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Relevant bibliographies by topics / Fluvio-lacustrine and shallow marine sedimentation

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Academic literature on the topic 'Fluvio-lacustrine and shallow marine sedimentation'

Author: Grafiati

Published: 4 June 2021

Last updated: 16 February 2022

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Journal articles on the topic "Fluvio-lacustrine and shallow marine sedimentation"

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Walley, C. D. "Depositional history of southern Tunisia and northwestern Libya in Mid and Late Jurassic time." Geological Magazine 122, no. 3 (1985): 233–47. http://dx.doi.org/10.1017/s0016756800031447.

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AbstractThe good exposures of virtually undeformed Callovian and Oxfordian strata along the Djeffara escarpment of southern Tunisia and northwestern Libya have allowed analysis of regional depositional history during this time.A number of lithostratigraphic problems are considered. In Tunisia, the Foum Tatahouine Formation is subdivided into members and in Libya some of the stratigraphic issues are clarified. A correlation between the two sequences is proposed. The widely claimed aeolian origin for the Libyan Chameau Mort Sandstone is rejected.The depositional patterns of the Callovian and Oxf

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Martín-Martín, Manuel, Francesco Guerrera, and Mario Tramontana. "Tectono-Sedimentary Evolution of the Cenozoic Basins in the Eastern External Betic Zone (SE Spain)." Geosciences 10, no. 10 (2020): 394. http://dx.doi.org/10.3390/geosciences10100394.

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Four main unconformities (1–4) were recognized in the sedimentary record of the Cenozoic basins of the eastern External Betic Zone (SE, Spain). They are located at different stratigraphic levels, as follows: (1) Cretaceous-Paleogene boundary, even if this unconformity was also recorded at the early Paleocene (Murcia sector) and early Eocene (Alicante sector), (2) Eocene-Oligocene boundary, quite synchronous, in the whole considered area, (3) early Burdigalian, quite synchronous (recognized in the Murcia sector) and (4) Middle Tortonian (recognized in Murcia and Alicante sectors). These unconfo

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Marenssi, Sergio A., Carlos O. Limarino, Laura J. Schencman, and Patricia L. Ciccioli. "Tectonic and geomorphic controls on the lacustrine deposits of the Neogene Vinchina basin, northwestern Argentina." Journal of Sedimentary Research 90, no. 2 (2020): 250–67. http://dx.doi.org/10.2110/jsr.2020.13.

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ABSTRACT Two episodes of lacustrine sedimentation, separated by an erosional surface and fluvial sedimentation, took place in the southern part of the broken foreland Vinchina basin (NW Argentina) between 11 and 5 Ma. The lacustrine deposits, 768 and 740 meters thick, are recorded in the upper part of the Vinchina Formation (“Vinchina lake”) and the lower part of the Toro Formation (“Toro Negro lake”) respectively. According to sedimentological features, four sedimentary facies associations (FAs) are recognized in the lacustrine deposits: 1) thinly laminated mudstones facies association (FA 1)

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Michelsen, Olaf, Lars H. Nielsen, Peter N. Johannessen, Jan Andsbjerg, and Finn Surlyk. "Jurassic lithostratigraphy and stratigraphic development onshore and offshore Denmark." Geological Survey of Denmark and Greenland (GEUS) Bulletin 1 (October 28, 2003): 145–216. http://dx.doi.org/10.34194/geusb.v1.4651.

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A complete updated and revised lithostratigraphic scheme for the Jurassic succession of the onshore and offshore Danish areas is presented together with an overview of the geological evolution. The lithostratigraphies of Bornholm, the Danish Basin and the Danish Central Graben are described in ascending order, and a number of new units are defined. On Bornholm, the Lower–Middle Jurassic coal-bearing clays and sands that overlie the Lower Pliensbachian Hasle Formation are referred to the new Sorthat Formation (Lower Jurassic) and the revised Bagå Formation (Middle Jurassic). In the southern Dan

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Woszczyk, Michał, Wojciech Tylmann, Jan Jędrasik, et al. "Recent sedimentation dynamics in a shallow coastal lake (Lake Sarbsko, northern Poland): driving factors, processes and effects." Marine and Freshwater Research 65, no. 12 (2014): 1102. http://dx.doi.org/10.1071/mf13336.

