Bibliografias temáticas / Kimmeridgium

Literatura científica selecionada sobre o tema "Kimmeridgium"

Autor: Grafiati
Publicado: 26 de julho de 2024
Última modificação: 27 de julho de 2024

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Artigos de revistas sobre o assunto "Kimmeridgium"

1

Weiss, Michael. "Neue Ostracoden aus dem Kimmeridgium NW-Deutschlands". Paläontologische Zeitschrift 70, n.º 3-4 (novembro de 1996): 461–74. http://dx.doi.org/10.1007/bf02988085.

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Schudack, M. E. "Some charophytes from the middle dinosaur member of the Tendaguru formation (Upper Jurassic of Tanzania)". Fossil Record 2, n.º 1 (1 de janeiro de 1999): 201–5. http://dx.doi.org/10.1002/mmng.1999.4860020115.

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Abstract. Biostratigraphy and paleoecology of the famous dinosaur beds of Tendaguru Formation, Tanzania, East Africa are still under discussion. Calcareous microfossils have not yet contributed to this question. Four samples from the Middle Dinosaur Member have now yielded charophyte gyrogonites of the species Aclistochara cf. bransonii, Aclistochara cf. minor, Mesochara canellata, and Mesochara harrisi. Considering ammonite datations in under- and overlying members, even their long stratigrapical ranges point to a Kimmeridgian age for the Middle Dinosaur Member of Tendaguru Formation. Salinity tolerances of the species (if autochthonous) suggest a variable environment with partly brackish, partly freshwater influences. Biostratigraphie und Paläoökologie der berühmten Dinosaurier-Fundschichten am Tendaguru Hill in Tansania (Ostafrika) sind bis heute umstritten. Kalkige Mikrofossilien hatten zu dieser Diskussion bisher nicht beigetragen. In vier Proben aus dem Mittleren Dinosauriermergel fanden sich nun Charophyten-Gyrogonite der Arten Aclistochara cf. bransonii, Aclistochara cf. minor, Mesochara canellata und Mesochara harrisi. Trotz generell langer stratigraphischer Reichweiten dieser Arten macht ihr Vorkommen im Zusammenhang mit Ammonitenfunden in unter- und überlagernden Schichten ein Kimmeridgium-Alter des Mittleren Dinosauriermergels wahrscheinlich, während ihre Salinitätstoleranzen (autochthones Vorkommen vorausgesetzt) auf ein wechselhaftes Milieu mit teils schwach brackischen, teils Süßwassereinflüssen hindeuten. doi:10.1002/mmng.1999.4860020115
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Schweigert, Günter, e Gerd Dietl. "Miscellanea aus dem Nusplinger Plattenkalk (Ober-Kimmeridgium, Schwäbische Alb) 7. Fossile Holzkohle". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 88 (18 de abril de 2006): 85–92. http://dx.doi.org/10.1127/jmogv/88/2006/85.

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Schweigert, G., e G. Dietl. "Miscellanea aus dem Nusplinger Plattenkalk (Ober-Kimmeridgium, Schwäbische Alb) 6. Das Spurenfossil Telsonichnus". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 87 (29 de março de 2005): 431–38. http://dx.doi.org/10.1127/jmogv/87/2005/431.

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Schweigert, Günter, Gerd Dietl e Rupert Wild. "Miscellanea aus dem Nusplinger Plattenkalk (Ober-Kimmeridgium, Schwäbische Alb) 3. Ein Speiballen mit Flugsaurierresten". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 83 (17 de abril de 2001): 357–64. http://dx.doi.org/10.1127/jmogv/83/2001/357.

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Schweigert, Günter, e Gerd Dietl. "Aptychen-Formgattung Miscellaneous from the Nusplingen Lithographic Limestone (Upper Kimmeridgian, Swabian Alb) 9. A new form-genus of aptychi". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 90 (25 de março de 2008): 45–55. http://dx.doi.org/10.1127/jmogv/90/2008/45.

