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Dissertations / Theses on the topic 'Kimmeridgium'

Author: Grafiati

Published: 26 July 2024

Last updated: 31 July 2025

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1

Cäsar, Sebastian [Verfasser], and 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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2

Cäsar, Sebastian Verfasser], and 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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3

Van, der Vyver C. P. "The stratigraphy and ammonite faunas of the Lower Kimmeridgian of Britain." Thesis, Swansea University, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.535648.

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4

MacDonald, Alister C. "Kimmeridgian and Volgian fault-margin sedimentation in the northern North Sea area." Thesis, University of Strathclyde, 1985. http://oleg.lib.strath.ac.uk:80/R/?func=dbin-jump-full&object_id=24323.

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The Upper Jurassic sediments of the East Coast of Sutherland and the South Brae Oilfield were deposited during the late Jurassic taphrogenic episode in which there was rapid subsidence in the grabens and uplift of the adjacent areas. The initiation of coarse-grained sedimentation in the grabens was directly related to an increase in subsidence rates. At Sutherland the most sand-rich sequences were deposited during the cymodoce zone of the Kimmeridgian, immediately after the increase in subsidence rates. Depositional environments varied from a relatively shallow water and sand-rich submarine sl

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5

Wignall, Paul Barry. "The palaeoecology and sedimentology of the Kimmeridgian of England and Northern France." Thesis, University of Birmingham, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.536551.

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The Kimmeridgian of England was characterised by the deposition of a widespread and frequently organic-rich mudrock formation, the Kimmeridge Clay. Significant lateral thickness variations are attributable to active faulting which is occasionally recorded within the sediments as a number--of earthquake-generated structures. The slowest subsidence rates occurred on the London platform and depositional depths increased away from this positive feature both to the north and the south. Organic-rich shales preferentially accumulated in the deeper basinal areas where the thickest sequences accumulate

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6

Williams, Ann Cerys. "Palaeoecological and palaeoenvironmental variations in the Callovian, Oxfordian and Kimmeridgian (Jurassic) of Britain." Thesis, University of Leicester, 1988. http://hdl.handle.net/2381/34984.

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Carbon and oxygen stable isotope analyses have been performed on well preserved calcareous fossils from Callovian, Oxfordian and Kimmeridgian (Jurassic) mudrock facies of Britain. Assemblages of ammonites, bivalves and belemnites have been sampled from the Lower Oxford Clay of the English Midlands, the Kimmeridge Clay of Wiltshire and the Dorset coast, and the Staffin Shale Formation of Skye. In this way it was hoped to cover a wide stratigraphic and geographic range. Carbon isotope stratigraphy reveals a positive excursion in the Callovian, which is interpreted as an oceanic anoxic event. On

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7

Bernard, Pierre. "La plate-forme carbonatée niverno-icaunaise à l'oxfordien supérieur et au kimmeridgien inférieur." Dijon, 1987. http://www.theses.fr/1987DIJOS048.

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8

Bernard, Pierre. "La Plate-forme carbonatée niverno-icaunaise à l'Oxfordien supérieur et au Kimmeridgien inférieur." Grenoble 2 : ANRT, 1988. http://catalogue.bnf.fr/ark:/12148/cb37611865m.

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9

Bernard, Pierre. "La plate-forme carbonatée niverno-icaunaise à l'oxfordien supérieur et au kimmeridgien inférieurTexte imprimé." Dijon, 1988. http://www.theses.fr/1988DIJOS026.

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Les séries d'âge oxfordien supérieur et kimméridgien inférieur de la bordure sud et sud-est du bassin de paris autorisent un découpage lithostratigraphique en huit unités d'extension variable. L'agencement géométrique de celles-ci est directement influencé par la présence d'un important complexe récifal médian et d'une zone à forte subsidence en bordure de Loire. L'étude des phénomènes diagénétiques ayant affecté certains facies ou éléments particuliers permet : de rattacher la diversité faciologique des micrites à la diversité des boues initiales, de mettre en évidence au sommet du calcaire d

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10

Brealey, Simon. "The late Oxfordian to Kimmeridgian history of the Rob Roy and Ivanhoe fields, Outer Moray Firth." Thesis, University College London (University of London), 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.555873.

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11

Taylor, Steve P. "Sequence evaluation of the Kimmeridgian stage and Kimmeridge clay formation : a regional appraisal (UK & UKCS)." Thesis, University of Reading, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.271199.