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Despite the fact that sediment dynamics in shallow coastal lakes strongly influences lake water quality and is crucial for preserving good quality paleo-records from coastal zones, the depositional processes in coastal lakes have not been thoroughly recognised so far. The present study aims at investigating the relationship between lake water circulation and the distribution of surface sediments, identifying the postdepositional physical mechanisms affecting lake deposits, and estimating the intensity of sediment mixing in a coastal lake on the Baltic coast. Our approach includes analyses of s

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Mueller, W., and J. A. Donaldson. "Development of sedimentary basins in the Archean Abitibi belt, Canada: an overview." Canadian Journal of Earth Sciences 29, no. 10 (1992): 2249–65. http://dx.doi.org/10.1139/e92-177.

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Sedimentation in the Archean Abitibi greenstone belt occurred during four depositional episodes: (i) sedimentary cycle 1, 2730–2720 Ma; (ii) sedimentary cycle 2, 2715–2705 Ma; (iii) sedimentary cycle 3, 2700–2687 Ma; and (iv) sedimentary cycle 4, 2685–2675 Ma. Records of the first two sedimentary cycles are preserved in basins within the northern volcanic zone, whereas basins formed during the latter two sedimentary cycles are located within the southern volcanic zone of the Abitibi belt. Sedimentary cycles 1 and 3 represent deep-water facies, as indicated by turbidites, resedimented conglomer

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Corrêa, Iran Carlos Stalliviere, Svetlana Medeanic, Jair Weschenfelder, Elírio Ernestino Toldo Júnior, José Carlos Nunes, and Ricardo Baitelli. "THE PALAEO-DRAINAGE OF THE LA PLATA RIVER IN SOUTHERN BRAZIL CONTINENTAL SHELF." Revista Brasileira de Geofísica 32, no. 2 (2014): 259. http://dx.doi.org/10.22564/rbgf.v32i2.481.

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ABSTRACT. This paper addresses the characterization of the geomorphology and palaeo-evolution of the La Plata River on the south Brazilian continental shelf,through bathymetric data and sedimentary and palynological analysis from sediment core samples. The analysis allowed us to characterize a transgressive depositionalsequence in the La Plata River palaeo-channel. The palynological sequences revealed continental fresh water environments, that involved into lagoonal and mixohalineenvironments and then into shallow marine environments towards the top, thus characterizing a fluvial-estuarine env

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Ku, Teh-Lung, Shangde Luo, Tim K. Lowenstein, Jianren Li, and Ronald J. Spencer. "U-Series Chronology of Lacustrine Deposits in Death Valley, California." Quaternary Research 50, no. 3 (1998): 261–75. http://dx.doi.org/10.1006/qres.1998.1995.

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Uranium-series dating on a 186-m core (DV93-1) drilled from Badwater Basin in Death Valley, California, and on calcareous tufas from nearby strandlines shows that Lake Manly, the lake that periodically flooded Death Valley during the late Pleistocene, experienced large fluctuations in depth and chemistry over the last 200,000 yr. Death Valley has been occupied by a long-standing deep lake, perennial shallow saline lakes, and a desiccated salt pan similar to the modern valley floor. The average sedimentation rate of about 1 mm/yr for core DV93-1 was punctuated by episodes of more-rapid accumula

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Anderton, R. "Sedimentology of the Dinantian of Foulden, Berwickshire, Scotland." Transactions of the Royal Society of Edinburgh: Earth Sciences 76, no. 1 (1985): 7–12. http://dx.doi.org/10.1017/s0263593300010233.

