Relevant bibliographies by topics / Aquifer Stratigraphy

Contents

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

Academic literature on the topic 'Aquifer Stratigraphy'

Author: Grafiati
Published: 5 June 2025
Last updated: 2 August 2025

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Journal articles on the topic "Aquifer Stratigraphy"

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Wood, Alexander J., Abraham E. Springer, and Benjamin W. Tobin. "Geochemical Variability in Karst-Siliciclastic Aquifer Spring Discharge, Kaibab Plateau, Grand Canyon." Environmental and Engineering Geoscience 26, no. 3 (2020): 367–81. http://dx.doi.org/10.2113/eeg-2345.

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ABSTRACT The source area of groundwater for springs discharging from lithologically variably perched aquifers is essential to understand when establishing baseline aquifer characteristics. Stratigraphic data from hydrostratigraphic outcrops and geochemical data from springs were used to characterize the hydrogeology of a remote, data-poor aquifer. This study focuses on the hydrogeological variability within the shallow karst-siliciclastic Coconino (C) aquifer on the Kaibab Plateau, north of Grand Canyon National Park. Stratigraphic data were collected from 8 locations, and 22 C aquifer springs
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HENRY, J. L., P. R. BULLOCK, T. J. HOGG, and L. D. LUBA. "GROUNDWATER DISCHARGE FROM GLACIAL AND BEDROCK AQUIFERS AS A SOIL SALINIZATION FACTOR IN SASKATCHEWAN." Canadian Journal of Soil Science 65, no. 4 (1985): 749–68. http://dx.doi.org/10.4141/cjss85-080.

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The stratigraphy and hydrology of saline soils were investigated at 15 sites in Saskatchewan, Canada. At five sites (Series A) nests of piezometers were installed and at 10 sites (Series B) a single piezometer was installed in or near an aquifer. Piezometric surface data from the nests showed the potential for upward movement in all Series A sites. The electrical conductivity (EC) of water from Series A piezometers increased from the deepest to shallowest and there was a general increase in soil EC towards the soil surface. Hydraulic conductivity of strata was measured at three sites and varie
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Warner, Don L. "On: “Subsurface fault detection using seismic data for hazardous‐waste‐injection well permitting: An example from St. John the Baptist Parish, Louisiana” by E. V. Zinni (March‐April 1995 GEOPHYSICS, 60, p. 468–475)." GEOPHYSICS 62, no. 1 (1997): 381–83. http://dx.doi.org/10.1190/1.1444142.

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Zinni (1995) has studied the stratigraphy and structural geology of injection reservoirs and aquifers in the vicinity of the DuPont Ponchartrain Works plant and has concluded that “The injection of liquid hazardous waste into the 2440-, 1430-m, and 1130-m injection reservoirs could jeopardize not only the water quality of the Covington aquifer, but possibly other shallow freshwater aquifers….”
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Wrege, Beth M., and J. Jeffery Isely. "High-resolution hydro- and geo-stratigraphy at Atlantic Coastal Plain drillhole CR-622 (Strat 8)." Stratigraphy 6, no. 1 (2009): 79–86. http://dx.doi.org/10.29041/strat.06.1.06.

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We interpret borehole geophysical logs in conjunction with lithology developed from continuous core to produce high-resolution hydro- and geo-stratigraphic profiles for the drillhole CR-622 (Strat 8) in the Atlantic Coastal Plain of North Carolina. The resulting hydrologic and stratigraphic columns show a generalized relation between hydrologic and geologic units. Fresh-water aquifers encountered are the surficial,Yorktown, Pungo River and Castle Hayne.Geologic units present are of the middle and upper Tertiary and Quaternary periods, these are the Castle Hayne (Eocene), Pungo River (Miocene),
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Balia, Roberto, Enrico Gavaudò, Federica Ardau, and Giorgio Ghiglieri. "Geophysical approach to the environmental study of a coastal plain." GEOPHYSICS 68, no. 5 (2003): 1446–59. http://dx.doi.org/10.1190/1.1620618.

