Relevant bibliographies by topics / Sedimentary

Academic literature on the topic 'Sedimentary'

Author: Grafiati
Published: 4 June 2021
Last updated: 27 February 2023

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

Journal articles on the topic "Sedimentary":

1

Yue, Shao Fei, De Tian Yan, Xiao Peng Li, and Guang Zeng Song. "The Characteristics of Sedimentary Facies of Tanzhuang Formation of Upper Triassic of Luoyi District." Advanced Materials Research 868 (December 2013): 7–10. http://dx.doi.org/10.4028/www.scientific.net/amr.868.7.

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Based on the observation and description of single well and outcrops and the analysis of reservoir compositions, petrology, clastic structure and sedimentary structure,this paper determines the sedimentaty facies characteristics of Tanzhuang formation. The types of sedimentary facies in late Triassic epoch are delta front,shallow lake and semi-deep lake. The delta front develops subaqueous distributary channel, mouth bar and distal bar. Lacustrine facies develops shallow lake mud, shallow lake sand bar, turbidite sand and semi-deep lake mud.The reservoir rock formations in this area are lithic sandstone,feldspathic lithic sandstone with high content of feldspar and debris.The sedimentary structures include ripple, scour surface and cross-bedding are identified.
2

Otavio, Jonatas Malaquias, Osvaldo Girão, Tiago Fernando de Holanda, and Wenderson Sávyo Aguiar Da Silva. "FORMAÇÃO E DIAGÊNESE DE ARENITOS DE PRAIA: Uma Revisão Conceitual." CLIO – Arqueológica 32, no. 3 (September 5, 2017): 88. http://dx.doi.org/10.20891/clio.v32n3p88-106.

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Os arenitos de praia, ou beachrocks, são sedimentos que sofreram um processo de litificação e são encontrados paralelamente à linha de costa na zona intermaré, apresentando uma forma alongada, estreita e cimentados por carbonato de cálcio. O processo de diagênese consiste na formação da rocha sedimentar propriamente dita a partir da compactação, dissolução, cimentação e recristalização. O estudo da formação e diagênese do arenito de praia são relevantes pois possibilita o entendimento de como as rochas sedimentares detríticas são geradas, além de reconhecer como a variação do nível do mar se comportou durante o Holoceno, permitindo a gênese destas feições que se constituem em relevantes elementos de resguardo das linhas de costas em ambientes majoritariamente tropicais. FORMATION AND DIAGENÈSE IN BEACHROCKS:A Conceptual Review ABSTRACTThe beach sandstones, or beachrocks, are sediments that underwent a lithification process and are found parallel to the coastline in the intertidal zone, presenting an elongated, narrow shape and cemented by calcium carbonate. The process of diagenesis consists on the formation of the sedimentary rock itself, following deposition, compaction, dissolution, cementation and recrystallization. The study of the formation and diagenesis of beach sandstone is relevant since it permits the understanding of how clastic sedimentary rocks are formed, besides with recognizing how sea level variation behaved during the Holocene, thus allowing the genesis of these features that constitute relevant elements of shelter along coastlines in most tropical environments. Keywords: Beachrocks, sedimentary rock, cementation.
3

Holanda, Werlem, Anderson Costa dos Santos, Camila Cardoso Nogueira, Luiz Carlos Bertolino, Sérgio Bergamaschi, René Rodrigues, and Diego Felipe da Costa. "EFFECTS OF IGNEOUS INTRUSION ON THE MINERALOGICAL CONTENT OF IRATI FORMATION, PARANÁ BASIN, IN SAPOPEMA (PR), SOUTHERN BRAZIL." Journal of Sedimentary Environments 4, no. 3 (September 28, 2019): 350–60. http://dx.doi.org/10.12957/jse.2019.45796.

