Relevant bibliographies by topics / Stratigraphie – Lias

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

Academic literature on the topic 'Stratigraphie – Lias'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Stratigraphie – Lias"

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Duarte, Luis Vitor, Manfred Krautter, and Antonio Ferreira Soares. "Bioconstructions a spongiaires siliceux dans le Lias terminal du Bassin lusitanien (Portugal); stratigraphie, sedimentologie et signification paleogeographique." Bulletin de la Société Géologique de France 172, no. 5 (2001): 637–46. http://dx.doi.org/10.2113/172.5.637.

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Abstract The Upper Liassic series in the western border of Iberia (Lusitanian Basin, Portugal), show an important lutitic sedimentation, characterized generally by a monotonous marl/limestone alternation. Small scale siliceous sponge mudmounds occur in these deposits from Middle Toarcian to Lower Aalenian age. The scope of this work is to pinpoint the stratigraphical and sedimentological context and to characterize controlling factors of the spongioliths. Stratigraphic and facies analysis. Relevant sections were observed and investigated in different locations of the Lusitanian Basin (e.g., Al
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Boutakiout, Mohamed. "Les foraminifères "benthiques" de la limite Lias moyen - Lias supérieur dans les rides sud-rifaines (Maroc). Biostratigraphie et considérations paléobiogéographiques." Géologie Méditerranéenne 14, no. 2 (1987): 167–70. http://dx.doi.org/10.3406/geolm.1987.1375.

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Fontana, Fernando F., Steven Tassios, Jessica Stromberg, Caroline Tiddy, Ben van der Hoek, and Yulia A. Uvarova. "Integrated Laser-Induced Breakdown Spectroscopy (LIBS) and Multivariate Wavelet Tessellation: A New, Rapid Approach for Lithogeochemical Analysis and Interpretation." Minerals 11, no. 3 (2021): 312. http://dx.doi.org/10.3390/min11030312.

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This paper demonstrates a novel approach that uses wavelet tessellation in rapid analysis of raw geochemical data produced by laser-induced breakdown spectroscopy (LIBS) to produce pseudologs that are representative of stratigraphy. Single-line LIBS spectral data for seven major rock-forming elements (Al, Ca, Fe, Mg, Si, Na and K) were collected from a synthetic 22-sample rock-block comprising two distinct lithological groups based on mineralogy, chemistry and texture: plutonic rocks and marble. Seven sublithologies are identified within the rock-block from traditional laboratory whole-rock ge
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Alméras, Yves. "Les Brachiopodes du Lias-Dogger: Paléontologie et biostratigraphie." Geobios 20 (January 1987): 161–219. http://dx.doi.org/10.1016/s0016-6995(87)80073-6.

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Reyre, Yves. "Pollenospores du Lias du sondage de Sancerre-Couy (Cher, France)." Géologie Méditerranéenne 14, no. 4 (1987): 271–81. http://dx.doi.org/10.3406/geolm.1987.1389.

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Boomer, Ian. "Ostracod Biostratigraphy of two borehole sections across the Toarcian/Aalenian (Lias/Dogger) boundary, southern Germany." Newsletters on Stratigraphy 31, no. 3 (1994): 143–50. http://dx.doi.org/10.1127/nos/31/1994/143.

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Smith, David G. "Stratigraphic correlation of presumed Milankovitch cycles in the Blue Lias (Hettangian to earliest Sinemurian), England." Terra Nova 1, no. 5 (1989): 457–60. http://dx.doi.org/10.1111/j.1365-3121.1989.tb00410.x.

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Donovan, D. T., M. L. K. Curtis, and T. R. Fry. "The lower part of the Lias Group in south Gloucestershire: zonal stratigraphy and structure." Proceedings of the Geologists' Association 116, no. 1 (2005): 45–59. http://dx.doi.org/10.1016/s0016-7878(05)80016-1.