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In the study of coastal plains affected by soil and water salination, a knowledge of several geological aspects, such as structural features, depth to basement, stratigraphy of sedimentary cover, relationships between the phreatic aquifer and underlying aquifers, and the latter's structure, is basic to gaining an adequate understanding of both the causes and possible evolution of salination. In this framework, geophysical techniques can play a very important role. To improve the available geophysical information about the Muravera coastal plain, Sardinia, Italy, which is affected by severe soi
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Strehlow, K., J. H. Gottsmann, and A. C. Rust. "Poroelastic responses of confined aquifers to subsurface strain and their use for volcano monitoring." Solid Earth 6, no. 4 (2015): 1207–29. http://dx.doi.org/10.5194/se-6-1207-2015.

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Abstract. Well water level changes associated with magmatic unrest can be interpreted as a result of pore pressure changes in the aquifer due to crustal deformation, and so could provide constraints on the subsurface processes causing this strain. We use finite element analysis to demonstrate the response of aquifers to volumetric strain induced by pressurized magma reservoirs. Two different aquifers are invoked – an unconsolidated pyroclastic deposit and a vesicular lava flow – and embedded in an impermeable crust, overlying a magma chamber. The time-dependent, fully coupled models simulate c
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Sugarman, Peter J., Kenneth G. Miller, James V. Browning, Andrew A. Kulpecz, Peter P. McLaughlin, Jr., and Donald H. Monteverde. "Hydrostratigraphy of the New Jersey Coastal Plain: Sequences and facies predict continuity of aquifers and confining units." Stratigraphy 2, no. 3 (2005): 259–75. http://dx.doi.org/10.29041/strat.02.3.04.

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The regional extent and connectivity of Cretaceous to Miocene aquifer sands in the New Jersey Coastal Plain are evaluated using detailed facies analysis within a sequence stratigraphic framework.We correlate sequences from continuous coreholes using well logs to trace strike and dip sections throughout this region, allowing us to predict the continuity of confining units and aquifer sands. Marine sequences follow a predictable shallowing upward pattern: fine-grained shelf and prodelta sediments grade upward into delta front and shallow-marine sands, corresponding to confining unit-aquifer coup
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Camuñas Palencia, Carlos, Miguel Mejías Moreno, Jorge Hornero Díaz, Fernando Ruíz Bermudo, and Olga García Menéndez. "Deep aquifers as strategic groundwater reservoir in Spain." BOLETÍN GEOLÓGICO Y MINERO 133, no. 3 (2022): 7–26. http://dx.doi.org/10.21701/bolgeomin/133.3/001.

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The objective of this paper is to establish a definition of deep aquifers, develop a methodological proposal to help select them as strategic groundwater reserves and develop a first inventory of deep aquifers in peninsular Spain, organized by hydrographic districts. The basic premises followed to consider a permeable formation as a deep aquifer are: water table depth greater than 300 m in free aquifers or the top of the permeable formation in the case of confined aquifers. A deep aquifer is also considered to be the lower horizon of very thick aquifers (from 300 m), from which the most superf
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Lévesque, Yan, Julien Walter, and Romain Chesnaux. "Transient Electromagnetic (TEM) Surveys as a First Approach for Characterizing a Regional Aquifer: The Case of the Saint-Narcisse Moraine, Quebec, Canada." Geosciences 11, no. 10 (2021): 415. http://dx.doi.org/10.3390/geosciences11100415.

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Geological contexts that lack minimal stratigraphic and piezometric information can be challenging to produce an initial hydrogeological map in remote territories. This study proposes an approach to characterize a regional aquifer using transient electromagnetic (TEM) surveys. Given the presence of randomly dispersed boreholes, the Saint-Narcisse moraine in the Mauricie region of Quebec (Canada) is an appropriate site for collecting the required geophysical data, correlating the stratigraphic and piezometric information, and characterizing regional granular aquifers in terms of stratigraphy, g
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Morrison, T., E.E Esonanjor, and S. Mangewosa. "An Evaluation of Aquifer Lithostratigraphy and groundwater quality in Ikwerre Local Government Area in the Niger Delta, Nigeria." Journal of Scientific and Engineering Research 9, no. 11 (2022): 119–30. https://doi.org/10.5281/zenodo.10529764.

