Bibliografias temáticas / Oxfordium

Literatura científica selecionada sobre o tema "Oxfordium"

Autor: Grafiati
Publicado: 25 de julho de 2024

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Artigos de revistas sobre o assunto "Oxfordium"

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Gröschke, Manfred, e Annette Kossler. "Reineckeiidae of Late Caliovian/Early Oxfordian age from northern Chile". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 211, n.º 1-2 (29 de janeiro de 1999): 31–48. http://dx.doi.org/10.1127/njgpa/211/1999/31.

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Riegraf, Wolfgang. "Planktonic Foraminifers and Radiolarians from Callovian to Oxfordian (Jurassic) Deposits of Southern Germany". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 176, n.º 1 (22 de dezembro de 1987): 91–103. http://dx.doi.org/10.1127/njgpa/176/1987/91.

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Gawlick, Hans-Jürgen, e Hisashi Suzuki. "Stratigraphy of the Strubberg Formation in the Northern Calcareous Alps (Callovian-Oxfordian)". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 211, n.º 3 (23 de abril de 1999): 233–62. http://dx.doi.org/10.1127/njgpa/211/1999/233.

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Helm, Carsten, Markus Reuter e Immo Schülke. "Die Korallenfauna des Korallenooliths (Oxfordium, Oberjura, NW-Deutschland): Zusammensetzung, Stratigraphie und regionale Verbreitung". Paläontologische Zeitschrift 77, n.º 1 (abril de 2003): 77–94. http://dx.doi.org/10.1007/bf03004561.

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Krautter, Manfred. "Gregoryceras aus dem Weißen Jura alpha (Oxfordium) vom "Lochen" bei Balingen (Schwäbische Alb, Baden-Württemberg)". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 76 (5 de abril de 1994): 325–34. http://dx.doi.org/10.1127/jm//76/1994/325.

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Krautter, Manfred. "Gregoryceras aus dem Weißen Jura alpha (Oxfordium) vom "Lochen" bei Balingen (Schwäbische Alb, Baden-Württemberg)". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 76 (5 de abril de 1994): 325–34. http://dx.doi.org/10.1127/jmogv/76/1994/325.

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Krautter, Manfred. "Gregoryceras aus dem Weißen Jura alpha (Oxfordium) vom "Lochen" bei Balingen (Schwäbische Alb, Baden-Württemberg)". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 76 (5 de abril de 1994): 325–34. http://dx.doi.org/10.1127/jm/76/1994/325.

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Helm, Carsten, e Immo Schülke. "Crustaceen-Koprolithen aus dem Korallenoolith (Oxfordium, Niedersächsisches Becken, NW-Deutschland) (Crustacean coprolites trom the Korallenoolith Formation (Lower Saxony Basin, Oxtordian, NW Germany))". Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2004, n.º 8 (20 de agosto de 2004): 496–512. http://dx.doi.org/10.1127/njgpm/2004/2004/496.

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Gawlick, Hans-Jürgen, Wolfgang Janauschek, Sigrid Missoni, Volker Diersche e Heinrich Zankl. "Facies, stratigraghy and component analysis of polymict mass-flow deposits in Jurassic cherty sediments (Callovian - Oxfordian) of the Büchsenkopf in the Nationalpark Berchtesgaden and their significance for the tectonic and paleogeographic interpretation of the Berchtesgaden Calcareous Alps (Germany)". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 228, n.º 2 (28 de maio de 2003): 275–304. http://dx.doi.org/10.1127/njgpa/228/2003/275.

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Melendez, Guillermo. "Oxfordian". Geobios 27 (dezembro de 1994): 761–65. http://dx.doi.org/10.1016/s0016-6995(94)80243-2.

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Teses / dissertações sobre o assunto "Oxfordium"

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Rais, Pauline Sophie Claudine. "Evidence for a major paleoceanographic reorganization during the Late Jurassic : insights from sedimentology and geochemistry /". Zürich : ETH, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=16932.

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Reyle, Michael. "Fazies- und Beckenentwicklung im Oxfordium (Oberjura) des zentralen Lusitanischen Beckens (Portugal)". [S.l. : s.n.], 2004. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB11103981.