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Weedon, Graham P., Kevin N. Page, and Hugh C. Jenkyns. "Cyclostratigraphy, stratigraphic gaps and the duration of the Hettangian Stage (Jurassic): insights from the Blue Lias Formation of southern Britain." Geological Magazine 156, no. 9 (2018): 1469–509. http://dx.doi.org/10.1017/s0016756818000808.

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AbstractThe lithostratigraphic characteristics of the iconic Blue Lias Formation of southern Britain are influenced by sedimentation rates and stratigraphic gaps. Evidence for regular sedimentary cycles is reassessed using logs of magnetic susceptibility from four sites as an inverse proxy for carbonate content. Standard spectral analysis, including allowing for false discovery rates, demonstrates several scales of regular cyclicity in depth. Bayesian probability spectra provide independent confirmation of at least one scale of regular cyclicity at all sites. The frequency ratios between the d
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Baudelot, Sabine, André Charriere, Driss Ouarhache, and Abdellah Sabaoui. "Données palynologiques nouvelles concernant l'Ordovicien et le Trias - Lias du Moyen-Atlas (Maroc)." Géologie Méditerranéenne 17, no. 3 (1990): 263–77. http://dx.doi.org/10.3406/geolm.1990.1444.

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Dissertations / Theses on the topic "Stratigraphie – Lias"

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Brunel, François. "Etude stratigraphique et paléontologique du Lias moyen du Quercy septentrional." Toulouse 3, 1996. http://www.theses.fr/1996TOU30200.

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Plusieurs coupes stratigraphiques ont ete levees dans le lias moyen du quercy septentrional (bassin d'aquitaine), entre les regions de saint-cere, a l'est, de gramat, au sud, et de terrasson, a l'ouest. Les analyses stratigraphiques, sedimentologiques (figures et structures sedimentaires, micropetrographie), paleontologiques, mineralogiques, geochimiques et palynologiques, consacrees a la serie calcaire et marneuse de la coupe-type de loubressac-lapoujade, ont permis d'etablir une evolution dans le temps des paleonenvironnements successifs, sur une plate-forme carbonatee, depuis un domaine cir
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Galien, Françoise. "Le Lias inferieur et moyen du bassin de Privas (Ardèche) : sédimentologie, interprétations tectono-sedimentaires et paléogéographiques." Phd thesis, Université Claude Bernard - Lyon I, 1985. http://tel.archives-ouvertes.fr/tel-00769745.

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Le Lias ardéchois montre d ' importantes variations de faciès et d'épaisseur. De plus la coexistence de faciès détritiques grossiers et de faciès carbonatés marins laisse supposer une activité tectonique synsédimentaire intense. Je me suis donc consacrée à l'étude du Lias inférieur et moyen du bassin de Privas , dans lequel les formations de cette période affleurent relativement bien. Il s'agira ici de rassembler le maximum de données (paléontologiques,stratigraphiques et sédimentolog iques) avec deux objectifs principaux : -la reconstitution paléogéographique du bassin aux divers étages étudi
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Thévenard, Frédéric. "La paléoflore du jurassique inférieur (Lias) du bassin des Causses (France) : étude systématique, stratigraphique et paléoécologique." Lyon 1, 1992. http://www.theses.fr/1992LYO10049.

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La paleoflore du lias inferieur du bassin des causses a ete etudiee dans son cadre stratigraphique, sedimentologique, systematique et paleoecologique. De nouvelles recoltes, le reexamen de collections et l'emploi de plusieurs techniques et methodes d'etude, ont permis de realiser une nouvelle approche du materiel des causses. Les niveaux reperes a accumulation de vegetaux sont remis en cause. Une analyse morphometrique est proposee pour repondre a certains problemes de reconnaissance de forme. Les prespermatophytes sont reparties en trois ordres: pteridospermales (deux genres), cycadales (un g
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Cubaynes, René. "Le lias du Quercy méridional : études lithologiques, biostratigraphique, paléoécologique et sédimentologique." Toulouse 3, 1986. http://www.theses.fr/1986TOU30113.