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<strong>Abstract</strong> The Stratigraphy of the aquifer and hydrochemical properties of groundwater in Ikwerre Local Government Area were assessed. This was to determine the aquifer location, composition and type, and also to ascertain the groundwater suitability for domestic use. Six boreholes in six communities were used.iStrata log was used for the stratigraphic studies while water samples were analysed for iron, chloride, salinity, pH, conductivity and Alkalinity. Two aquifers were delineated at varying depths. Sample analysis in the laboratory was done using the standard method of ASTM
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Dissertations / Theses on the topic "Aquifer Stratigraphy"

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Banaszak, Joel F. "Hydrostratigraphic Framework for the Surficial Aquifer in the Indian River Bay, Delaware, Watershed." University of Toledo / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=toledo1313531448.

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Gámez, Torrent Desiré. "Sequence Stratigraphy as a tool for water resources management in alluvial coastal aquifers: application to the Llobregat delta (Barcelona, Spain)." Doctoral thesis, Universitat Politècnica de Catalunya, 2007. http://hdl.handle.net/10803/6255.

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Most coastal aquifers undergo seawater intrusion. Mitigating this risk depends on a sound knowledge of flow mechanisms, well located and constructed wells, an effective management, suitable policies and the desire to conserve the aquifer. To this end, a comprehensive geological model is essential. The single most important question that the geological model should address is the degree and nature of the connection of the aquifer to the sea. Differences in the connection explain why apparently similar coastal aquifers display very different salinitzation behavior. Some aquifers salinize with mo
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Friedenberg, Roselyne, and Michel Hoffert. "Stratigraphie genetique et architecture du facies buntsandstein de l'est du bassin de paris avec applications aux stockages de gaz naturel en nappe aquifere." Strasbourg 1, 1994. http://www.theses.fr/1994STR13241.

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Des reservoirs greseux (structures de velaines-sous-amance et hoeville), situes dans le buntsandstein superieur (scythien-anisien) de lorraine (est de nancy), sont exploites par gaz-de-france depuis 1968, pour le stockage souterrain du gaz naturel en nappes aquiferes. La nature sedimentologique et la geometrie des niveaux reservoirs restaient encore mal connues. Les nombreuses donnees disponibles (plus de 50 puits avec diagraphies et carottes) ainsi qu'un maillage serre (environ 100 metres) ont permis une etude sedimentologique poussee et l'utilisation de la stratigraphie genetique a haute res
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Aunay, Bertrand. "Apport de la stratigraphie séquentielle à la gestion et à la modélisation des ressources en eau des aquifères côtiers." Phd thesis, Université Montpellier II - Sciences et Techniques du Languedoc, 2007. http://tel.archives-ouvertes.fr/tel-00275467.

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Lieu de développement économique et démographique intense, les zones littorales font l'objet de pressions importantes sur l'environnement et, en particulier, sur les ressources en eau. Bien que la gestion des eaux souterraines côtières bénéficie de nombreux résultats issus de la recherche scientifique, une des problématiques majeures reste la connaissance de la géométrie des aquifères. Des interprétations géologiques de la genèse du bassin Plio-Quaternaire du Roussillon, issues de la stratigraphie séquentielle, sont confrontées, par l'intermédiaire d'une base données, à l'hydrogéologie de cet
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Yitbarek, Baye Andarge. "Hydrogeological and hydrochemical framework of complex volcanic system in the Upper Awash River basin, Central Ethiopia : with special emphasis on inter-basins groundwater transfer between Blue Nile and Awash rivers." Poitiers, 2009. http://theses.edel.univ-poitiers.fr/theses/2009/Yitbarek-Baye-Andarge/2009-Yitbarek-Baye-Andarge-These.pdf.