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Igneous intrusions in sedimentary basins are commonly related with mineralogical association changes in host-rock. At Sapopema region (Paraná State, southern Brazil), an extensive diabase sill (associated to Serra Geral Formation) was emplaced in pelitic-carbonate succession during post-Triassic. The sedimentary host-rock association includes mostly shale, siltstone and carbonate of the Permian Irati Formation. X-ray diffraction (XRD), scanning electron microscopy (SEM) and energy dispersive spectroscopy (EDS) data revealed that heat transfer was not enough to cause modifications in mineral assemblage of the Taquaral Member (quartz + albite + muscovite + illite + kaolinite + chlorite). However, mineralogical content from Assistência Member presented changes probably caused by the intrusion of diabase sill (talc + pyrophyllite + calcite). Talc and calcite were formed due to the reaction between dolomite and quartz, while pyrophyllite was the product of reaction between kaolinite and quartz. EFEITOS DA INTRUSÃO IGNEA NA COMPOSIÇÃO MINERALÓGICA DA FORMAÇÃO IRATI, BACIA DO PARANÁ, SAPOPEMA (PR), SUL DO BRASIL ResumoAs intrusões ígneas em bacias sedimentares dão origem em geral a alterações mineralógicas da rocha hospedeira. Na região de Sapopema (Estado do Paraná, sul do Brasil), uma extensa soleira de diabásio (associada à Formação Serra Geral) pós-Triássica, foi intrudida numa sucessão sedimentar constituída por pelitos e carbonatos. A associação de rochas sedimentares hospedeiras, era principalmente constituída por folhelho, siltito e carbonato da Formação Irati, do Permiano. Dados de difração de raios X (DRX), microscopia eletrônica de varredura (MEV) e espectroscopia de energia dispersiva (EDS) revelaram que a transferência de calor não foi suficiente para causar modificações na composição mineralógica do membro Taquaral (quartzo + albita + moscovita + ilita + caulinita + clorita). No entanto, o conteúdo mineralógico do Membro Assistência apresentou alterações, provavelmente causadas pela intrusão do diabásio (talco + pirofilita + calcita). O talco e a calcita foram formados devido à reação entre dolomita e quartzo, enquanto a pirofilita foi o produto da reação entre a caulinita e o quartzo. Palavras-chave: Bacia Sedimentar. Intrusões Ígneas. Metamorfização de sedimentos. Reações mineralógicas. XRD. SEM / EDS.
4

SANDY, MICHAEL R. "Sedimentary microrhythms." Nature 318, no. 6041 (November 1985): 81. http://dx.doi.org/10.1038/318081a0.

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Tankard, Anthony J. "Sedimentary Petrology." Sedimentary Geology 152, no. 1-2 (September 2002): 159–60. http://dx.doi.org/10.1016/s0037-0738(01)00254-8.

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Föllmi, Karl B. "Sedimentary condensation." Earth-Science Reviews 152 (January 2016): 143–80. http://dx.doi.org/10.1016/j.earscirev.2015.11.016.

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Rickard, David, Marc Mussmann, and Jeffrey A. Steadman. "Sedimentary Sulfides." Elements 13, no. 2 (April 2017): 117–22. http://dx.doi.org/10.2113/gselements.13.2.117.

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8

Postma, George. "Sedimentary basins." Earth-Science Reviews 34, no. 4 (August 1993): 276–77. http://dx.doi.org/10.1016/0012-8252(93)90064-e.

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Postma, George. "Sedimentary petrology." Sedimentary Geology 84, no. 1-4 (April 1993): 249. http://dx.doi.org/10.1016/0037-0738(93)90064-c.

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Morad, Sadoon. "Sedimentary petrography." Sedimentary Geology 92, no. 3-4 (September 1994): 292–94. http://dx.doi.org/10.1016/0037-0738(94)90114-7.