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Les concepts séquentiels, la définition scalaire des séquences et de leur contexte paléogéographique ont permis de proposer une première trame séquentielle pour le lias quercynois et un premier modèle d'évolution des paysages sédimentaires sous un climat tropical. Le lias du secteur étudie forme une mégaséquence d'ouverture et constitue une marge stable et peu subsidente. La distension crustale marquée au trias avec la mise en place d'une série synrift continentale, se poursuit au lias en s'atténuant progressivement. L’installation de la plateforme carbonatée du dogger clôture cette histoire d
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Forest-Bize, Nadège. "Variation de la préservation des dépôts et signification des séries condensée : les séries liasiques d'une marge en phase de rifting (Alpes) et d'une plate-forme épicontinentale (Bourgogne)." Dijon, 2000. http://www.theses.fr/2000DIJOS090.

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Au Lias inférieur et moyen, l'éperon bourguignon et la marge NW Téthys sont caracterisés par le dépôt de séries condensées carbonatées et phosphatées, d'offshore supérieur et inférieur. Ce travail établit la distribution des faciès de ces séries dans un cadre-temps à haute résolution (horizon ou sous-zone) afin de comprendre la variation de la préservation des dépôts et les variations de l'espace disponible. Des séries plurimétriques contenant ponctuellement des niveaux supercondensés, phosphates et riches en ammonites (Oisans, Vanoise, Préalpes) s'opposent ici à des séries pluridécimétriques
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Lézin, Carine. "Analyses des facies et stratigraphie integree : application aux evenements du passage lias-dogger sur la plate-forme du quercy." Toulouse 3, 2000. http://www.theses.fr/2000TOU30162.

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Ce travail montre la contribution d'une approche pluri-disciplinaire pour la reconstitution de l'evolution du bassin quercynois durant l'intervalle toarcien superieur-bajocien inferieur et l'identification des facteurs controlant cette evolution. La serie, composee de 7 unites lithostratigraphiques, a ete subdivisee en zones et horizons, plusieurs nouveaux bio-horizons locaux etant individualises. L'analyse des facies (analyse statistique) a permis d'individualiser 25 facies qui se repartissent dans un domaine de plate-forme ouverte au toarcien superieur-aalenien inferieur et dans un domaine d
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Ouahhabi, Bénali. "Le Lias moyen et supérieur des Beni Znassen orientaux et des Zekkara (Maroc nord-oriental) : biostratigraphie, paléontologie des Hildoceras." Lyon 1, 1986. http://www.theses.fr/1986LYO11721.

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Le Lias moyen et supérieur de la région d'Oujda ont été étudiés grâce à 9 coupes. Les ammomites ont permis d'établir une biostratigraphie relativement fine : niveaux pour le Carixien (Tropidoceras), 9 pour le Domérien (Protogrammoceras, Arieticeras, Amaltheus), 10 pour le Toarcien (Hildaites, Harpoceras et surtout Hildoceras, Hammatoceras). L'Aalénien signalé pour la première fois, est très réduit. Une étude systématique et biométrique du genre Hildoceras avec ses espèces et leurs morphotypes variés bien situés dans le temps, donne une image de l'évolution de ce genre. L'influence du milieu se
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Améziane-Cominardi, Nadia. "Distribution bathymétrique des pentacrines du Pacifique occidental : essai de modélisation et d'application aux faunes du lias (problèmes de tectono-eustatisme au cours du rifting téthysien)." Lyon 1, 1989. https://tel.archives-ouvertes.fr/tel-02314185/document.

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Hamon, Youri. "Morphologie, évolution latérale et signification géodynamique des discontinuités sédimentaires : exemple du Lias de la marge ouest du bassin du sud-est (France)." Montpellier 2, 2004. https://tel.archives-ouvertes.fr/tel-00009709.

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GEILLER, MAGALI. "Sedimentologie de facies, mineralogie et stratigraphie genetique des reservoirs silico-clastiques du lias inferieur de cere-la-ronde (d'apres les donnees de forages gdf de sologne - sw du bassin de paris)." Université Louis Pasteur (Strasbourg) (1971-2008), 1997. http://www.theses.fr/1997STR13238.