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Laternser, Ralf. "Oberjurassische Korallenriffe von Nordostfrankreich (Lothringen) und Südwestdeutschland". [S.l. : s.n.], 2001. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB9372874.

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Cäsar, Sebastian [Verfasser], e Christian [Akademischer Betreuer] Betzler. "Sedimentologie und Sequenzstratigraphie oberjurassischer Karbonate von Norddeutschland (Oxfordium, Kimmeridgium, Niedersächsisches Becken) / Sebastian Cäsar. Betreuer: Christian Betzler". Hamburg : Staats- und Universitätsbibliothek Hamburg, 2012. http://d-nb.info/1025150937/34.

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Cäsar, Sebastian Verfasser], e Christian [Akademischer Betreuer] [Betzler. "Sedimentologie und Sequenzstratigraphie oberjurassischer Karbonate von Norddeutschland (Oxfordium, Kimmeridgium, Niedersächsisches Becken) / Sebastian Cäsar. Betreuer: Christian Betzler". Hamburg : Staats- und Universitätsbibliothek Hamburg, 2012. http://nbn-resolving.de/urn:nbn:de:gbv:18-57862.

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Mahjoub, Mohamed. "Modélisation du couplage endommagement-perméabilité dans les géomatériaux anisotropes. Application aux ouvrages souterrains du site de Bure". Thesis, Paris Sciences et Lettres (ComUE), 2017. http://www.theses.fr/2017PSLEM043/document.

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Le but de cette thèse est de mettre en place un nouveau modèle de comportement hydromécanique permettant de prendre en compte les anisotropies initiale et induite et l'impact de l'endommagement mécanique sur la perméabilité. Afin de construire ce modèle, une nouvelle approche de modélisation permettant d'étendre les lois de comportement mécaniques des matériaux isotropes aux matériaux anisotropes est développée. Cette approche, employée dans le cadre des milieux continus à variables internes, est utilisée pour construire une loi de comportement elasto-viscoplastique qui distingue les régimes de sollicitation en compression et en traction. Un tenseur de second ordre est introduit pour décrire l'anisotropie induite suite à des sollicitations de traction et une variable interne scalaire est utilisée pour traduire le durcissement/adoucissement du matériau suite à des sollicitations de compression. Sous des sollicitations complexes, ces deux mécanismes sont couplés et l'effet de fermeture/réouverture des fissures est traité. Le couplage endommagement-perméabilité est ensuite modélisé par l'introduction d'une loi phénoménologique reliant la perméabilité intrinsèque du matériau aux variables internes de la mécanique.Ce modèle a été appliqué dans le cas des ouvrages souterrains du site de Bure afin de comprendre les mécanismes d'altération des propriétés hydromécaniques autour des galeries et des alvéoles de stockage causée non seulement par les opérations de creusement mais également par les surpressions dues à la production d'hydrogène gazeux suite à la corrosion des parties métalliques des modules de déchets
This thesis aims to introduce a new hydromechanical constitutive model taking into account both initial and induced anisotropies and the impact of the mechanical damage on the permeability. To build this model, a new modeling approach is developed allowing the extension of mechanical behavior laws from isotropic materials to transversely isotropic materials. This approach is used, within the framework of continuous media with internal variables, to propose an elasto-viscoplastic behavior law that distinguishes between compressive and tensile loading regimes. A second order tensor is introduced to describe the induced anisotropy due to tensile loadings, and a scalar internal variable is employed to account for hardening and softeningof the material due to compressive loadings. Under complex loadings, these two mechanisms are coupled, and the effect of cracks closing/reopening is taken into consideration. The damage-permeability coupling is modeled by the introduction of a phenomenological law linking the material intrinsic permeability to the mechanical internal variables.The developed model is applied to the case of the underground drifts of Bure site in order to better understand the mechanisms of hydromechanical properties alteration, around drifts and storing cells. Not only the impact of the excavation operations is considered but also the consequences of the overpressures caused by the produced hydrogen due to the corrosion of the metallic parts of nuclear waste containers
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Collin, Pierre-Yves. "Environnements, géochimie et processus de formation de séries condensées au Callovo-Oxfordien : du Bassin de Paris à des considérations globales". Dijon, 2000. http://www.theses.fr/2000DIJOS092.