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You might also be interested in the extended bibliographies on the topic 'Sedimentary' for particular source types:
Journal articles Dissertations / Theses Books

Dissertations / Theses on the topic "Sedimentary":

1

Tavares, Sandra Aparecida Simionato 1969. "Fósseis do afloramento Santa Irene, cretácio superior da Bacia Bauru = inferências paleoecológicas." [s.n.], 2011. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287322.

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Orientadores: Frésia Soledad Ricardi Torres Branco, Ismar de Souza Carvalho
Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências
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Resumo: O Afloramento Santa Irene tem sido considerado um dos mais significativos da Bacia Bauru, na Formação Adamantina, pela abundancia e boa conservação de fósseis associados ali encontrados, como dentes isolados de arcossauros carnívoros associados a fósseis de um dinossauro saurópode herbívoro. Os fósseis foram coletados nos anos de 1997 e 1998, na área rural do Município de Monte Alto - SP, e hoje compõem parte do acervo do Museu de Paleontologia de Monte Alto. Os dentes isolados de tal afloramento são o principal material de estudo deste trabalho, que, acrescidos a outros dados obtidos através da análise das feições bioestratinômicas e geológicas da região, permitiram tecer uma interpretação paleoecológica para o Afloramento Santa Irene. Foram analisados vinte e seis exemplares de dentes de arcossauros carnívoros, sendo dezoito deles enquadrados como Theropoda e oito como elementos dentários pertencentes aos Crocodyliformes. Os dentes de Theropoda se distinguem daqueles de Crocodyliformes por serem os primeiros mais achatados lateralmente, além de apresentarem serrilhas. Foi possível constatar que quatorze dos dezoito exemplares classificados dentro da Subordem Theropoda apresentam características pertencentes à Ceratosauria, família Abelisauridae, e Maniraptora, família Dromaeosauridae. A coleção de dentes de Crocodyliformes coletados no afloramento Santa Irene consiste de oito exemplares em geral cônicos, com estriamento ao longo da carena, podendo ou não apresentar bordos serrilhados e seção basal arredondada, sendo possível classificá-los dentro da família Trematochampsidae. Os fósseis articulados e com pouco desgaste do Aeolosaurus indicam um soterramento parcial logo após a morte ou ainda na fase de destruição de seus elementos não esqueléticos. A observação do afloramento e do seu entorno permitiu deduzir que a região apresentava rios, possivelmente, entrelaçados com deposição sazonal de sedimentos e períodos de estabilidade com a formação de solos incipientes. Durante os períodos interdeposicionais e de formação do solo, nota-se a ocorrência da precipitação de minerais, dando origem à formação de calcretes, resultado de períodos secos marcantes. O afloramento Santa Irene representa a deposição de rios que formavam barras arenosas, nas quais diversos grupos de animais buscavam água e alimento. Conclui-se que estes animais habitavam ou transitavam por aquele ambiente, pois não há sinais de que os fósseis tenham sido transportados até o local no qual foram coletados, mas sim que a carcaça do Aeolosaurus serviu de alimentação para outros animais no local de sua morte. Desta forma, o material analisado permitiu a reconstituição de um retrato impar de um ecossistema a muito extinto
Abstract: The Santa Irene outcrop has been considered one of the most significant of the Bauru Basin, in the Adamantina formation, because of abundance and good preservation of associated fossils found there, as isolated teeth of carnivorous archosaurs associated with fossils of a herbivorous sauropod dinosaur. The fossils were found in 1997 and 1998, in rural areas of the city of Monte Alto - SP, and today compose the collection of the Museum of Paleontology of Monte Alto. The isolated teeth from this outcrop is the main material of this paper, which, together with other data obtained by analysis of biostratonomic and geological features of the region, allowed to make a paleoecological interpretation of the outcrop Santa Irene. Twenty-six copies of teeth of carnivorous archosaurs were analyzed, eighteen of them being classified as Theropodomorpho and eight teeth as belonging to Crocodyliformes. The teeth of Theropodomorpho can be distinguished from those to be the first Crocodyliformes as they are more flattened laterally, besides having serrations. It was found that fourteen of the eighteen specimens classified within the suborder Theropoda fit the characteristics belonging to Ceratosauria, family Abelisauridae and Maniraptora, family Dromaeosauridae. The collection of Crocodyliformes teeth collected from the outcrop Santa Irene consists of eight copies generally conical, with streaking along the keel, presenting or not serrated edges and rounded basal section, being possible to classify them within the family Trematochampsidae. The articulated and with little wear fossils of Aeolosaurus indicate a burial soon after death or during the destruction of its non-skeletal elements. The observation of the outcrop and its surroundings allow deducing that the region had braided rivers with seasonal sediment deposition and periods of stability with the formation of incipient soils. During no deposicional intervals periods and soil formation, can be noted the occurrence of precipitation of minerals, giving rise to the formation of calcrete, result of striking dry periods. The outcrop of St. Irene was formed by rivers that formed sand bars, in which various groups of animals tried to find food and water. It can be deduced that these animals lived or transited through that environment, because there is no evidence that the fossils were transported to the location in which they were collected, but that the Aeolosaurus remains served as food for other animals at his death location. Thus, the analyzed material allowed the reconstitution of an unique portrait of an ecosystem to long extinct
Mestrado
Geologia e Recursos Naturais
Mestre em Geociências
2