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Schweigert, Günter. "Miscellaneous from the Nusplingen Lithographic Limestone (Upper Kimmeridgian, Swabian Alb). 18. Bridgman fractures". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 99 (11 de março de 2017): 545–52. http://dx.doi.org/10.1127/jmogv/99/0018.

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Schweigert, Günter, e Jürgen Härer. "Miscellaneous from the Nusplingen Lithographic Limestone (Upper Kimmeridgian, Swabian Alb). 22. Ammonites with preserved septa". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 103 (11 de abril de 2021): 291–98. http://dx.doi.org/10.1127/jmogv/103/0009.

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Baier, Johannes, e Günter Schweigert. "On the occurrence of Aulacostephanus yo (d'Orbigny) in Swabia (Late Kimmeridgian, SW Germany)". Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2001, n.º 3 (8 de março de 2001): 184–92. http://dx.doi.org/10.1127/njgpm/2001/2001/184.

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Schweigert, Günter, e Gerd Dietl. "Miscellaneous from the Nusplingen Lithographic Limestone (Upper Kimmeridgian, Swabian Alb). 10. Sliding marks and roll marks". Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 91 (14 de abril de 2009): 89–99. http://dx.doi.org/10.1127/jmogv/91/2009/89.

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Teses / dissertações sobre o assunto "Kimmeridgium"

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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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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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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 slope during the early Kimmeridgian to a deeper water sediment starved submarine slope during the early Volgian. The sediments of the South Brae Oilfield were deposited in the channelised part of a submarine fan system which was sourced from a point which lay to the west of the 16/7a-8 well and to the southwest of the 16/7a-12 well. The South Brae sequences are part of a much larger complex which was composed of at least seven different submarine fan systems. Sediment entry points occurred along the western margin of the South Viking Graben from the T-Block in the south to East Brae in the north and each of these fed a submarine fan system. The reservoir sequences will tend to be vertically stacked and spatially restricted in proximal areas and will become less stacked and less restricted distally. Stratigraphically trapped "Brae-like" plays probably exist at the margins of many North Atlantic Continental Shelf grabens. The eastern margins of the Vøring and Træna Basins have especially high prospectivity.
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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 accumulated. Even in the deepest locations storms were able to influence the depositional environment. This is reflected by a range of tempestite beds and by the highly opportunistic character of the benthic fauna which responded to the brief storm-induced oxygenation events. Palaeocommunity analysis indicates that a number of variables were controlling the faunal distribution. Substrate consistency, environmental stability and oxygen levels all interacted to produce a diverse range of community types composed of a few euryoxic, opportunistic molluscs. A major change occurs in the middle of the Upper Kimmeridge Clay when softground faunas are replaced by firmground faunas. This appears to reflect a marked reduction in sedimentation rate related to a sudden increase in aridity at this time. Sandy marginal marine facies were developed on the London Platform throughout much of the Kimmeridgian; they are best seen at outcrop in the cliff sections of the Boulonnais. Facies range from shallow marine glauconitic sandstones with intensive bioturbation and a fauna of large bivalves, to shell-poor shoreface sandstones with well preserved sedimentary structures. Analysis of this latter facies indicates that storms and waves were the two principal sources of hydrodynamic energy. Tides were probably of negligible importance in the Kimmeridgian epeiric seas. Local cyclicity in the Boulonnais sediments appears to be due to small-scale fluctuations of narrow, nearshore facies belts; they are not related to the more ubiquitous shale: mudstone rhythms which characterise the offshore mudrocks. Investigation of eustatic sea level changes indicates a Jurassic highstand of sea level in the Lower Kimmeridgian followed by a slow progressive fall through the Upper Kimmeridgian. The highstand appears to have produced relatively deep water conditions in many epeiric settings throughout the world which led to organic-rich shale formation. Finer scale eustatic sea level changes are more equivocal although a highstand may have occurred in the Eudoxus zone. No substantiating evidence was found for the fine scale eustatic fluctuations recently proposed by the Vail team.
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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 the basis of palaeontological and sedimentological evidence, the Callovian has long been viewed as a time of oxygen deficiency. These views are supported by this, the first detailed isotopic study of the stage. A comparison of the 613 C values of the ammonites and infaunal bivalves reveals a major anomaly, in that the latter show very positive values. Tentative suggestions are put forward to account for this. Oxygen isotope (and hence palaeotemperature) stratigraphy reveals a cooling through the Upper Callovian and Oxfordian, consistant with the "Boreal spread" of Arkell (1956), with a warming into the Lower Kimmeridgian. Palaeotemperature variations within individual assemblages raise important questions about palaeoecology. On the basis of this data, it appears that bivalves previously considered to be nekto - or pseudoplanktonic did not occupy the upper reaches of the water column. Suggestions have been made that ammonites were benthic rather than nektonic, but the evidence presented here implies that this was not the case. Relative to the rest of the assemblage, belemnite temperatures tend to be low, highlighting their migratory nature. Boreal ammonites are found to precipitate their shells in cooler waters than those from the Tethyan Realm. The significance of this, and other factors, in terms of controls on provinciality are discussed.
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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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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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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 de Tonnerre, l'existence locale d'une zone émergée temporaire sous forme de cayes sableuses, d'établir une filiation directe entre boues, pellets et oolites micritiques de cette même formation, de démontrer la nature calcitique initiale des nanoconstituants élémentaires, de préciser, par la précipitation directe, leur origine. L’étude sédimentologique des divers facies répertoriés permet de caractériser quinze milieux élémentaires de dépôt et conduit à proposer un dispositif sédimentaire virtuel de type plate-forme carbonatée insulaire. Celui-ci s'organise entre une plate-forme basse peu profonde, ouverte sur le large, soumise aux apports terrigènes et une plate-forme superficielle, vaste, très peu profonde, à hydrodynamisme variable complexe ou s'individualisent latéralement quatre zones ou domaines à sédimentation tranchée. Les deux séquences régressive et transgressive définies reflètent les phases de comblement et d'approfondissement respectives aux deux mégaséquences du jurassique supérieur
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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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Livros sobre o assunto "Kimmeridgium"