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Une approche utilisant plusieurs méthodes convergentes a été mise en oeuvre pour étudier le cadre hydrogéologique du système aquifère volcanique fracturé et complexe du bassin supérieur du fleuve Awash situé sur le bord du Rift éthiopien. L'écoulement des eaux souterraines et les mécanismes de recharge des différents aquifères ont été étudiés à l'aide de méthodes conventionnelles de terrain, de l'hydrochimie, de l'hydrologie isotopique et de la modélisation numérique des flux souterrains. Des relations lithohydrostratigraphiques ont été établies à partir des logs lithologiques de forages explo
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Erskine, Jon Allen. "The stratigraphy, depositional history, and hydrogeology of a shallow, coastal aquifer system, northern Monterey County, CA new interpretations based on indicator geostatics /." Diss., 1998. http://catalog.hathitrust.org/api/volumes/oclc/41147095.html.

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Jones, Ian Christopher. "Geochemical evolution of groundwater in the Pleistocene limestone aquifer of Barbados." Thesis, 2002. http://wwwlib.umi.com/cr/utexas/fullcit?p3110625.

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"Sequence Stratigraphy as a tool for water resources management in alluvial coastal aquifers: application to the Llobregat delta (Barcelona, Spain)." Universitat Politècnica de Catalunya, 2007. http://www.tesisenxarxa.net/TDX-0523108-093948/.

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Duvail, Cédric. "Expression des facteurs régionaux et locaux dans l'enregistrement sédimentaire d'une marge passive. Exemple de la marge du Golfe du Lion, étudiée selon un continuum terre-mer." Phd thesis, 2008. http://tel.archives-ouvertes.fr/tel-00438146.

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L'objectif de ce travail est l'étude de l'enregistrement sédimentaire de la marge du Golfe du Lion pendant son évolution post-rift. On met au point une méthodologie basée sur l'exploitation et de données disparates (Banque du Sous-Sol du BRGM, sismique réflexion industrielle, forages pétroliers profonds, affleurements de terrain), conduisant à des corrélations terre-mer haute-résolution et aboutissant à des interprétations de l'évolution post-rift de plusieurs segments de la marge. On met en évidence le rôle de la crise de salinité messinienne dans l'évolution de la marge et les modalités de l
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Books on the topic "Aquifer Stratigraphy"

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Arthur, J. Kerry. Definition of the geohydrologic framework and preliminary simulation of ground-water flow in the Mississippi embayment aquifer system, gulf coastal plain, United States. U.S. Geological Survey, 1990.

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D, Conti Robert, and University of Texas at Austin. Bureau of Economic Geology., eds. Stratigraphy and influence of effective porosity on ground-water flow in the Wolfcamp brine aquifer, Palo Duro Basin, Texas Panhandle. Bureau of Economic Geology, University of Texas at Austin, 1988.

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Anderson, S. R. Stratigraphy of the unsaturated zone and the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho. U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

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Anderson, S. R. Stratigraphy of the unsaturated zone and uppermost part of the Snake River Plain aquifer at test area north, Idaho National Engineering Laboratory, Idaho. U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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Anderson, S. R. Stratigraphy of the unsaturated zone and uppermost part of the Snake River Plain aquifer at Test Area North, Idaho National Engineering Laboratory, Idaho. U.S. Dept. of the Interior, U.S. Geological Survey, 1991.

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D, Weedman Suzanne, Florida Geological Survey, South Florida Water Management District (Fla.), and Geological Survey (U.S.), eds. Lithostratigraphy, geophysics, biostratigraphy, and strontium-isotope stratigraphy of the surficial aquifer system of eastern Collier County and northern Monroe County, Florida. U.S. Geological Survey, 1999.

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Anderson, S. R. Stratigraphy of the unsaturated zone and uppermost part of the Snake River Plain aquifer at the Idaho Chemical Processing Plant and Test Reactors Area, Idaho National Engineering Laboratory, Idaho. U.S. Dept. of the Interior, U.S. Geological Survey, 1991.