Souza, Agda Eunice de [UNESP]. "Argilominerais: influência dos aditivos (cinza de bagaço de cana-de-acúcar e rocha sedimentar) no processo de sinterização." Universidade Estadual Paulista (UNESP), 2008. http://hdl.handle.net/11449/88494.

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Foi estudada a influência de cinza de bagaço de cana e rocha sedimentar, adicionadas a um material argiloso, durante o processo de sinterização. O material argiloso e os aditivos foram caracterizados utilizando Difratometria de Raio X, Espectrometria de flurescência de Raio X e Análise Térmica. As amostras de cinza e rocha foram moídas, peneiradas a 0,088 mm e 0,125 mm, respectivamente, e incorporadas nos teores de 0, 20, 40, 60 e 80% em massa ao material argiloso. Foram preparados corpos de prova, prensados uniaxialmente a 19 Mpa, para cada corpo de prova, em uma prensa manual. As peças foram sinterizadas nas temperaturas de 500, 800, 900, 1000, 1100 e 1200º C, usando um forno tipo mufla e, posteriormente, submetidos a análise difratométrica e a ensaios físicos e mecânicos de absorção de água, retração linear de queima, massa específica aparente, perda de massa ao fogo, porosidade aparente e módulo de ruptura à flexão. A difratometria de raios X mostrou que a cinza é composta de material cristalino, predominantemente quartzo; a rocha sedimentar apresentou, além de quartzo, argilominerais micáceos e o material argiloso teve como fase principal a caulinita, contendo ainda hidróxido de alumínio e óxidos de ferro em menores concentrações. A análise química mostrou que, além do silício, a cinza e a rocha sedimentar apresentaram concentrações de óxidos de alumínio, potássio, cálcio, ferro e magnésio, enquanto que no material, os óxidos de silício, alumínio, ferro e titânio foram predominantes. As análises térmicas das diferentes misturas mostraram algumas reações que indicam transformação (inversão do quartzo), decomposição (perda de hidróxidos) e formação de fase (mulita) durante o aquecimento das amostras. Difração de raios X sustentou as hipóteses levantadas nos termograms das amostras...
The influence of sugar cane bagasse ash and sedimentary rock, added to clay material, in the sintering process was studied. The clay material and the additives were characterized by X-ray diffraction, X-ray spectroscopy and thermal analysis. The ash and rock samples were triturated, sieved to 0.088 mm and 0.125 mm, respectively, and incorporated at 0, 20, 40, 60, and 80% in the clay material. Prismatic probes were prepared, each pressed at 19 Mpa in a manual press. The pieces were sintered at 500, 800, 900, 1000, 1100 ans 1200ºC, and then characterized by X-ray diffraction and tests for water absorption, linear shrinkage, apparent specific mass, loss on ignition, apparent porosity and flexural strength. X-ray diffraction showed that the ash was composed of crystalline material, predominantly quartz; the sedimentary rock contained, besides quartz, mica; and the main phase of the clay material was kaolinite, but also contained aluminum hydroxide and iron oxides in lower concentrations. Chemical analysis showed that, besides silicon, the ash and the sedimentary rock also contained concentrations of oxides of aluminum, potassium, calcium, iron and magnesium, while in the clay material, silicon oxide, aluminum, iron and titanium were predominant. Thermal analyses of the different of the mixtures showed some reactions that indicated transformation (inversion of the quartz), decomposition (loss of hydroxides) and phase formation (mullite) during the heating of the samples. X-ray diffraction supported the findings in the thermal analysis of the analyzed samples. The tests showed that both the ash and sedimentary rock worsened the mechanical properties of the clay material, although they contributed to the improvement of other attributes. The presence of quartz in the ash and rock hindered the formation of the mullite phase formed during the sintering process... (Complete abstract click electronic acess below)
3