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Mélendez, Hevia Guillermo. "El Oxfordiense en el sector central de la Cordillera Ibérica, provincias de Zaragoza y Terúel /". [Zaragoza] : [Terúel] : Institución Fernando el Católico ; Instituto de estudios turolenses, 1989. http://catalogue.bnf.fr/ark:/12148/cb35702465f.

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Mahjoub, Mohamed. "Modélisation du couplage endommagement-perméabilité dans les géomatériaux anisotropes. Application aux ouvrages souterrains du site de Bure". Electronic Thesis or Diss., Paris Sciences et Lettres (ComUE), 2017. http://www.theses.fr/2017PSLEM043.

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Le but de cette thèse est de mettre en place un nouveau modèle de comportement hydromécanique permettant de prendre en compte les anisotropies initiale et induite et l'impact de l'endommagement mécanique sur la perméabilité. Afin de construire ce modèle, une nouvelle approche de modélisation permettant d'étendre les lois de comportement mécaniques des matériaux isotropes aux matériaux anisotropes est développée. Cette approche, employée dans le cadre des milieux continus à variables internes, est utilisée pour construire une loi de comportement elasto-viscoplastique qui distingue les régimes de sollicitation en compression et en traction. Un tenseur de second ordre est introduit pour décrire l'anisotropie induite suite à des sollicitations de traction et une variable interne scalaire est utilisée pour traduire le durcissement/adoucissement du matériau suite à des sollicitations de compression. Sous des sollicitations complexes, ces deux mécanismes sont couplés et l'effet de fermeture/réouverture des fissures est traité. Le couplage endommagement-perméabilité est ensuite modélisé par l'introduction d'une loi phénoménologique reliant la perméabilité intrinsèque du matériau aux variables internes de la mécanique.Ce modèle a été appliqué dans le cas des ouvrages souterrains du site de Bure afin de comprendre les mécanismes d'altération des propriétés hydromécaniques autour des galeries et des alvéoles de stockage causée non seulement par les opérations de creusement mais également par les surpressions dues à la production d'hydrogène gazeux suite à la corrosion des parties métalliques des modules de déchets
This thesis aims to introduce a new hydromechanical constitutive model taking into account both initial and induced anisotropies and the impact of the mechanical damage on the permeability. To build this model, a new modeling approach is developed allowing the extension of mechanical behavior laws from isotropic materials to transversely isotropic materials. This approach is used, within the framework of continuous media with internal variables, to propose an elasto-viscoplastic behavior law that distinguishes between compressive and tensile loading regimes. A second order tensor is introduced to describe the induced anisotropy due to tensile loadings, and a scalar internal variable is employed to account for hardening and softeningof the material due to compressive loadings. Under complex loadings, these two mechanisms are coupled, and the effect of cracks closing/reopening is taken into consideration. The damage-permeability coupling is modeled by the introduction of a phenomenological law linking the material intrinsic permeability to the mechanical internal variables.The developed model is applied to the case of the underground drifts of Bure site in order to better understand the mechanisms of hydromechanical properties alteration, around drifts and storing cells. Not only the impact of the excavation operations is considered but also the consequences of the overpressures caused by the produced hydrogen due to the corrosion of the metallic parts of nuclear waste containers
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Aburto, Mardones Danitza. "Filtrage géostatistique de données géophysiques en vue de la cartographie de l’impédance d’une formation argileuse : exemple du Callovo-Oxfordien de Meuse". Thesis, Paris, ENMP, 2012. http://www.theses.fr/2012ENMP0012/document.