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Les niveaux reservoirs silicoclastiques du sud-ouest du bassin de paris sont exploites par gaz de france pour le stockage du gaz naturel en nappe aquifere. L'ojectif est de definir la geometrie des reservoirs, et les differents facteurs controlant leur mise en place dans le bassin de sologne, au rhetien et a l'hettangien. La demarche pluridisciplinaire adoptee allie des analyses palynologiques, sedimentologiques, mineralogiques et sequentielles. Elle est appliquee aux depots de chenaux, ainsi qu'aux depots d'interchenaux plus rarement consideres dans le cadre de l'etude de reservoirs. L'ensemb
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Books on the topic "Stratigraphie – Lias"

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Sadki, Driss. Le Haut-Atlas central (Maroc): Stratigraphie et paléontologie du Lias supérieur et du Dogger inférieur : dynamique du bassin et des peuplements. Centre des sciences de la terre, Université Claude-Bernard, Lyon I, 1997.

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Stratigraphie, sédimentologie et interprétations géodynamiques du Lias-début du Dogger: Exemple de sédimentation carbonatée de plate-forme en Oranie (Monts de Sidi el Abed, Hautes-Plaines, Algérie occidentale. Centre des sciences de la terre, Université Claude-Bernard, Lyon, 1996.

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Centre international d'études du Lias. (3rd 1990 Lyon, France). Troisième Colloque du Centre international d'études du Lias (C.I.E.L.): Lyon, 16 juillet 1990. Association des facultés catholiques de Lyon, 1992.

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Centre international d'études du Lias. Colloque. Premier Colloque du Centre international d'études du Lias (C.I.E.L.): 15-18 mai 1984. Association des facultés catholiques de Lyon, 1985.

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Centre international d'études du Lias. Colloque. Deuxième Colloque du Centre international d'études du Lias (C.I.E.L.): Lyon, 27-30 mai 1986. Association des Facultés catholiques de Lyon, 1987.

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Centre international d'études du Lias. Colloque. Premier Colloque du Centre international d'études du Lias (C.I.E.L.), 15-18 mai 1984. Associations des facultés catholiques de Lyon, 1985.

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Jäger, Rolf Josef. Foraminiferen und Ostracoden aus den Fleckenmergeln des Kalkalpinen Lias: Biostratigraphie und Paläoökologie. F. Pfeil, 1997.

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Ebli, Oskar. Sedimentation und Biofazies an passiven Kontinentalrändern: Lias und Dogger des Mittelabschnittes der Nördlichen Kalkalpen und des frühen Atlantik (DSDP site 547B, offshore Marokko). F. Pfeil, 1997.

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Lianda, Gao, and Jin Jianhua, eds. Liao dong Taizi He liu yu zao shi tan shi zhi wu gu sheng tai yu gu huan jing. Di zhi chu ban she, 2001.

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Université Claude Bernard. Département des sciences de la terre., ed. Lias-Dogger du Moyen-Atlas plissé (Maroc): Sédimentologie, biostratigraphie et évolution paléogéographique. Centre des sciences de la terre, Université Claude-Bernard, 1989.

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Book chapters on the topic "Stratigraphie – Lias"

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Bessereau, G., and F. Guillocheau. "Sequence Stratigraphy and Organic Matter Distribution of the Lias of the Paris Basin." In Hydrocarbon and Petroleum Geology of France. Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-78849-9_7.

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Targowski, P., E. Kwiatkowska, M. Sylwestrzak, et al. "Absolute LIBS stratigraphy with Optical Coherence Tomography." In Lasers in the Conservation of Artworks VIII. CRC Press, 2010. http://dx.doi.org/10.1201/b10567-25.

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Bessereau, G., F. Guillocheau, and A. Y. Huc. "Source Rock Occurrence in a Sequence Stratigraphic FrameworkThe Example of the Lias of the Paris Basin." In Paleogeography, Paleoclimate, and Source Rocks. American Association of Petroleum Geologists, 1995. http://dx.doi.org/10.1306/st40595c12.