1

Wignall, Paul B. The palaeoecology and sedimentology of the Kimmeridgian of England and northern France. Birmingham: University of Birmingham, 1988.

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2

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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Gygi, Reinhart A. Integrated stratigraphy of the Oxfordian and Kimmeridgian (late Jurassic) in northern Switzerland and adjacent southern Germany. Basel: Birkhäuser, 2000.

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Gygi, Reinhart A. Integrated stratigraphy of the Oxfordian and Kimmeridgian (late Jurassic) in northern Switzerland and adjacent southern Germany. Boston, MA: Birkhäuser, 1999.

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5

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.

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6

Verma, Harish M. Ammoniod Fauna Kimmeridgian (Life Sciences Contributions,). Royal Ontario Museum, 1990.

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7

Integrated Stratigraphy of the Oxfordian and Kimmeridgian in northern Switzerland and adjacent southern Germany. Birkhäuser, 2001.

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8

Gygi, Reinhart A. Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in Northern Switzerland and Adjacent Southern Germany. Birkhauser Verlag, 2013.

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9

Lindgreen, Holger. Elemental and structural changes in illite/smectite mixed-layer clay minerals during diagenesis in Kimmeridgian- Volgian (-Ryazanian) clays in the Central Trough, North Sea, and the Norwegian-Danish Basin. 1991.

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Capítulos de livros sobre o assunto "Kimmeridgium"

1

Sempere, T. "Kimmeridgian? to Paleocene Tectonic Evolution of Bolivia". In Cretaceous Tectonics of the Andes, 168–212. Wiesbaden: Vieweg+Teubner Verlag, 1994. http://dx.doi.org/10.1007/978-3-322-85472-8_4.