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Dans le cadre de recherches menées par l'ANDRA, qui visent à évaluer la faisabilité de créer un stockage de déchets radioactifs dans la formation argileuse du Callovo Oxfordien, cette thèse s'intéresse à deux étapes indispensables pour obtenir une image 3D du sous sol. La première étape concerne la cartographie de la géométrie de la formation. Celle-ci est déterminée à partir de temps pointés le long de profils sismiques, orientés suivant deux directions principales. Aux intersections, les valeurs enregistrées par deux profils sont différentes. Le faible nombre d'intersections ne permettant pas une étude détaillée du comportement spatial de ces différences, elles sont analysées par le biais du pseudo variogramme croisé. L'analyse variographique permet de choisir un modèle cohérent pour l'ensemble des profils. À partir de ce modèle une estimation du temps corrigée est présentée. La deuxième étape concerne l'étude de l'impédance, variable liée aux propriétés intrinsèques de la roche. Deux types de mesure sont disponibles. D'une part l'impédance sismique résultant de l'inversion géophysique de l'amplitude enregistrée le long de profils de sismique réflexion est largement étendue dans la zone d'intérêt. D'autre part, l'impédance log, résultant du produit de la densité de la roche et de la vitesse des ondes P, n'est connue uniquement dans quelques puits. Le comportement spatial bivariable, le long de la direction verticale, a permis de formuler l'hypothèse suivante : chaque mesure d'impédance est décomposée en une somme d'une variable Z (commune aux deux mesures) et d'un résidu différent pour chaque mesure. Sous certaines hypothèses supplémentaires, il est possible d'estimer la composante commune sur l'ensemble des sections sismiques. En complément à ces études, d'autres points ont été évoqués, par exemple la correspondance entre procédés géophysiques et géostatistiques, ou la prise en compte d'incertitude sur les amplitudes
In the framework of researches carried out by ANDRA (the French agency for nuclear waste), which aim at evaluating the feasibility of creating a repository of radioactive waste in the Callovo Oxfordian clay formation. This thesis studies two key steps to obtain a 3D image of the formation: its geometry and its internal heterogeneity. The geometry of the sedimentary formation is determined from seismic time picking along profiles. These profiles are oriented along two main directions. At the intersections, the values registered by two profiles are different. The low number of intersections does not allow a precise study of the spatial behavior of these differences; they are analyzed via the pseudo-cross-variogram. The variography analysis allows the choice of a coherent model for all the profiles, from which an estimation of the corrected time is presented. The internal heterogeneity is performed through the study of the impedance, a variable linked to the intrinsic properties of the rock. Two types of measurements are available. On one hand, the seismic impedance resulting from the geophysical inversion of the amplitude recorded along seismic reflection profiles is densely distributed in the area of interest. On the other hand, the impedance log, resulting from the product of rock density and P wave velocity, is known at only few wells. Bivariate spatial behavior along the vertical direction has allowed the formulation of the following hypothesis: each impedance measurement can be decomposed into a sum of a variable Z (common to both measures) and a residual specific to each measure. Under certain supplementary hypotheses, it is possible to estimate the common component along the seismic sections. Some complements to these studies are mentioned, for example the correspondence between geophysical and geostatistical methods or the consideration of uncertainty in the amplitudes
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Livros sobre o assunto "Oxfordium"

1

Herrmann, Regina. Entwicklung einer oberjurassischen Karbonatplattform: Biofazies, Riffe und Sedimentologie im Oxfordium der Zentralen Dobrogea (Ost-Rumänien). Berlin: Fachbereich Geowissenschaften. FU Berlin, 1996.

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2

Kästle, Bernhard. Fauna und Fazies der kondensierten Sedimente des Dogger und Malm (Bajocium bis Oxfordium) im südlichen Frankenjura. München: F. Pfeil, 1990.

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3

Helm, Carsten. Riffe und fazielle Entwicklung der florigemma-Bank (Korallenoolith, Oxfordium) im Süntel und östlichen Wesergebirge (NW-Deutschland). Hannover, Germany: Institut für Geologie und Paläontologie der Universität Hannover, 2005.

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4

Remsu, Olev. Armastusega Oxfordi. Tallinn: "Eesti Raamat", 1991.

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5

Iván, Andrassew, ed. Róna Péter: Miskolctól Oxfordig. Budapest: Noran Libro, 2012.