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Redwine, Joanna R., and Kenneth D. Adams. "A 740,000-yr-long Mohawk Lake record, Mohawk Valley, northeastern California, USA." In From Saline to Freshwater: The Diversity of Western Lakes in Space and Time. Geological Society of America, 2019. http://dx.doi.org/10.1130/2021.2536(21).

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ABSTRACT Mohawk Valley lies in northeastern California on the margin of the northernmost Sierra Nevada and was occupied by Mohawk Lake during much of the middle and late Pleistocene. Throughout that time, the Sierra Nevada ice cap repeatedly extended northward into Mohawk Lake, and ice-contact deltaic sediments were deposited along the valley margins and in the valley bottom. Nearly 200 m of lacustrine and deltaic sediments are now well exposed along streams draining the Sierra Nevada. Tephra beds deposited within the deltaic sediments allow correlation of stratigraphic sections around the valley margin and, together with geomorphic evidence of former lake levels, permit interpretation of a Mohawk Lake history as far back as 740 ka. Mohawk Valley changed from a through-flowing fluvial setting to an intermittent closed basin sometime before 740 ka. After this change occurred, relatively small lakes intermittently formed in Mohawk Valley until ca. 600 ka, when the lake dramatically deepened. Mohawk Lake fluctuated in size over the next ~400,000 yr and increased in size to its highest levels after ca. 200 ka, possibly due to drainage integration with the upstream Lake Beckwourth. After this time, Mohawk Lake spilled over its westward sill, incrementally eroding and lowering lake levels until Mohawk Lake was emptied by ca. 7 ka.
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Holman, J. Alan. "The Pleistocene in Britain and Europe." In Pleistocene Amphibians and Reptiles in Britain and Europe. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195112320.003.0006.

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A general introduction to the Pleistocene with an emphasis on herpetological remains was presented in the companion volume Pleistocene Amphibians and Reptiles in North America (Holman, 1995c). For a general introduction to the Pleistocene that gives much attention to Britain and Europe, the reader is referred to Sutcliffe (1985). A detailed account of Pleistocene mammals in Britain is given by Stuart (1982), and a general account of Pleistocene mammals in Europe is given by Kurten (1968). The present chapter deals mainly with chronological divisions of the Pleistocene in Britain and Europe. Early geologists recognized that glacial deposits and land forms existed far south of existing glaciated areas, and they correctly reasoned that these features indicated not only the presence of ice sheets but the onset of cold climates, as well. As these features were mapped and stratigraphic studies were made, it was found that some sections contained weathered zones of organic soils and plant remains between layers of glacially derived sediments. It was suggested that these organic zones represented nonglacial environments and that ice sheets must have advanced and retreated several times. In Europe, before studies of deep sea sediments were made, Pleistocene chronological events were determined on the basis of piecemeal evidence from terrestrial sediments. The earliest widely accepted chronology of climatic Pleistocene intervals was the classic fourfold subdivision of Pleistocene glacial events in the Alps by Penck and Bruckner (1909). These glacial stage names, from oldest to youngest, are Gu'nz glacial, Mindcl glacial, Riss glacial, and Wiirm glacial. Between the glacial stages, intcrglacial stages were designated by compound names based on the underlying and overlying glacial stages (e.g., The Gunz-Mindel intcrglacial stage lies between the Giinz and Mindel glacial stages). These Alpine glacial stages have been widely used, and one still finds references to them (especially the younger stages) in the recent literature (e.g., Fritz, 1995).
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"The Plot Against the Past: Reuse and Modification of Ancient Mortuary Monuments as Persuasive Efforts of Appropriation." In The Lives of Prehistoric Monuments in Iron Age, Roman, and Medieval Europe, edited by Marta Díaz-Guardamino, Leonardo García Sanjuán, and David Wheatley. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780198724605.003.0024.