Souza, Agda Eunice de. "Argilominerais : influência dos aditivos (cinza de bagaço de cana-de-acúcar e rocha sedimentar) no processo de sinterização /." Bauru : [s.n.], 2008. http://hdl.handle.net/11449/88494.

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Resumo: Foi estudada a influência de cinza de bagaço de cana e rocha sedimentar, adicionadas a um material argiloso, durante o processo de sinterização. O material argiloso e os aditivos foram caracterizados utilizando Difratometria de Raio X, Espectrometria de flurescência de Raio X e Análise Térmica. As amostras de cinza e rocha foram moídas, peneiradas a 0,088 mm e 0,125 mm, respectivamente, e incorporadas nos teores de 0, 20, 40, 60 e 80% em massa ao material argiloso. Foram preparados corpos de prova, prensados uniaxialmente a 19 Mpa, para cada corpo de prova, em uma prensa manual. As peças foram sinterizadas nas temperaturas de 500, 800, 900, 1000, 1100 e 1200º C, usando um forno tipo mufla e, posteriormente, submetidos a análise difratométrica e a ensaios físicos e mecânicos de absorção de água, retração linear de queima, massa específica aparente, perda de massa ao fogo, porosidade aparente e módulo de ruptura à flexão. A difratometria de raios X mostrou que a cinza é composta de material cristalino, predominantemente quartzo; a rocha sedimentar apresentou, além de quartzo, argilominerais micáceos e o material argiloso teve como fase principal a caulinita, contendo ainda hidróxido de alumínio e óxidos de ferro em menores concentrações. A análise química mostrou que, além do silício, a cinza e a rocha sedimentar apresentaram concentrações de óxidos de alumínio, potássio, cálcio, ferro e magnésio, enquanto que no material, os óxidos de silício, alumínio, ferro e titânio foram predominantes. As análises térmicas das diferentes misturas mostraram algumas reações que indicam transformação (inversão do quartzo), decomposição (perda de hidróxidos) e formação de fase (mulita) durante o aquecimento das amostras. Difração de raios X sustentou as hipóteses levantadas nos termograms das amostras... (Resumo completo, clicar acesso eletrônico abaixo)
Abstract: The influence of sugar cane bagasse ash and sedimentary rock, added to clay material, in the sintering process was studied. The clay material and the additives were characterized by X-ray diffraction, X-ray spectroscopy and thermal analysis. The ash and rock samples were triturated, sieved to 0.088 mm and 0.125 mm, respectively, and incorporated at 0, 20, 40, 60, and 80% in the clay material. Prismatic probes were prepared, each pressed at 19 Mpa in a manual press. The pieces were sintered at 500, 800, 900, 1000, 1100 ans 1200ºC, and then characterized by X-ray diffraction and tests for water absorption, linear shrinkage, apparent specific mass, loss on ignition, apparent porosity and flexural strength. X-ray diffraction showed that the ash was composed of crystalline material, predominantly quartz; the sedimentary rock contained, besides quartz, mica; and the main phase of the clay material was kaolinite, but also contained aluminum hydroxide and iron oxides in lower concentrations. Chemical analysis showed that, besides silicon, the ash and the sedimentary rock also contained concentrations of oxides of aluminum, potassium, calcium, iron and magnesium, while in the clay material, silicon oxide, aluminum, iron and titanium were predominant. Thermal analyses of the different of the mixtures showed some reactions that indicated transformation (inversion of the quartz), decomposition (loss of hydroxides) and phase formation (mullite) during the heating of the samples. X-ray diffraction supported the findings in the thermal analysis of the analyzed samples. The tests showed that both the ash and sedimentary rock worsened the mechanical properties of the clay material, although they contributed to the improvement of other attributes. The presence of quartz in the ash and rock hindered the formation of the mullite phase formed during the sintering process... (Complete abstract click electronic acess below)
Orientador: Elson Longo da Silva
Coorientador: Silvio Rainho Teixeira
Banca: Carla dos Santos Riccardi
Banca: Marcos Augusto de Lima Nobre
O Programa de Pós-Graduação em Ciência e Tecnologia de Materiais, PosMat, tem caráter institucional e integra as atividades de pesquisa em materiais de diversos campi da Unesp
Mestre
4

