Relevant bibliographies by topics / Glauconitic clay

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  1. Journal articles
  2. Dissertations / Theses
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  4. Conference papers

Academic literature on the topic 'Glauconitic clay'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Glauconitic clay"

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Huggett, J. M., B. Laenen, and N. Vandenberghe. "Green clays from the Lower Oligocene of Aardebrug, Belgium: a re-evaluation." Clay Minerals 31, no. 4 (1996): 557–62. http://dx.doi.org/10.1180/claymin.1996.031.4.13.

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Porrenga (1968) described the green clays from the Lower Oligocene of Aardebrug, east of Leuven (Louvain) in Belgium as glauconitic illite, a mineral intermediate in chemistry between glauconite and illite, and presumed this clay to be neoformed, though the mode of origin is not discussed. Notably, most of the section from which Porrenga obtained his sample of 'glauconitic illite' is nonmarine. Non-marine glauconites are rare in the literature and there is no standard terminology. Parry and Reeves (1966) reported green pellets of 10 Å clay from recent sediments at Lake Mound, Texas, but with n
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Baker, J. C. "Green ferric clay in non-marine sandstones of the Rewan Group, southern Bowen Basin, Eastern Australia." Clay Minerals 32, no. 4 (1997): 499–506. http://dx.doi.org/10.1180/claymin.1997.032.4.01.

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AbstractAccessory green ferric clay occurs in fluvial litharenites of the Early Triassic Rewan Group. Although resembling glauconitic minerals in thin-section, electron microprobe analyses indicate that the green ferric clay is mainly ferric illite. The ferric illite may have formed in a small hypersaline lake or well drained, flood-plain soil, and its presence in the Rewan Group cannot be used to support a notion that the unit is partly marine influenced. Identification of the ferric illite by electron microprobe analysis shows that some green ferric clays, particularly those that resemble gl
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Roy Choudhury, Tathagata, Pragya Singh, Arpita Chakraborty, and Santanu Banerjee. "Authigenic Fe Mineralization in Shallow to Marginal Marine Environments: A Case Study from the Late Paleocene—Early Eocene Cambay Shale Formation." Minerals 13, no. 5 (2023): 646. http://dx.doi.org/10.3390/min13050646.

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The late Paleocene–early Eocene warm greenhouse conditions, characterized by elevated pCO2 levels in the atmosphere and a dramatic increase in sea surface temperature, prompted abundant authigenic glauconite formation within the shallow marine sediments worldwide by lowering the net sedimentation rate, increasing organic productivity and expanding the oxygen minimum zones to shallow oceans. The early Eocene marginal marine Cambay Shale Formation experienced episodes of marine inundation represented by limestone–green shale alternations. The shales host abundant authigenic light-green, dark-gre
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Lebedeva, Marina, Alexander Makeev, Alexey Rusakov, et al. "Landscape Dynamics in the Caspian Lowlands Since the Last Deglaciation Reconstructed From the Pedosedimentary Sequence of Srednaya Akhtuba, Southern Russia." Geosciences 8, no. 12 (2018): 492. http://dx.doi.org/10.3390/geosciences8120492.

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Surface Kastanozem of the Lower Volga area was first studied as a part of the pedocomplex, with the lower part (148–160 cm) formed in Early Khvalynian Chocolate clays (13–15 ka), the middle part (100–148 cm) in a mixed clay-loess sediment sand, and the upper part (0–100 cm) in loess. This resulted from local aeolian transport, with the source material derived from the rewinding of marine sediments. They are enriched in aggregates of Chocolate clays and glauconitic grains of a fine sand-course silt size and have similar contents of clay minerals. The high salinity of similar types evidences mar
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HASSAN, M. "Glauconitic clay of El Gidida, Egypt: evaluation and surface modification." Applied Clay Science 27, no. 3-4 (2004): 219–22. http://dx.doi.org/10.1016/j.clay.2004.04.002.

