central Alberta, Canada and its regional implications." Waco, Tex. : Baylor University, 2005. http://hdl.handle.net/2104/3016.

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32

Zymela, Steve. "Carbon, oxygen and strontium isotopic composition of diagenetic calcite and siderite from the Upper Cretaceous Cardium Formation of Western Alberta /." *McMaster only, 1996.

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33

Stritch, Rebecca A. (Rebecca Ann) Carleton University Dissertation Earth Sciences. "Early Cretaceous (Albian) foraminifera in Northwestern and Central Alberta, Canada; biostratigraphy and paleoenvironmental changes." Ottawa, 1997.

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34

Smith, Sean G. W. "The origin and timing of late-stage carbonate cements in Devonian carbonates of the deep Alberta basin : based on fluid inclusion and isotopic evidence." Thesis, McGill University, 2001. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=31541.

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Deep basin Leduc Obed and Swan Hills Simonette calcite fluid inclusions yielded Th ranges of 127 to 172°C and 122 to 158°C; while saddle dolomites have Th from 136 to 148°C and 133 to 162°C, respectively. Calcite data from the subsurface suggest a 20°C/km geothermal gradient and saddle dolomite data a gradient around 23°C. Vug-filling calcites from Spray Lakes, Parker's Ridge and Big Hill, yielded Th data (128.0 to 155.1°C) similar to vug-filling cements from Obed and Simonette. Fluids in the fracture-filling saddle dolomites analysed have an average T h of 171.6°C and salinity of 17.1. Post-t

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35

Miyagi, Lowell. "Microstructures and Deformation in Some Fault Rocks From The McConnell Thrust at Mount Yamnuska (Alberta) : Implications for Fluid Flow and Faulting and Cycles of Strain-Hardening and Softening." Oberlin College Honors Theses / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1411739220.

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36

Tremblay, James Vincent. "Trilobites and strata of the Lower and Middle Cambrian Peyto, Mount Whyte and Naiset Formations, Alberta and British Columbia /." *McMaster only, 1996.

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37

Halim-Dihardja, Marjammanda K. "Diagenesis and sedimentology of the late Devonian (Famennian) Wabamun group in the Tangent, Normandville, and Eaglesham fields, north-central Alberta." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63807.

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38

Kaylor, Donald Charles. "Facies and diagenesis of the upper Devonian Palliser formation, front ranges of the Southern Rocky Mountains, Alberta and British Columbia." Thesis, McGill University, 1988. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=64029.

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39

Green, Darryl G. "Dolomitization and burial diagenesis of the Devonian west-central Alberta deep basin : Kaybob South and Fox Creek (Swan Hills Formation) and Pine Creek fields (Leduc and Wabamun Formations)." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0016/NQ50178.pdf.

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40

Rock, Luc. "Sedimentology, diagenesis and reservoir characteristics of the Devonian Simonette (Leduc Formation) and Ante Creek (Swan Hills Formation) fields : a comparison between a limestone and dolomite field, west-central Alberta basin." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0019/MQ55089.pdf.

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41

Ball, Nathaniel H. Atchley Stacy C. "Depositional and diagenetic controls on reservoir quality and their petrophysical predictors within the Upper Cretaceous (Cenomanian) Doe Creek Member of the Kaskapau Formation at Valhalla Field, Northwest Alberta." Waco, Tex. : Baylor University, 2009. http://hdl.handle.net/2104/5296.

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42

Hiller, Axel, and Werner Schuppan. "Geologie und Uranbergbau im Revier Schlema-Alberoda." Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2011. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-78919.

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Die Uran-Ganglagerstätte Schlema-Alberoda wurde, abgesehen von mehreren Altbergbauaktivitäten auf ihrem Territorium und der Nutzung ihrer radioaktiven Wässer im früheren Radiumbad Oberschlema, de facto erst nach dem Zweiten Weltkrieg entdeckt. Sie hat sich im Verlaufe ihrer Erkundung und des Abbaus als eine der größten Lagerstätten ihres Typs auf der Erde erwiesen. Die Lagerstätte Schlema-Alberoda liegt regionalgeologisch gesehen in der erzgebirgisch streichenden Lößnitz-Zwönitzer Synklinale im Kreuzungsbereich mit der NW-SO gerichteten Gera-Jáchymov-Störungszone. Bedeutsamstes tektonisches El

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43

Hiller, Axel, and Werner Schuppan. "Geologie und Uranbergbau im Revier Schlema-Alberoda." Sächsisches Landesamt für Umwelt, Landwirtschaft und Geologie, 2008. https://slub.qucosa.de/id/qucosa%3A1646.