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12

Zuo, Fanfan [Verfasser]. "Carbonate sedimentology and chemostratigraphy of Kimmeridgian shoal-water deposits in the Lower Saxony Basin of Northern Germany / Fanfan Zuo." Hannover : Gottfried Wilhelm Leibniz Universität Hannover, 2018. http://d-nb.info/1174302607/34.

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13

Hantzpergue, Pierre. "Les Ammonites kimmeridgiennes du haut-fond d'Europe occidentale, Perisphinctidae, Aulacostephanidae, Aspidoceratidae." Grenoble 2 : ANRT, 1987. http://catalogue.bnf.fr/ark:/12148/cb37605806v.

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14

Matos, José Esteves de. "Stratigraphy, sedimentation and oil potential of the Lower Jurassic to Kimmeridgian of the United Arab Emirates : outcrop and subsurface compared." Thesis, University of Aberdeen, 1997. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=120500.

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The Jurassic litho-biostratigraphy is reviewed and Jurassic depositional models are defined in order to clarify some regional stratigraphic uncertainties and to evaluate the hydrocarbon potential of the Jurassic of the United Arab Emirates (UAE). A thick succession of Triassic-Cretaceous shallow-marine carbonates is exposed in Wadi Naqab, southeast of Ras Al Khaimah in the UAE, Musandam Peninsula. The Jurassic, 1310 m thick, is examined using biostratigraphy, sedimentology and sequence stratigraphy and compared with the Abu Dhabi subsurface. Direct composition of the Jurassic foraminiferal bio

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15

Franţescu, Ovidiu Daniel. "Brachyuran decapods (including five new species and one new genus) from Jurassic (Oxfordian-Kimmeridgian) coral reef limestones from Dobrogea, Romania." Kent State University / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=kent1237581989.

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16

Samson, Yann. "Utilisation des foraminifères dans l'estimation des variations bathymétriques des environnements de dépôts marins jurassiques : application au Kimmeridgien de l'Ouest-européen." Paris 6, 1997. http://www.theses.fr/1997PA066174.

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Apres etude critique des techniques d'extraction des foraminiferes, deux protocoles de preparation des echantillons, reproductibles et respectueux des taphocenoses, sont proposes. L'analyse ecologique et morphofonctionnelle des petits foraminiferes actuels et jurassiques montre qu'ils sont lies a 3 super-biotopes ; un outil reproductible d'evaluation des variations bathymetriques dans les milieux marins jurassiques (valide par la confrontation de ses resultats avec ceux, sedimentologiques, macropaleontologiques. . . ) est propose sous deux formes : - un diagramme ternaire (% d'individus des 3

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17

Leinfelder, Reinhold R. "Facies, stratigraphy and paleogeographic analysis of upper? Kimmeridgian to upper Portlandian sediments in the environs of Arruda dos Vinhos, Estremadura, Portugal /." München : F. Pfeil, 1986. http://catalogue.bnf.fr/ark:/12148/cb37429276d.

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18

Boulila, Slah. "Cyclostratigraphie des séries sédimentaires du Jurassique supérieur (Sud-Est de la France, Nord de la Tunisie) : contrôle astro-climatique, implications géochronologiques et séquentielles." Paris 6, 2008. http://www.theses.fr/2008PA066019.

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Une étude cyclostratigraphique à haute résolution a été entreprise, en utilisant les variations de la susceptibilité magnétique (SM), sur trois coupes marneuses oxfordiennes et deux coupes d’alternances marno-calcaires kimméridgiennes du Bassin du Sud-Est de la France. Les séries marneuses oxfordiennes enregistrent avec les plus fortes amplitudes de SM, les cycles d’excentricité à 100 et 405 ka. Les séries d’alternances kimméridgiennes détectent plutôt préférentiellement les cycles de précession. Les durées estimées des zones d’ammonites sont très proches de celles de l’échelle des temps géolo

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19

Hudson, Neville. "The middle Jurassic of New Zealand : a study of the lithostratigraphy and biostratigraphy of the Ururoan, Temaikan and Lower Heterian Stages (?Pliensbachian to ?Kimmeridgian)." Thesis, University of Auckland, 2000. http://hdl.handle.net/2292/2135.