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Giresse, Pierre. "Quaternary Glauconitization on Gulf of Guinea, Glauconite Factory: Overview of and New Data on Tropical Atlantic Continental Shelves and Deep Slopes." Minerals 12, no. 7 (2022): 908. http://dx.doi.org/10.3390/min12070908.

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For a long time, particular attention was paid to glauconitization in the surficial sediments lying on the outer continental shelves of present oceans. Subsequently, the processes observed and analyzed may have served as models for studies of glauconite in Cenozoic or even Mesozoic shelf deposits. Access to the sedimentary domains of deep oceans, particularly those of contouritic accumulation fields, has made it possible to discover unexpected processes of glauconitization. Thus, the long-term prevalence of control using fairly high-temperature water has become obsolete, and the prerequisite i
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May, James H., Wayne C. Isphording, David Patrick, David R. Williamson, and James E. Lyles. "Stratigraphic and Geochemical Evidence for the Alteration of Calcareous Glauconitic Marine Sediments to Calcium Bentonite." Environmental & Engineering Geoscience 28, no. 2 (2021): 215–31. http://dx.doi.org/10.2113/eeg-d-20-00116.

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ABSTRACT Calcium bentonite mined in Smith County, Mississippi, has been reported in numerous publications to be derived from the weathering of volcanic ash. These interpretations were based on the bentonite having similar properties to bentonites actually formed from volcanic precursors. No recent detailed stratigraphic mapping in combination with modern laboratory analyses had been conducted for this area. Calcium bentonite, found at Olmstead, Illinois, in contrast, formed in situ from the weathering of biotite, glauconite, quartz, and other materials found in shallow calcareous marine deposi
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Nasibullin, B. A., A. Ya Oleshko, A. B. Zmievskiy, E. I. Baholdina та I. V. Savitskiy. "Сравнительная оценка результативности использования бентонитовых и глауконитовых глин на структурно-функциональные характеристики печени крыс с алкогольным гепатитом = Comparative evaluation of the use of bentonite and glauconitic clay on the structural and functional characteristics of rat liver with alcoholic hepatitis". Journal of Education, Health and Sport 5, № 2 (2015): 165–72. https://doi.org/10.5281/zenodo.15716.

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<strong>Nasibullin B A, Oleshko A Ya, Zmievskiy A B, Baholdina E I, Savitskiy I V. </strong><strong>Сравнительная</strong> <strong>оценка</strong> <strong>результативности</strong> <strong>использования</strong> <strong>бентонитовых</strong> <strong>и</strong> <strong>глауконитовых</strong> <strong>глин</strong> <strong>на</strong> <strong>структурно</strong><strong>-</strong><strong>функциональные</strong> <strong>характеристики</strong> <strong>печени</strong> <strong>крыс</strong> <strong>с</strong> <strong>алкогольным</strong> <strong>гепатитом</strong><strong> = Comparative evaluation of
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Dubey, Nageshwar, and B. K. Chatterjee. "Physical and biological changes across the Jurassic/Cretaceous Boundary in northwestern Kutch Basin." Journal of Palaeosciences 46, no. (1-2) (1997): 141–48. http://dx.doi.org/10.54991/jop.1997.1328.

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In the northwestern part of the Kutch Basin, Lower Cretaceous shales and trigonid-bearing / bioturbated/barren sandstones, overlie the glauconitic Upper Tithonian Virgatosphinctes-bearing "Umia Ammonite Bed" (138±20 Ma). During the lithofacies studies of this sequence, lithology, physical and biogenic sedimentary structures, bed geometry, palaeocurrent and fossil contents were given special attention. Laboratory investigations of heavy minerals, rock fragments and clay minerals revealed two distinct assemblages, one for the lower (Jurassic) and other for the upper (Cretaceous) part of the sequ
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Gazda, Lucjan, and Małgorzata Franus. "Physicochemical and mechanical properties of selected cohesive soils of Lublin region used in waterproofing applications." Budownictwo i Architektura 13, no. 2 (2014): 017–24. http://dx.doi.org/10.35784/bud-arch.1843.