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ABSTRACTThe Berwickshire Cementstone Group was deposited on a coastal plain crossed by meandering rivers flowing S into a marine gulf, the Northumberland basin. Sedimentation was mainly by overbank flooding onto an alluvial plain which largely dried out between floods. The resulting sediments include poorly-stratified mudstones and siltstones and crevasse splay sheet sandstones. The depositional environment of the cementstones is not clear. Lacustrine and tidal flat origins are considered. Semi-permanent floodplain lakes were very rare, but in one the uniquely fossiliferous Foulden Fish Bed wa

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Rigueti, Ariely L., Patrick Führ Dal' Bó, Leonardo Borghi, and Marcelo Mendes. "Bioclastic accumulation in a lake rift basin: The Early Cretaceous coquinas of the Sergipe–Alagoas Basin, Brazil." Journal of Sedimentary Research 90, no. 2 (2020): 228–49. http://dx.doi.org/10.2110/jsr.2020.11.

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ABSTRACT Coquinas constitute widespread deposits in lacustrine, estuarine, and shallow marine settings, where they are a valuable source of information on environmental conditions. Thick coquina successions were deposited in a series of lacustrine rift basins that formed along the Brazilian Continental Margin during the early stages of the opening of the South Atlantic Ocean, in the Early Cretaceous. In the Sergipe–Alagoas Basin, the coquina sequence, equivalent to the Morro do Chaves Formation, crops out in the Atol Quarry, and is considered a relevant analog for the economically important hy

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Dissertations / Theses on the topic "Fluvio-lacustrine and shallow marine sedimentation"

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Ribes, Charlotte. "Interaction entre la tectonique salifère et la sédimentation dans des mini-bassins : Exemple de l’Oligo-Miocène du bassin de Sivas, Turquie." Thesis, Pau, 2015. http://www.theses.fr/2015PAUU3034/document.

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L’objectif de cette thèse est d’analyser l’évolution d’une province à mini-bassins salifères, en s’appuyant sur l’étude des variations spatiales et temporelles de faciès, d’épaisseurs ainsi que des géométries développées lors du fluage des évaporites. L’exemple naturel investigué est le bassin de Sivas, situé sur le Plateau central Anatolien en Turquie. Ce bassin d’avant-pays enregistre à l’Oligo-Miocène la formation de nombreux mini-bassins secondaires au-dessus d’un niveau d’évaporites allochtones. A partir d’une cartographie et d’une description détaillées des séries sédimentaires accumulée

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Hlal, Osama Ahmed. "Diagenesis and Reservoir-Quality Evolution of Paralic, Shallow Marine and Fluvio-lacustrine Deposits : Links to Depositional Facies and Sequence Stratigraphy." Doctoral thesis, Uppsala universitet, Berggrundsgeologi, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-8986.

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Linking diagenesis to depositional facies and sequence stratigraphy enables better prediction of spatial and temporal distribution of diagenetic alterations, and thus of evolution of reservoir quality in sandstones. This thesis demonstrates that employing this approach is possible because depositional facies and sequence stratigraphy can provide useful information on parameters controlling the near-surface diagenesis, such as changes in: (i) pore-water chemistry, (ii) residence time of sediments under certain geochemical conditions, (iii) detrital composition and proportion of extra- and intra

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Book chapters on the topic "Fluvio-lacustrine and shallow marine sedimentation"

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MCKIE, T., J. AGGETT, and A. J. C. HOGG. "SEQUENCE ARCHITECTURE OF A TRIASSIC SEMI-ARID, FLUVIO-LACUSTRINE RESERVOIR, WYTCH FARM FIELD, SOUTHERN ENGLAND." In Shallow Marine and Nonmarine Reservoirs: Sequence Stratigraphy, Reservoir Architecture and Production Characteristics. SEPM Society for Sedimentary Geology, 1997. http://dx.doi.org/10.5724/gcs.97.18.0197.

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