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Grubb, Hayes F. Gulf Coast regional aquifer-system analysis: A Mississippi perspective. U.S. Dept. of the Interior, Geological Survey, 1986.

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Grubb, Hayes F. Gulf Coast Regional Aquifer-System Analysis: A Kentucky perspective. U.S. Dept. of the Interior, U.S. Geological Survey, 1991.

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Grubb, Hayes F. Gulf Coast Regional Aquifer-System Analysis: A Kentucky perspective. U.S. Dept. of the Interior, U.S. Geological Survey, 1991.

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Book chapters on the topic "Aquifer Stratigraphy"

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Al-Helal, Anwar, Yaqoub AlRefai, Abdullah AlKandari, and Mohammad Abdullah. "Subsurface Stratigraphy of Kuwait." In The Geology of Kuwait. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-16727-0_2.

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AbstractThis chapter reviews the subsurface stratigraphy of Kuwait targeting geosciences educators. The lithostratigraphy and chronostratigraphy of the reviewed formations (association of rocks whose components are paragenetically related to each other, both vertically and laterally) followed the formal stratigraphic nomenclature in Kuwait. The exposed stratigraphic formations of the Miocene–Pleistocene epochs represented by the Dibdibba, Lower Fars, and Ghar clastic sediments (Kuwait Group) were reviewed in the previous chapter as part of near-surface geology. In this chapter, the description
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Shah, Babar Ali. "Arsenic Contamination in Groundwater in the Middle Gangetic Plain, India: Its Relations to Fluvial Geomorphology and Quaternary Stratigraphy." In Safe and Sustainable Use of Arsenic-Contaminated Aquifers in the Gangetic Plain. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16124-2_3.

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Datsenko, Liudmyla, and Serhii Kolomiiets. "GROUNDWATERS OF NIKOLSKOHO REGION (DONBASS): GEOLOGY, STRATIGRAPHY, HYDROGEOLOGY, TOPOGRAPHIC AND GEODESIC WORKS." In State, trends and prospects of land sciences, environment, physics, mathematics and statistics’ development (1st. ed). Primedia eLaunch LLC, 2020. http://dx.doi.org/10.36074/stplsepmad.ed-1.03.

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Arid regions of the south of Ukraine (Donetsk, Zaporizhia, Kherson regions) are facing an acute shortage of drinking and technical water, which consumption increases from year to year. A clear understanding of the shortage not only drinking water but also water for fish breeding, cultural and recreational needs is worrying the world scientific community. Understanding of hydrogeological, hydrogeochemical processes is important for groundwater protection, especially in arid regions of the world. The study area is located within the central part of the Priazovsk highland. Administratively, it be
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Venable, Niah B. H., David A. Barnes, David B. Westjohn, and Peter J. Voice. "Pennsylvanian fluvial-deltaic depositional systems in central lower Michigan: Sedimentology, stratigraphy, and hydrogeology of the Saginaw Aquifer." In Insights into the Michigan Basin: Salt Deposits, Impact Structure, Youngest Basin Bedrock, Glacial Geomorphology, Dune Complexes, and Coastal Bluff Stability. Geological Society of America, 2013. http://dx.doi.org/10.1130/2013.0031(04).

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SCHULMEISTER, MARCIA K., JAMES J. BUTLER, EVAN K. FRANSEEN, DOUGLAS A. WYSOCKI, and JAMES A. DOOLITTLE. "HIGH-RESOLUTION STRATIGRAPHIC CHARACTERIZATION OF UNCONSOLIDATED DEPOSITS USING DIRECT-PUSH ELECTRICAL CONDUCTIVITY LOGGING: A FLOODPLAIN-MARGIN EXAMPLE." In Aquifer Characterization. SEPM (Society for Sedimentary Geology), 2004. http://dx.doi.org/10.2110/pec.04.80.0067.

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Bethke, Craig M. "Modeling Overview." In Geochemical Reaction Modeling. Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195094756.003.0006.