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‘The were not for something in human beings in complicity with it’ writes Alexander Kluge (1990, 20) in The Assault of the Present on the Rest of Time. Kluge is concerned with condensed dramatic cinematic time and his present now lies several decades in the past. However, the image of an empowered present plotting against a defenceless past presents itself as an adequate point of departure. Reuse and modification of ancient monuments after extended periods of disuse—monuments herein defined as anything from monoliths and sarcophagi to large earthen mounds and wooden or stone buildings—are frequent phenomena throughout the world. Reuse can range from one-time visits and the placing of human remains and artefacts to the rearrangement of architectural elements and remodelling of entire structures. No cultural continuity is required (Bradley 1993, 117–21) for discontinuous reuse can bridge centuries and even millennia. Reuse of monuments is an ongoing phenomenon. Not only prehistoric monuments but also historic monuments have been affected. I therefore will follow Taylor’s lead (Taylor 2008, 24), overstep the disciplinary thresholds and not pay attention to a prehistory-history distinction. The term prehistory was only born in the early nineteenth century AD (Rowley-Conwy 2006; Taylor 2008, 2) and people who reuse or manipulate monuments do not draw lines between historic and prehistoric monuments. Additionally, the onset of modernity brought along expanded chronological constructions of time. How we from the so-called Western World look upon the past and our expectations of the future not only has made us more time conscious in relation to the present but entirely changed our conceptualization of time (Koselleck 2004). To historians and archaeologists time is stratigraphic and sequential. Archaeologists are concerned with fixing objects and events in their proper place and time. Today most people look at the past with a temporal depth to it (Dodgshon 2008, 6). However, the way we look at time is not how everybody else conceives of it. Different cultural contexts create different concepts of time (e.g. Lévi-Strauss, 1970, 16; Hirsch 2006).
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Diaz-Andreu, Margarita. "An Alternative Account of the History of Archaeology in the Nineteenth Century." In A World History of Nineteenth-Century Archaeology. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780199217175.003.0006.

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Historians of science (whether philosophers, epistemologists, historians of science, or sociologists of science) have been stubbornly reluctant to deal with archaeology in favour of other disciplines such as geology and medicine. Most histories of archaeology have, therefore, been written by archaeologists and this book is no exception. Being trained in the subtleties of stratigraphy and typology does not, however, provide archaeologists with the necessary tools to confront the history of their own discipline. Many of the histories of archaeology so far written revolve around a narrow, almost positivistic, understanding of what the writing of one’s own disciplinary history represents. This volume attempts to overcome these limitations. Questions addressed have been inspired by a wide range of authors working in the areas of history, sociology, literary studies, anthropology, and the history of science. It uses the case of nineteenth-century world archaeology to explore the potential of new directions in the study of nationalism for our understanding of the history of archaeology. Key concepts and questions from which this study has drawn include the changing nature of national history as seen by historians (Berger et al. 1999b; Hobsbawm 1990) and by scholars working in the areas of literature and political studies (Anderson 1991); transformations within nationalism (Smith 1995); new theoretical perspectives developed within colonial and post-colonial studies (Asad 1973; Said 1978); the relationship between knowledge and power (Foucault 1972 (2002); 1980b); and the consideration of social disciplines as products of history (Bourdieu 1993; 2000; 2004). Perhaps historians and sociologists of science’s lack of enthusiasm to engage with archaeology derives from its sheer lack of homogeneity. The term comes from the Greek arkhaiologia, the study of what is ancient. It most commonly encompasses the analysis of archaeological remains, but the emphasis on what body of data lies within its remit has always differed—and still does—from country to country and within a country between groups of scholars of the various academic traditions. For some it revolves around the study of artistic objects, as well as of ancient inscriptions and coins, for others it encompasses all manifestations of culture from every period of human existence.
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Crouch, Dora P. "Central Greco-Roman Cities." In Geology and Settlement. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195083248.003.0010.