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De Vere as Shakespeare: An Oxfordian reading of the canon. Jefferson, N.C: McFarland & Co., 2006.

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7

Sewell, Byron W. The Carrollian tales of Inspector Spectre: R.I.P. (Restless in pieces) and the Oxfordic oracle. Westport: Evertype, 2011.

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8

Hedinger, A. S. Upper Jurassic (Oxfordian-Volgian) foraminifera from the Husky Formation, Aklavik Range, District of Mackenzie, Northwest Territories. Ottawa, Ont: Geological Survey of Canada, 1993.

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9

Gygi, Reinhart A. Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany. Basel: Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7778-7.

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Insalaco, Enzo. A sedimentological and palaecological study of Oxfordian (Upper Jurassic) coral-dominated reefal carbonates in Western Europe. Birmingham: University of Birmingham, 1995.

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Capítulos de livros sobre o assunto "Oxfordium"

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Liu, Zaobao, Jianfu Shao e Ying Xu. "Water Saturation Induced Strength Degradation of Callovo-Oxfordian Claystone". In Springer Series in Geomechanics and Geoengineering, 11–17. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-56397-8_2.

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2

Gens, A., M. Mánica, J. Vaunat e D. F. Ruiz. "Modelling the Mechanical Behaviour of Callovo-Oxfordian Argillite. Formulation and Application". In Advances in Laboratory Testing and Modelling of Soils and Shales (ATMSS), 37–44. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-52773-4_4.

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Trammer, J. "Ecologic History of the Oxfordian Sponge Assemblage in the Polish Jura Chain". In Fossil and Recent Sponges, 506–15. Berlin, Heidelberg: Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-75656-6_42.

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Vu, M. N., M. Souley, M. Alonso, Jean Vaunat, Antonio Gens, C. Plua, C. De Lesquen e G. Armand. "Creep Effects on the Thermo-Hydro-Mechanical Responses of Callovo-Oxfordian Claystone". In Challenges and Innovations in Geomechanics, 663–71. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-64514-4_69.

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Pellenard, Pierre, Romain Tramoy, Marine Cornuault, Emmanuelle Pucéat, Anna-Chiara Bartolini, Emilia Huret, Mathieu Martinez, Dominique Fortwengler, Didier Marchand e Jacques Thierry. "Carbon and Oxygen Isotope Signals from the Callovian–Oxfordian in French Sedimentary Basins". In Springer Geology, 865–67. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_163.

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Wierzbowski, Andrzej, e Bronisław A. Matyja. "On the Proposed Oxfordian–Kimmeridgian (Upper Jurassic) Boundary Stratotype and Its Potential for Correlation". In Springer Geology, 287–90. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_58.

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Domenico, Gilamichael Kidanemariam. "Upper Jurassic (Oxfordian—Kimmeridgian) Benthic Foraminifera and Algae from the Blue Nile Basin, Ethiopia". In Selected Studies in Geomorphology, Sedimentology, and Geochemistry, 189–93. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-43744-1_37.

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Pardoen, B., S. Levasseur e F. Collin. "Using Shear Strain Localisation to Model the Fracturing Around Gallery in Unsaturated Callovo-Oxfordian Claystone". In Springer Series in Geomechanics and Geoengineering, 285–91. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-13506-9_41.

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Pellenard, Pierre, Anna-Chiara Bartolini, Slah Boulila, Pierre-Yves Collin, Dominique Fortwengler, Bruno Galbrun, Silvia Gardin et al. "Integrated Stratigraphy of the Potential Candidate Oxfordian GSSP at Thuoux and Saint-Pierre d’Argençon (France)". In Springer Geology, 271–75. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_55.

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Gygi, Reinhart A. "Introduction". In Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany, 11–18. Basel: Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7778-7_1.

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Trabalhos de conferências sobre o assunto "Oxfordium"

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Belmokhtar, M., P. Delage, S. Ghabezloo e N. Conil. "Poroelastic Investigation of the Callovo-Oxfordian Claystone". In Sixth Biot Conference on Poromechanics. Reston, VA: American Society of Civil Engineers, 2017. http://dx.doi.org/10.1061/9780784480779.103.