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Die Uran-Ganglagerstätte Schlema-Alberoda wurde, abgesehen von mehreren Altbergbauaktivitäten auf ihrem Territorium und der Nutzung ihrer radioaktiven Wässer im früheren Radiumbad Oberschlema, de facto erst nach dem Zweiten Weltkrieg entdeckt. Sie hat sich im Verlaufe ihrer Erkundung und des Abbaus als eine der größten Lagerstätten ihres Typs auf der Erde erwiesen. Die Lagerstätte Schlema-Alberoda liegt regionalgeologisch gesehen in der erzgebirgisch streichenden Lößnitz-Zwönitzer Synklinale im Kreuzungsbereich mit der NW-SO gerichteten Gera-Jáchymov-Störungszone. Bedeutsamstes tektonisches El

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44

Berra, Ivan. "Sédimentologie, stratigraphie isotopique du strontium et chemostratigraphie à la transition Frasnien-Famennien (Dévonien supérieur) en Amérique du Nord: implications orogéniques dans la crise biologique." Doctoral thesis, Universite Libre de Bruxelles, 2008. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/210400.

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Le sommet du Frasnien est une époque difficile pour la biodiversité sur la Terre, en particulier pour les organismes d’eaux chaudes et peu profondes. Cette étude vise à établir un lien entre l’activité tectonique et la crise biologique. Trois coupes d’Amérique du Nord, de la marge ouest du paléocontinent Laurentia, liées au front orogénique Antler ont été étudiées pour leurs rapports isotopiques 87Sr/86Sr dans les carbonates. La coupe de Devils Gate dans le centre Nevada (USA) présente au sommet du Frasnien des faciès de turbidites carbonatées de bassin. Trois pics successifs de 87Sr/86Sr s’ob

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45

Fanti, Federico <1981&gt. "Stratigraphy and Palaeontology of the Late Cretaceous Wapiti Formation, west-central Alberta, Canada." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2009. http://amsdottorato.unibo.it/1498/.

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A complete stratigraphic assessment and revision of the middle Campanian to upper Maastrichtian Wapiti Formation in north-western Alberta and north-eastern British Columbia is the main aim of this research project. The study area encompasses an area of approximately 200X180 km in the Grande Prairie County (west-central Alberta) and easternmost British Columbia, Canada. Results presented here indicate that the 1300m thick succession currently reported in the literature as “undifferentiated lithostratigraphic unit”, consists of five lithostratigraphic units and four unconformity-bounded depositi

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46

Dias, Cíntia Melazo. "Emissão de 14C pelas unidades I e II da Central Nuclear Almirante Álvaro Alberto (CNAAA) e seu efeito local nos níveis ambientais." reponame:Repositório Institucional da UnB, 2006. http://repositorio.unb.br/handle/10482/1938.

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Tese (doutorado)—Universidade de Brasília, Instituto de Geologia, 2006.<br>Submitted by Fernanda Weschenfelder (nandaweschenfelder@gmail.com) on 2009-10-07T19:50:55Z No. of bitstreams: 1 2006_Cintia Melazo Dias.pdf: 4634963 bytes, checksum: 758314d9ec5efba3aee170fe32fcf97f (MD5)<br>Approved for entry into archive by Tania Milca Carvalho Malheiros(tania@bce.unb.br) on 2009-10-13T14:36:31Z (GMT) No. of bitstreams: 1 2006_Cintia Melazo Dias.pdf: 4634963 bytes, checksum: 758314d9ec5efba3aee170fe32fcf97f (MD5)<br>Made available in DSpace on 2009-10-13T14:36:31Z (GMT). No. of bitstreams: 1 200

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McFarland, Lynn Margaret. "Using the chemical and isotopic characteristics of drinking water to determine sources of potable water and subsurface geologic controls on water chemistry, Stoney Indian Reserve, Morley, Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp04/mq20840.pdf.

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Shulba, William Paul. "Geovisualization of boreal peatland architecture in a three dimensional hydrogeological framework using ground penetrating radar and LiDAR at Mariana Lakes, Alberta, Canada." Thesis, 2021. http://hdl.handle.net/1828/13022.

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Communicating science in three-dimensional (3D) multimedia is an immersive and interactive way to explore scientific processes (Signals and Communication Technology, 2019). Geovisualization is an emerging 3D multimedia method for visual analysis, synthesis, and presentation of geospatial, geologic, and geophysical data (MacEachren & Kraak, 2001). There is an identified need to develop scientific communication tools to further understand boreal peatland evolution, hydrogeology, ecology, and geochemistry (Bubier et al., 2003) since the International Union of Conservation of Nature asserts that p

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