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A model is a simplified version of reality that is useful as a tool. A successful model strikes a balance between realism and practicality. Properly constructed, a model is neither so simplified that it is unrealistic nor so detailed that it cannot be readily evaluated and applied to the problem of interest. Geologic maps constitute a familiar class of models. To map a sedimentary section, a geologist collects data at certain outcrops. He casts his observations in terms of the local stratigraphy, which is itself a model that simplifies reality by allowing groups of sediments to be lumped toget
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THOMSEN, R. O., I. LERCHE, R. Evans, and N. Piggot. "Hydrodynamic Flow of Oil and Gas in Aquifers and Stratigraphic Trapping." In Rates of Geologic Processes, Tectonics, Sedimentation, Eustasy and Climate - Implications for Hydrocarbon Exploration: 14th Annual. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 1993. http://dx.doi.org/10.5724/gcs.93.14.0243.

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Hickson, Thomas A., Kevin M. Theissen, and Melissa A. Lamb. "Microbialites right under our noses: Miocene and modern lakes near Las Vegas, Nevada, USA." In Field Excursions from Las Vegas, Nevada: Guides to the 2022 GSA Cordilleran and Rocky Mountain Joint Section Meeting. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.0063(06).

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ABSTRACT On this field trip, we will examine a modern lake in central Nevada, the Lower Pahranagat Lake, and lacustrine carbonate outcrops of the late Miocene, upper Horse Spring Formation. Both of the modern and ancient systems hold significant microbialite populations and we interpret that the Lower Pahranagat Lake is a possible analog for the ancient unit. Both systems are or were spring-fed from a similar Paleozoic carbonate aquifer. Both have evidence of microbially influenced sedimentation, probably related to spring activity. Both are dominated by the deposition of carbonate to the excl
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Lamarre, Robert A. "Hydrodynamic and Stratigraphic Controls for a Large Coalbed Methane Accumulation in Ferron Coals of East-Central Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c20.

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Abstract Upper Cretaceous coals within the Ferron Sandstone Member of the Mancos Shale contain large volumes of coalbed methane. Coals at the northern end of the 80-mi (129 km)-long Ferron trend have produced 469 bcf of coalbed methane, as of the end of July 2003. At that time, 735 wells were producing 275 mmcfd. Analysis of cores from exploratory wells indicate that the gas content of the coals decreases dramatically from north to south, even though the rank and maturity of the coals decreases only slightly. The area with lowest gas content correlates with the outcrop of the Ferron coals in t
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Conference papers on the topic "Aquifer Stratigraphy"

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F. Dominic, David, Benjamin H. Richard, Paul J. Wolfe, and Songlin Cheng. "Gamma Logging To Define The Stratigraphy In A Buried-Valley Aquifer System." In 7th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.208.1994_064.

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Dominic, David F., Benjamin H. Richard, Paul J. Wolfe, and Songlin Cheng. "Gamma Logging to Define the Stratigraphy in a Buried‐Valley Aquifer System." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 1994. Environment and Engineering Geophysical Society, 1994. http://dx.doi.org/10.4133/1.2922120.

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Haines, Seth S. "Comparison of Compressional and Shear Wave Seismic Reflection Methods for Characterizing Aquifer Stratigraphy at the Former Fort Ord, California." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2007. Environment and Engineering Geophysical Society, 2007. http://dx.doi.org/10.4133/1.2924690.

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S. Haines, Seth. "Comparison Of Compressional And Shear Wave Seismic Reflection Methods For Characterizing Aquifer Stratigraphy At The Former Fort Ord, California." In 20th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609-pdb.179.0368-377.

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McLaughlin, Peter P., Kenneth G. Miller, James V. Browning, and Peter J. Sugarman. "PALYNOLOGICAL CONSTRAINTS ON THE STRATIGRAPHY OF THE MAGOTHY FORMATION (CRETACEOUS), NEW JERSEY AND DELAWARE, AND IMPLICATIONS FOR INTERSTATE AQUIFER CORRELATION." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287774.