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In this paper preliminary characteristics of selected cohesive soils of Lublin region that can be used in waterproofing applications in geotechnics and constructions is presented. The investigations and analysis were made according to the applicability criteria of materials used as mineral waterproofing barriers which have been elaborated in the last years in Institute of Building Techniques. On the basis of petrographical, mineral, filtering, structural and mechanical properties, the usability of slits from Bychawa and Łążek Ordynacki and powdery clay from Markowicze was confirmed, whereas gl
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Dissertations / Theses on the topic "Glauconitic clay"

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Udgata, Devi Bhagabati Prasad. "DEPOSITIONAL AND STRATIGRAPHIC SIGNIFICANCE OF MARINE, GREEN-CLAY, MINERAL FACIES IN THE LOWER-MIDDLE MISSISSIPPIAN BORDEN AND FORT PAYNE FORMATIONS, WESTERN APPALACHIAN AND EASTERN ILLINOIS BASINS, KENTUCKY." UKnowledge, 2011. http://uknowledge.uky.edu/gradschool_diss/808.

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Detailed study of strata associated with the glauconite-rich Floyds Knob Bed in the western Appalachian and eastern Illinois basins have corroborated previous interpretations that the unit is a widespread, largely synchronous marker horizon. However, in some areas there are multiple glauconite beds; in others a distinct bed is lacking, but the glauconite is dispersed throughout many beds, forming an interval rather than a distinct bed. In Kentucky and adjacent states, the Floyds Knob interval, in upper parts of the Lower-Middle Mississippian Borden-Grainger delta sequence and in lower parts of
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Book chapters on the topic "Glauconitic clay"

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Zwingmann, Horst. "Clays and Glauconites (K–Ar/Ar–Ar)." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6326-5_37-1.

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Zwingmann, Horst. "Clays and Glauconites (K–Ar/Ar–Ar)." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_37.

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"glauconite clay." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_71270.

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Corrêa, Iran Carlos Stalliviere. "Outros Minerais Autigênicos no Ambiente Marinho." In Recursos Minerais Marinhos. Sociedade Brasileira de Geofísica - SBGf, 2023. http://dx.doi.org/10.22564/sbgfbook.cad5.2023.cap13.

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Existem muitos tipos e formas de depósitos minerais autigênicos no fundo marinho, alguns em maior abundância e, em alguns casos, potencialmente econômicos. Entre este encontram-se os depósitos ferromanganesíferos, fosforíticos, barita marinha e minerais silicatados autigênicos. Aqui serão descritos alguns dos demais minerais autigênicos de importância nos sedimentos do fundo oceânico, tais como glauconita, francolita, zeolita/filipsita, pirita, calcita/aragonita e argilominerais. As zeolitas e argilas mais abundantes, como a esmectita, se formam principalmente a partir da alteração diagenética
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Huggett, J. M. "Minerals: Glauconites and Green Clays." In Reference Module in Earth Systems and Environmental Sciences. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-12-409548-9.02893-1.

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Tardy, Y., and O. Touret. "Hydration Energies of SmectitesA Model for Glauconite, Illite, and Corrensite Formation." In Proceedings of the International Clay Conference Denver, 1985. Clay Minerals Society, 1985. http://dx.doi.org/10.1346/cms-icc-1.6.

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Self-Trail, Jean M., David L. Govoni, Laurel M. Bybell, and Kristina F. Gardner. "Geology and paleontology of Cretaceous and Paleocene sediments of the Cabin Branch, Cabin Creek (Cappy Avenue), and Tinkers Creek outcrops, Prince George’s County, Maryland." In Field Excursions to the Northern Sierra Nevada of California, the Mining Districts of the Sierra Nevada, and Cretaceous and Paleocene Sediments in Maryland, USA. Geological Society of America, 2023. http://dx.doi.org/10.1130/2023.0065(01).