Newman, Robert. "Mechanics of sedimentary basin extension." Thesis, University of Oxford, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305480.

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Wilson, N. P. "Thermal studies in sedimentary basins." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383208.

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Dodd, Matthew S. "Biosignatures in Precambrian sedimentary rocks." Thesis, University College London (University of London), 2018. http://discovery.ucl.ac.uk/10055383/.

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The overarching goal of this work was to trace the origins of organic matter as a possible biosignature for early life on Earth. This work documented the petrological, structural, isotopic, elemental and molecular properties of organic matter, in a suite of sediments ranging from the Eoarchean to the Phanerozoic. Particular attention was paid to iron formations which form a major part of the Precambrian sedimentological record. Optical and micro-Raman spectroscopy were used to document the petrological occurrences of organic matter and its associated diagenetic features. Focused ion beam and transmission electron microscopy were used to detail the nanoscale structures of the organic matter. Mass spectroscopic techniques were utilised to measure the isotopic, elemental and molecular properties of organic matter and its petrographically associated carbonate. The timing and possible mechanisms of organic matter formation were investigated and evaluated, against the observed attributes of the organic matter. This work has documented organic matter forming key mineral associations with apatite and carbonate, which point to the diagenetic recycling of biogenic carbon. The diagenetic cycling of organic matter is proposed, to fuel the formation of granules during organic matter, iron and sulphur cycling. This cycling is hypothesised to lead to heterogeneity in organic matter structure and preservation in sediments. Additionally, this work has demonstrated that fluid deposited graphite in metamorphosed sediments may represent redistributed, syngenetic organic matter, shedding light on the controversial origins of graphite biosignatures in Earths oldest rocks. Finally, a detailed study of microfossil structures and their associations with organic matter and biominerals in iron formations was conducted to provide evidence for the preservation of Proterozoic microfossils, and the earliest signs of life on Earth.
7

Turner, Jonathan David. "The subsidence of sedimentary basins." Thesis, University of Edinburgh, 1997. http://hdl.handle.net/1842/13150.