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Fowler, M. G., e K. D. McAlpine. "The Egret Member, a Prolific Kimmeridgian Source Rock from Offshore Eastern Canada". In Casebooks in Earth Sciences, 111–30. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-78911-3_7.

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Jaillard, E. "Kimmeridgian to Paleocene Tectonic and Geodynamic Evolution of the Peruvian (and Ecuadorian) Margin". In Cretaceous Tectonics of the Andes, 101–67. Wiesbaden: Vieweg+Teubner Verlag, 1994. http://dx.doi.org/10.1007/978-3-322-85472-8_3.

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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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Sequero, Cristina, Beatriz Bádenas e Marcos Aurell. "Factors Controlling Oncoid Distribution in the Inner Areas of a Late Kimmeridgian Carbonate Ramp (Northeast Spain)". In Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas, 171–74. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01452-0_41.

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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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Gygi, Reinhart A. "Facies analysis". In Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany, 19–30. Basel: Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7778-7_2.

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Gygi, Reinhart A. "Lithostratigraphy". In Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany, 31–68. Basel: Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7778-7_3.

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Gygi, Reinhart A. "Biostratigraphy". In Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany, 69–103. Basel: Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-7778-7_4.

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Trabalhos de conferências sobre o assunto "Kimmeridgium"

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San Miguel, G., M. Aurell, B. Badenas e B. Caline. "Factors Controlling Reef fabric Distribution (Kimmeridgian Ramp, Iberian Basin) - Unravelling Reservoir Heterogeneities". In 77th EAGE Conference and Exhibition 2015. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201412655.

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Jurado, Bauluz e Canudo. "First approach to the paleohistology of the sauropod Galvesaurus (Kimmeridgian, Galve, Spain)". In XVIII Encuentro de Jóvenes Investigadores en Paleontologia. Nova.id.fct, 2021. http://dx.doi.org/10.21695/cterraproc.v1i0.405.

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Popov, Aleksey Yu. "Comparative characteristics of lithogeochemical features of the upper jurassic deposits of the paksa and lower lena facies regions (north of Сentral Siberia)". 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/b978-5-4262-0102-6-2020-020.

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A comparative analysis of lithogeochemical features of Upper Jurassic rock composition of the lower reaches of the Anabar river and the Urdyukh-Haya cape (Nordvik peninsula) was performed. Several common features, differences and regularities of changes in the section of lithogeochemical characteristics of the studied strata were revealed. The rocks of the Kimmeridgian and upper-middle Volgian have the greatest differences from the higher and lower layers. They are characterized by an increase in the content some of impurity elements (Co, Ni, Zn, U, and some TR). The identified features can be used for correlation when comparing faunal mute strata in the considered part of the sedimentary basin.
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Trunilina, Vera. "VOLCANOGENIC FORMATION OF THE UYANDINO-YASACHNAYA MAGMATIC ARC IN THE MIDSTREAM OF THE INDIGIRKA RIVER (VERKHOYANSK-KOLYMA OROGENIC REGION)". In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/1.1/s01.007.