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Ullah, Saif, Mohammed Y. Ali, Muhammad A. Iqbal, Fateh Bouchaala, and Hakim Saibi. "Structure and stratigraphy of Al Jaww Plain, southeastern Al Ain, United Arab Emirates: Implications for aquifer systems and mantle thrust sheets." In Seventh International Conference on Engineering Geophysics, Al Ain, UAE, 16–19 October 2023. Society of Exploration Geophysicists, 2024. http://dx.doi.org/10.1190/iceg2023-057.1.

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Ibrahim, Shrief, Ahmed Elshafei, M. Fathy, et al. "Extensive Development of Highly Diverse and Multi-Reservoir Field Using Numerical/Analytical Modeling Yields Significant Production and Recovery Boosts in Western Desert, Egypt." In Mediterranean Offshore Conference. SPE, 2024. http://dx.doi.org/10.2118/223201-ms.

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Abstract The good characterization of reservoir properties and extensions simplifies its development plan including appraisal/infill drilling, completion type, and reserves estimation, especially, in fields with multi-layered reservoirs characterized by complicated geology environment where abrupt changes in stratigraphy are expected in vertical and lateral directions. And all those layers need to be developed at the same time with different completion type causing surface complexities, which makes the challenges of field development plans reach its peak. This paper will demonstrate the develo
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Chapuis, Flavien, and Daniela Zapata Franco. "On an atypical moraine of the Swiss Plateau and the presence of a continuous aquifer between Lausanne Aquitanian grey molasse and Quaternary deposits." In 4th European Regional Conference of IAEG. University of Zagreb Faculty of Civil Engineering, 2024. https://doi.org/10.5592/co/euroengeo.2024.216.

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Switzerland is geographically divided into three geologically differentiated regions linked to the Alpine orogeny: the Alps, the Plateau and the Jura. The Plateau separates the other two entities and constitutes the glacial foreland. From a stratigraphic point of view, it is classically characterised by a sub-horizontal molasse overlaid by Quaternary glacial or periglacial deposits inherited from the Würmian glaciation. The quintessential morainic facies of the northern Alps is the ground moraine, which varies in thickness but is often metric to plurimetric. This moraine has low permeabilities
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Jarvis, Jacob C., Joe C. Yelderman, Stephanie Wong, Wayne Hamilton, and Scooter Radcliffe. "THE IMPORTANCE OF DETAILED STRATIGRAPHY IN ASSESSING ALLUVIAL AQUIFERS." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289537.

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Tu, Jiawei, William Ampomah, Nathan Moodie, et al. "Demonstration Numerical Simulation of Field-Scale CO2 Sequestration Project with Complex Faulting System in San Juan Basin, USA." In SPE Annual Technical Conference and Exhibition. SPE, 2022. http://dx.doi.org/10.2118/210082-ms.

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Abstract San Juan Basin (SJB) is a geologic structural basin located in northwest New Mexico. Comprehensive field-scale reservoir simulation work was performed in finely constructed basin-wide geologic models, targeting sequestering over 120 million metric tons of CO2 for a period of 20 years. Petrophysical properties were populated through well logs and measurements on core samples obtained from nearby wells within the study area. Various critical storage trapping mechanisms were considered. The threshold pressure in delineating AoR is formulated based on guidance provided by the Environmenta
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Reports on the topic "Aquifer Stratigraphy"

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Bobst, A., J. Rose, and J. Berglund. An evaluation of the unconsolidated hydrogeologic units in the south-central Flathead Valley, Montana. Montana Bureau of Mines and Geology, 2022. http://dx.doi.org/10.59691/srlk8303.

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An evaluation of the work that has been done at the BFF site. Stratigraphy (including downhole geophysics) from a 1600 ft well drilled in 2021 into the tertiary sediments underlying the deep aquifer. Water-quality results from wells in the tertiary, deep aquifer, confining layer, and shallow aquifer. Aquifer tests and hydrograph analysis of the shallow aquifer, confining layer, deep aquifer, and tertiary sediments. Evaluation of using TEM and MT surficial geophysical techniques.
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Anderson, S. R., and M. J. Liszewski. Stratigraphy of the unsaturated zone and the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho. Office of Scientific and Technical Information (OSTI), 1997. http://dx.doi.org/10.2172/578514.