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The lithologic and biostratigraphic successions of Ururoan, Temaikan and Lower - Middle Heterian (?Sinemurian, Pliensbachian - ?Kimmeridgian) strata from southwest Auckland, south Otago and Southland, New Zealand, are described and discussed. A more logical correlation of the lithologic sequence at Port Waikato with that at Te Akau is proposed. Two new formations are introduced for the sequences on the western limb of the Kawhia Regional Syncline, the Whakapatiki Mudstone for the fine grained lower Kirikiri Group strata in the Awakino Valley and the Gribbon Formation for the Rengarenga Group s

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20

MONGENOT, THIERRY. "Etudes petrographiques et geochimiques d'un depot sedimentaire tres riche en soufre organique (orbagnoux, kimmeridgien superieur) : reconstitution paleoenvironnementale - - mecanisme de preservation de la matiere organique -." Orléans, 1998. http://www.theses.fr/1998ORLE2019.

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Les cinq facies carbonates (lamines paralleles ou ondulees, claires et sombres, calcaires massifs) qui composent la formation des laminites bitumineuses d'orbagnoux (france, kimmeridgien superieur), resultent de l'interaction entre l'installation de tapis cyanobacteriens et la decantation de coccolithes. Ces facies se caracterisent par des teneurs en carbone organique tres contrastees (de 0,05 a 8,63%) alors que les valeurs du potentiel petroligene et de l'indice de soufre sont toujours tres elevees (ih : 755 a 966 mg hc/g cot ; is : jusqu'a 854 mg cos/g cot) ; la matiere organique (mo) est de

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21

Boussafir, Mohammed. "Microtexture et structure ultrafine des roches et matieres organiques petroligenes : nature et mode de fossilisation de la matiere organique dans les series organo-sedimentaires cycliques du kimmeridgien d'angleterre." Orléans, 1994. http://www.theses.fr/1994ORLE2006.

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Cette etude a pour objectif fondamental d'etudier l'evolution de la nature et de l'etat de preservation des constituants organiques des argiles noires du kimmeridgien d'angleterre, en relation avec la variation quantitative et qualitative de la matiere organique des differentes cyclicites. L'originalite du present sujet reside dans le fait qu'il integre un nouveau type d'approche petrologique a une reflexion sur la sedimentation et la diagenese precoce de la matiere organique ainsi que sur la problematique des cycles organiques. Les etudes ultrastructurales de la roche et de sa matiere organiq

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22

Adigozalova, Teyyuba. "High-resolution sedimentological, petrographic, and petrophysical analysis of Late Oxfordian - Early Kimmeridgian (?), Ulayyah Member, Hanifa Formation: Insights from behind-the-outcrop core WB-01." Thesis, 2021. http://hdl.handle.net/10754/671358.

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The Hanifa Formation has a high-economic value in Saudi Arabia and many middle-eastern countries where it exists both as a reservoir and source rock. A few examples of the super-giant oil and gas fields that have Hanifa reservoir in the subsurface include Berri and Khurais fields. In this project, an analogue core for Hanifa reservoir facies that was drilled behind-the-outcrop, ~ 150 km south of Riyadh, along the Tuwaiq Mountain escarpment is studied. The main objective of this study is to analyze the vertical facies heterogeneity of Ullayah Member of Hanifa Formation. Thus, for this study sed

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23

Guillaume, Alexandre Renaud Daniel. "Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal)." Master's thesis, 2018. http://hdl.handle.net/10362/58236.

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The Upper Jurassic of Portugal has been globally known for its microfossil vertebrate fauna thanks to the Konzentrat-Lagerstätte of the Guimarota mine, which provided thousands of bone fragments, isolated teeth, and even complete specimens. Other vertebrate microfossil assemblages have been studied around the world. Besides Guimarota, no other Portuguese Jurassic assemblage has been extensively studied. Hereby is presented a revision of the state of the art on Portuguese microvertebrate record, and the first microvertebrate studies on three localities from the Lourinhã Formation (Late Jurassic

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24

Tejo, Yuwono Nahrowi. "Lithostratigraphie, microfacies et analyse de la matiére organique des formations géologiques ( Kimméridgien à Berriasien ) du Jura méridonnal. Région de Seyssel : Ain et Haute Savoie." Phd thesis, 1987. http://tel.archives-ouvertes.fr/tel-00634409.

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Les formations, de plate-forme carbonatée, d'âge Kimémridgien à Berriasien affleurent, de part et d 'autre du synclinal molassique de Seyssel emprunté par la vallée du Rhône, dans les anticlinaux du Gros Foug, à l'Est et du Grand Colombier, à l'Ouest. Dans ces deux structures des coupes détaillées permettent de séparer les différentes formations et d'analyser les variations latérales de faciès. Les études lithostratigraphiques et pétrographiques associées amènent à distinguer, de bas en haut : - la formation des couches à Céphalopodes (Kimméridgien inférieur) et la formation des calcaires de T

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