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Kanakova, K. I., M. S. Kanakov e S. M. Ibragimova. "GEOLOGY ASPECTS OF CALLOVIAN AND OXFORDIAN DEPOSITS". In All-Russian Youth Scientific Conference with the Participation of Foreign Scientists Trofimuk Readings - 2021. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1251-2-138-141.

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This work is devoted to the development of a technique for automatic identification of lithological types according to well logging data in terrigenous deposits of the J1 horizon in the south of the Tomsk region.
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Talandier, J., F. Skoczylas, B. M. Krooss e M. Prat. "Gas Migration into Low Permeability Callovo-Oxfordian Argillite". In 2nd EAGE International Conference on Fault and Top Seals - From Pore to Basin Scale 2009. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609.20147163.

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Didier, M., J. Talandier, P. Berne e L. Charlet. "Hydrogen Gas Transfer Experiments within Callovo- Oxfordian Clayrock". In 3rd EAGE Shale Workshop - Shale Physics and Shale Chemistry. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143924.

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Wang, X. R., H. Shao, J. Hesser, C. L. Zhang, W. Q. Wang e O. Koditz. "Modeling of Laboratory Heating Experiment on Saturated Callovo-Oxfordian". In International Workshop on Geomechanics and Energy. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20131944.

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6

Belmokhtar, Malik, Pierre Delage, Siavash Ghabezloo e Nathalie Conil. "Thermal Behaviour and Creep of the Callovo-Oxfordian Claystone". In Sixth Biot Conference on Poromechanics. Reston, VA: American Society of Civil Engineers, 2017. http://dx.doi.org/10.1061/9780784480779.104.

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7

Tang, Chao-Sheng, Anh-Minh Tang, Yu-Jun Cui, Pierre Delage, Bin Shi e Christian Schroeder. "Investigating the Microstructure of Compacted Crushed Callovo-Oxfordian Argillite". In GeoShanghai International Conference 2010. Reston, VA: American Society of Civil Engineers, 2010. http://dx.doi.org/10.1061/41101(374)28.

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Poppelreiter, M. C., W. Kolkmann, H. Hordijk e M. Stevanovich. "Regional Settings and Characteristics of an Oxfordian Hot Shale". In Fourth Arabian Plate Geology Workshop. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142802.

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9

Zaychikova, Ekaterina V. "Biostratigraphy of the upper jurassic of the Verkh-Tarskaya drilling area (South of Western Siberia in foraminifera)". In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-009.

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The study of the taxonomic composition of foraminifera in the wells of the Verkh-Tarskaya drilling area formed the basis of this study. This made it possible to clarify the content of the complexes and trace the zones and layers with foraminifera. The biostratigraphic characteristics of the middle oxfordian-lower volgian sediments are also presented in the work, and changes in the taxonomic composition and structure of foraminifera complexes from wells in the Verkh-Tarsky district.
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"The Oxfordian Ichnology of Cap-Ghir, Western High Atlas mrocco". In 4th International Conference on Engineering and Applied Natural Sciences ICEANS 2023. All Sciences Academy, 2023. http://dx.doi.org/10.59287/as-proceedings.319.

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Relatórios de organizações sobre o assunto "Oxfordium"

1

Hedinger, A. S. Upper Jurassic (Oxfordian-Volgian) Foraminifera from the Husky Formation, Aklavik Range, District of Mackenzie, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/41746.

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2

Poulton, T. P. Jurassic [oxfordian] ammonites from the Fernie formation of western Canada: a giant peltoceratinid,and cardioceras canadense whiteaves. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127722.

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3

Poulton, T. P., J. H. Callomon e R. L. Hall. Bathonian Through Oxfordian [Middle and Upper Jurassic] Marine Macrofossil Assemblages and Correlations, Bowser Lake Group, West - Central Spatsizi map area, northwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132497.

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4

Dixon, J. Jurassic - Lower Cretaceous (Oxfordian to Lower Aptian) Strata, Yukon Territory - Northwest Territories (a contribution to the Geological Atlas of the Northern Canadian Mainland Sedimentary Basin). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215466.

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