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Anderson, S. R., and B. Bowers. Stratigraphy of the unsaturated zone and uppermost part of the Snake River Plain aquifer at test area north, Idaho National Engineering Laboratory, Idaho. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/10183223.

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Hurlow, Hugh A., Paul C. Inkenbrandt, and Trevor H. Schlossnagle. Hydrogeology, Groundwater Chemistry, and Water Budget of Juab Valley, Eastern Juab County, Utah. Utah Geological Survey, 2022. http://dx.doi.org/10.34191/ss-170.

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Juab Valley is a north-south-trending basin in the eastern Basin and Range Province. Juab Valley is bounded on the east by the Wasatch normal fault and the Wasatch Range and San Pitch Mountains, bounded on the west by Long Ridge and the West Hills. Juab Valley is at the southern end of Utah’s Wasatch Front, an area of projected rapid population growth and increased groundwater use. East-west-trending surface-water, groundwater, and water-rights boundaries approximately coincide along the valley’s geographic midline at Levan Ridge, an east-west trending watershed divide that separates the north
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Ardakani, O. H. Organic petrography and thermal maturity of the Paskapoo Formation in the Fox Creek area, west-central Alberta. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330296.

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The Paskapoo Formation, which ranges in age from middle to upper Paleocene, is the major shallow aquifer in Alberta. This study is part of a larger GSC-led study on the potential environmental impact of hydrocarbon development in the Fox Creek area (west-central Alberta) on shallow aquifers. Fox Creek is located near the northern limit of the Paskapoo Formation. In addition to the underlying organic-rich source rocks in the study area, including the Duvernay Formation that is currently exploited for hydrocarbon resources, the Paskapoo Formation contains organic-rich intervals and coal seams. I
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Pugin, A. J. M., S. E. Pullan, and D. R. Sharpe. Seismic reflection data and hydro-stratigraphic implications for Ballantrae-Aurora area buried valley aquifers. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/288542.

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Sharpe, D. R., S. E. Pullan, and G. Gorrell. Geology of the Aurora high-quality stratigraphic reference site and significance to the Yonge Street buried valley aquifer, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/286269.

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Akto, P., Z. Chen, and K. Hu. Evaluation of geothermal resource potential of hot sedimentary aquifers in the Horn River Basin, northeast British Columbia, Canada. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331225.

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This study assesses the geothermal potential of Hot Sedimentary Aquifers underlying the Horn River Basin (HRB) based on analyses of borehole temperatures, geological and production data, core porosity and permeability measurements, and geophysical well logs. The proposed criteria are applied to evaluate the geothermal potential of the Horn River Group (HRG) and sub-HRG formations. Favourable spots are identified and ranked by applying temperature, thickness, porosity, permeability and flow rate mapping. The results show that the HRG and its underlying strata have a good potential of geothermal
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Connell, Sean D. Geologic map of the Albuquerque - Rio Rancho metropolitan area and vicinity, Bernalillo and Sandoval counties, New Mexico. New Mexico Bureau of Geology and Mineral Resources, 2008. http://dx.doi.org/10.58799/gm-78.

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This is the most comprehensive compilation of the geology of the Albuquerque Basin to be printed in 30 years. The area covered by this new compilation, though not as large as the earlier map, is presented at a scale nearly four times the detail (1:50,000 scale compared to the earlier map's 1:190,000 scale). This new geologic map is a compilation of sixteen 7.5-min USGS quadrangle maps and encompasses an area from Tijeras Arroyo on the south to Santa Ana Mesa north of Santa Ana and San Felipe Pueblos, and from the crest of the Sandia Mountains westward across the Rio Grande and onto the Llano d
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Stratigraphy of the unsaturated zone and the Snake River Plain Aquifer at and near the Idaho National Engineering Laboratory, Idaho. US Geological Survey, 1997. http://dx.doi.org/10.3133/wri974183.

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