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ABSTRACT This field guide presents a one-day excursion in Prince George’s County, Maryland, USA, and documents the transition across the Cretaceous-Paleogene boundary by examining sediments from the upper Maastrichtian of the Severn Formation to the Paleocene sediments of the Brightseat and Aquia formations. Emphasis is placed on understanding how differences in depositional character and lithostratigraphy are related to changes in both microfossil and macrofossil assemblages. Particular attention is given to the difficulty in distinguishing Upper Cretaceous sediments from lower Paleocene sedi
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Hallam, Tony. "Sea-level changes." In Catastrophes and Lesser Calamities. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780198524977.003.0008.

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In earlier times many geologists clearly became cynical about what they had learned as students about Earth history from their stratigraphy courses. ‘The sea comes in, the sea goes out.’ This is indeed one of the most striking signals that emerges from study of the stratigraphic record in a given region: a succession of marine transgressions and regressions on the continents. Little scientific rigour was, however, applied to the subject, and students were left with no overarching explanation to provide any intellectual stimulation. Since the 1970s things have begun to change for the better, as
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Conference papers on the topic "Glauconitic clay"

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Quinteros, VS, Z. Westgate, K. Vinck, V. Dantal, A. Lindtorp, and M. A. Toma. "Interface Friction Angle of Glauconitic Sands for Pile Design." In Innovative Geotechnologies for Energy Transition. Society for Underwater Technology, 2023. http://dx.doi.org/10.3723/lkri8285.

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The soil-to-steel residual interface friction angle (δres) is an important parameter for designing monopiles. The δres is usually obtained using the ring shear or the interface direct shear box test. To date, there is a limited body of knowledge on interface behaviour of glauconitic soil, and no database or guidelines are available on how to obtain reliable estimates of δres in glauconitic soil Obtaining res can be challenging as the glauconitic soil may behave sand- or clay-like dependent on the degree of particle crushing taking place either in advance of the test as part of the specimen pre
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Abouzaid, Ahmed, Holger Thern, Mohamed Said, Mohammad ElSaqqa, Mohamed Elbastawesy, and Sherin Ghozlan. "Nuclear Magnetic Resonance Logging While Drilling in Complex Lithology – Solution for a Glauconitic Sandstone Reservoir." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2579089-ms.

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ABSTRACT The evaluation of logging data in shaly sand reservoirs can be a challenging task, particularly in the presence of accessory minerals such as glauconite. Accessory minerals affect the measurements of conventional logging tools, thus, introducing large uncertainties for estimated petrophysical properties and reservoir characterization. The application of traditional Gamma Ray and Density-Neutron crossover methods can become unreliable even for the simple objective of differentiating reservoir from non-reservoir zones. This was the situation for many years in the glauconite-rich Upper B
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Westgate, Zack, Chris McMullin, and Don DeGroot. "Glauconite Sand Challenges for US Offshore Wind Development." In ASME 2022 4th International Offshore Wind Technical Conference. American Society of Mechanical Engineers, 2022. http://dx.doi.org/10.1115/iowtc2022-98666.

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Abstract Glauconite sand, otherwise known as ‘greensand’, is a challenging sediment type that can pose significant risks to foundation installation and performance. This is due to its tendency to transform from a stiff, high permeability coarse-grained material to a weak, low permeability fine-grained material due to particle crushing. Glauconite is an iron potassium mica, characteristically green and often found in peloidal form. It forms under reducing conditions within shallow marine depositional environments and has been found in coastal regions of the USA including locations along the Atl
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Aluvihara, Suresh, C. S. Kalpage, P. W. S. K. Bandaranayake, W. M. A. T. Bandara, and Ciprian Chelaru. "Investigations and Analysis of Earth Materials towards the Developments in Some Advanced Chemical and Catalytic Uses." In The 9th International Conference on Advanced Materials and Systems. INCDTP - Leather and Footwear Research Institute (ICPI), Bucharest, Romania, 2022. http://dx.doi.org/10.24264/icams-2022.i.3.