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Argos, situated in the southern peninsula of Greece called the Peloponnese, lies on the northwest side of the Argos Plain, backed by hills to the north and west that are the eastern edge of an extensive region of mountains and intermountain basins. A road runs northward through the valley and over the hills to Nemea and Corinth. Eastward beyond the capricious rivers lie the old Mycenaean cities of Mycenae and Tiryns on their knolls, with the port of Nauplia closing the circuit to the southeast. Beyond Nauplia is the Argolid peninsula with the ancient pilgrimage and health center of Epidauros. (The term “Argolid” as used in the literature sometimes means all the area near Argos and sometimes means only the peninsula south and east of Nauplia. Herein, we will use Argolid for the latter and Argive Plain for the former.) Between Argos and the gulf about 6 km south is the marshy area of Lerna, remnant of a lake that once reached nearly to the outskirts of Argos, while the southeast part of the plain was until recently a series of lagoons (Piérart 1992). To the southwest, skirting the mountains, runs the road to Sparta. The advantages for Argos of being situated at the center of gravity in the triangular plain (Runnels 1995) continued throughout all the periods studied herein. Argos is unusual among ancient cities because we have ample modern geological investigations of regional structure, morphology, karst geology, and hydrogeology, literary evidence from antiquity, and archaeological data from decades of investigation. These materials contribute to a detailed understanding of how human settlement built on and responded to local resources. We will therefore describe the regional setting of the city before turning to an examination of the urban core. Below its mountains, the city of Argos stands on a shelf overlooking a plain of extensive fertile agricultural land that curves around the site from north to southwest. The stratigraphy is as follows, beginning with the topmost modern layers: . . . Higher plateau and mountains are Tripoli limestone. Tripoli plateau sits amid karstic mountains. (Older) Triassic and Jurassic limestones to the northeast. . . .
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Conference papers on the topic "Stratigraphie – Lias"

1

Kwiatkowska, Ewa A., Jan Marczak, Roman Ostrowski, et al. "Absolute LIBS stratigraphy with optical coherence tomography." In SPIE Europe Optical Metrology, edited by Luca Pezzati and Renzo Salimbeni. SPIE, 2009. http://dx.doi.org/10.1117/12.827271.

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2

Jordan, Patrick D., and Jesse J. Melick. "Stratigraphic Variability of the Demoinesian Marmaton Group Across the Lips Fault System in the Texas Panhandle Granite Wash, Southern Anadarko Basin." In Unconventional Resources Technology Conference. American Association of Petroleum Geologists, 2017. http://dx.doi.org/10.15530/urtec-2017-2671416.

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3

Fatta, Francesca, Andrea Marraffa, and Claudio Patanè. "Geometrie dello sguardo nel paesaggio calabrese." In FORTMED2020 - Defensive Architecture of the Mediterranean. Universitat Politàcnica de València, 2020. http://dx.doi.org/10.4995/fortmed2020.2020.11543.

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Geometries of the gaze in the Calabrian landscapeHaving lost their function of sighting as an instrument of strategic control, inclusion and protection from presumed pirate invasions, the coastal towers of Calabria Ultra, represented in the Diary of Wonders of the end of the sixteenth century, called Codice Romano Carratelli, will act as the key and device of the gaze that links the land to the expanse of water. A vast geometric, precise and linear system that will connect, through the gaze, the “terracqueo landscape”, unstable and multiform, continuously changing. The ninety-nine watercolour
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Bishop, Mark Emmanuel, Wilson Lalla, and Xavier Ravi Moonan. "Evaluating the Lower Cruse and Navet Formations Within the Wd-8 Lease Operatorship Block." In SPE Trinidad and Tobago Section Energy Resources Conference. SPE, 2021. http://dx.doi.org/10.2118/200925-ms.

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Abstract Lease Operatorship block WD-8, lies within the Forest Reserve oilfield. Forest Reserve is known for having the ENE-WSW trending, south easterly verging Forest Reserve anticline which plunges into NW-SE trending Los Bajos Fault. Regionally to the south of the Forest Reserve anticline lies the south westerly plunging Siparia syncline and to the north of the Forest Reserve anticline is the Morne L′ Enfer syncline. WD-8 is situated on the northern flank of the Forest Reserve anticline with the axis of the anticline occurring within the southern part of the block. Prior to 2018, TETL last
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