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The Uyandino-Yasachnaya magmatic arc is the largest volcanic-plutonic belt in the north-east of Russia. However, there is yet to be a consensus on the nature of the arc, despite a long study of the rocks composing it. Most researchers consider it to be an island arc formation, however, some researchers also believe that it of a riftogenic or heterogeneous nature. The arc is composed of volcanogenic-sedimentary strata of variegated composition and associated subvolcanic formations. The rocks were formed during the Oxfordian-Volgian stage; their formation either preceded that of the Late Jurassic-Early Cretaceous granitoid massifs, or was synchronous with it. The research focused on volcanogenic and subvolcanic formations of the southeastern part of the arc in the midstream of the Indigirka River. The purpose of the research was to determine their composition and geodynamic conditions of formation. For this purpose, the study of the structure of volcanogenic strata and sub-volcanoes, their petrographic and chemical compositions, relations with granitoids was carried out. The volcanogenic strata within the territory are represented by two formations of rhyolite and their clastolavas: low-alkaline tholeiitic Oxfordian-Kimmeridgian formation and calcalkaline Medium Kimmeridgian � Early Volgian formation. The lower formation developed in the island-arc setting the upper formation developed under transitional conditions of the island-arc to the marginal-continental regime. The subvolcanic massifs have a dacite-rhyodacite composition; they intrude volcanogenic strata of both these suites and are metamorphosed near the contacts of the Early Cretaceous massifs. Their parental melt was produced at the boundary of amphibolite and dacite-tonalite substrates at maximum temperature (up to 1050oC) and pressure (up to 11.1 kbar). They are of Middle or Late Volga age and formed in the initial stages of the development of the active margin of the continent.
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Eltom, Hassan, Luis A. Gonzalez, Eugene C. Rankey, Stephen T. Hasiotis e Dave Cantrell. "MIDDLE – UPPER JURASSIC (UPPER CALLOVIAN TO LOWER KIMMERIDGIAN) CARBON ISOTOPE CHEMOSTRATIGRAPHY FROM CENTRAL SAUDI ARABIA". In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286324.

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Villaorduna Artola, Fredy A., Julio C. Hernandez Villalobos, Citlali Silva Martinez, Gorka Garcia Leiceaga, Rodolfo Camacho Velazquez, Blanca E. Gonzalez, Francisco Olarte Zaleta e Luis J. Alpirez Garcia. "Geophysical pore type characterization in carbonates: Cretaceous and Kimmeridgian carbonates, TS oil field, Gulf of Mexico". In 14th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 3-6 August 2015. Brazilian Geophysical Society, 2015. http://dx.doi.org/10.1190/sbgf2015-151.

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Chan, Septriandi A., John Humphrey, Baqer Albensaad, Muhammad Usman, Khalid Alramadan e Yaser Alzayer. "Sedimentology, Geochemistry, and Mechanical Stratigraphy of an Early Kimmeridgian Carbonate Mudstone in an Arabian Intrashelf Basin". In Unconventional Resources Technology Conference. Tulsa, OK, USA: American Association of Petroleum Geologists, 2022. http://dx.doi.org/10.15530/urtec-2022-3721116.

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Alrowaie, M., R. Algeer, C. West e F. Lu. "Geochemical isotopic analysis to determine the origin of H2S in the Anisian to Kimmeridgian carbonate intervals". In Third EAGE Geochemistry Workshop. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.2021623001.

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Al-Suwaidi, A. S., e S. K. Aziz. "Regional Basin Modelling: An Approach to Understand Sheifal Carbonate Reservoirs of the Oxfordian and Kimmeridgian in Offshore Abu Dhabi". In Abu Dhabi International Petroleum Exhibition and Conference. Society of Petroleum Engineers, 1998. http://dx.doi.org/10.2118/49471-ms.

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Kidambi, Vijaya Kumar, Chinmaya Pattnaik, Srinivasa Rao Narhari e Qasem Dashti. "Opportunities and challenges of the deep Kimmeridgian - Tithonian age evaporates in the light of unconventional reservoir appraisal: Kuwait case study". In International Conference and Exhibition, Barcelona, Spain, 3-6 April 2016. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2016. http://dx.doi.org/10.1190/ice2016-6533813.1.

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Relatórios de organizações sobre o assunto "Kimmeridgium"

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Poulton, T. P., A. Ziess e J. A. Jeletzky. New molluscan faunas from the late Jurassic [Kimmeridgian and early Tithonian] of western Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/126975.

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Kimmeridgian Shales Total Petroleum System of the North Sea Graben Province. US Geological Survey, 2005. http://dx.doi.org/10.3133/b2204c.

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