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Earth materials are some sort of valuable resources with some multiples uses in some of industrial purposes and they are obtaining some economical values based upon the demand and the abundance. According to the most of research and experiments that relevant with the characteristics of solid earth materials, mainly there were obtained and disclosed some various outstanding physic-chemical characteristics of a large number of earth materials including the applications of material processing, nano-materials, composite materials and hard materials. In the existing research there were expected to
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Jeanjean, P., and A. Zakeri. "Efficiencies and Challenges in Offshore Wind Foundation Design." In Innovative Geotechnologies for Energy Transition. Society for Underwater Technology, 2023. http://dx.doi.org/10.3723/cnie2258.

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An efficient site-independent, rule-based, four-spring model for the design of monopiles in clays is presented. DSS stress-strain curves are scaled to derive a set of default lateral load, distributed moment, base shear, and base moment soil reaction curves as a function of the soil OCR and plasticity index. The model is used to hindcast seven lateral load tests on monopiles in soils conditions ranging from soft clays to glacial tills and shows good agreement with the measured loads, displacements, and bending moments. The paper also explores challenges related to the geo-materials encountered
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Hathon, Lori A., Michael T. Myers, and William Horvath. "Validating the Extended Thomas-Stieber Model Using A Variety of Imaging Modalities." In 2024 SPWLA 65th Annual Symposium. Society of Petrophysicists and Well Log Analysts, 2024. https://doi.org/10.30632/spwla-2024-0124.

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In thinly bedded, shaly-sand reservoirs, a Thomas-Stieber model is used to quantify volumes of clean sandstone from that of laminar, dispersed, and structural shales. In the absence of a whole core data set, this is done using a log-based volumetric lithologic indicator (i.e., gamma ray) and porosity, which is often inverted from the bulk density data set. The Thomas-Stieber model typically assumes all types of shales have the same properties. This is consistent with observations in the Miocene section of the central Gulf of Mexico, where the model was developed. However, in more heterogeneous
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Netto, Paulo R. A., and Manuel Pozo. "Use of Spectral Gamma Ray and Lithogeochemical Logs Combined With XRD Data to Identify Mg-Clay Mineral Sequences in Barra Velha Formation (BVE) – Lower Cretaceous of the Santos Basin." In 2024 SPWLA 65th Annual Symposium. Society of Petrophysicists and Well Log Analysts, 2024. https://doi.org/10.30632/spwla-2024-0022.

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Natural radioactivity in rocks is usually the result of the presence of natural isotopes: potassium – 40K, uranium – 238U, 234U, 235U, and thorium – 232Th and their decay products. Initially contained in acid igneous rocks, these isotopes are released through weathering processes and subsequently transported to sedimentary sites, where they primarily accumulate by adsorption onto clay mineral particles. Direct measurements of potassium, uranium, and thorium activity in sedimentary rocks provide crucial insights into their geochemistry and mineral content. Methods proposed the use of gamma ray
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Permana, Aziz, Mateos Naiola, Daniel Siregar, et al. "Low Resistivity Reservoir Identification of Gumai Formation Using Weighted Scoring Method in West Benakat, South Sumatra Basin, Indonesia." In SPE Annual Technical Conference and Exhibition. SPE, 2022. http://dx.doi.org/10.2118/210109-ms.

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Abstract The mature oil field of West Benakat is located in the South Sumatra Basin, one of the most hydrocarbon prolific Indonesian tertiary back-arc basins in Indonesia. Since its discovery in 1933, West Benakat Field has been operating and producing oil for nearly nine decades from Talang Akar Formation (TAF) as the main sand reservoir target with good porosity and permeability. Recently, Talang Akar reservoirs have been depleted through massive development programs, whereas more than 290 wells have been drilled for exploration, production, and injection wells. Decreasing oil production pus
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