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Theoretical models for the evolution of extensional sedimentary basins make a number of simple, testable predictions for subsidence behaviour. These are that active extension (the syn-rift) will generally be accompanied by rapid subsidence on the downthrown side of normal faults. Once faulting has ceased (the post-rift) the entire basin is predicted to subside at an exponentially decreasing rate, driven by the cooling and thickening of the lithosphere. The aim of this thesis is to determine the significance of second-order departures from this predicted subsidence. Three periods of North Sea subsidence appear to violate these simple predictions: anomalously slow Late Jurassic/Early Cretaceous subsidence, which marks the syn-rift/post-rift transition, and two periods of accelerated post-rift subsidence during the Early Paleogene and Plio-Quaternary. Subsidence data from over 300 boreholes from several basins with different rifting histories on the Northwest European continental plate have been analysed to determine the spatial and temporal distribution of these and other second-order subsidence anomalies. Uncertainties and errors in the observed subsidence calculations cannot explain the anomalous behaviour recognised. The periods of apparently anomalous subsidence are, instead, shown to be the result of geological or tectonic processes that modified either the subsidence history or record of subsidence of the basins studied. Apparent slow Late Jurassic/Early Cretaceous subsidence in the North Sea was the result of well siting and sediment starvation. Analysis of wells from the downthrown side of normal faults in several basins reveals an excellent correlation between rapid subsidence (often >1000m in 10My) and active extension (as documented from other sources of geological information). This was obscured by intense sediment starvation (sedimentation rates <20m/My) in the Central North Sea during Late Jurassic times which generated the apparent subsidence anomaly. Sedimentation rate maps reveal an expansion of the area of sediment starvation during late Jurassic times and into the Early Cretaceous. Cretaceous to Recent sedimentation patterns were then dominated by the interplay between the location and erosion history of extra-basinal sediment source areas and the remnant underfilled Jurassic rift topography.
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Symons, William Owen. "Sedimentary processes in submarine canyons." Thesis, University of Southampton, 2017. https://eprints.soton.ac.uk/416834/.

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Submarine canyons are one of the most dramatic morphological features on continental margins and enable sediment transport from the shelf to the deep sea; however, the exact processes operating within submarine canyons are poorly understood. Much of our understanding of the dynamics of sediment-laden flows in submarine canyons results from making inferences from the deposits that they leave behind in the geological record. This thesis aimed to better understand what deposits can reveal about flow processes and ultimately to test the validity of this approach for reconstructing flow dynamics. This aim was achieved by 1) analysing seafloor bedforms, 2) the detailed lithological and ichnological analysis of submarine canyon deposits, and 3) utilising turbidity current monitoring data. Construction and analysis of a global database of seafloor bedforms suggests that bedforms across all scales and a wide variety of settings can be generated by supercritical flows. The most complete dataset of monitored turbidity currents in a submarine canyon was combined with precisely located vibracores collected in Monterey Canyon. The combination of these datasets demonstrates that deposits can be used to accurately infer flow properties, and the data were further used to develop a new three-part model for turbidity current behaviour: 1) flows begin as thin, high-concentration highly energetic flows; 2) the flows become more dilute with an expanding head; and 3) the flow rapidly thickens along its length. This new model of turbidity current behaviour, along with understanding the frequency of these events, explains the distribution of benthic communities in Monterey Canyon based on the biogenic sedimentary structures identified within the sedimentary cores.
9

Bastow, Trevor. "Sedimentary Processes Involving Aromatic Hydrocarbons." Thesis, Curtin University, 1998. http://hdl.handle.net/20.500.11937/833.

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Sedimentary organic matter contains many compounds that have no obvious biogenic precursors, so their formation and occurrence are of geochemical interest. The first part of this thesis (chapters 2-5) discusses the results obtained from studying hydrocarbon racemates. Some of the compounds identified are also suggested as intermediates in the formation of alkylnaphthalenes identified in chapters 6-7. The second part of this thesis (chapters 6-11) covers the identification of a range of alkylnaphthalenes and alkylphenanthrenes in sedimentary organic matter. Possible pathways for the formation of these hydrocarbons are outlined and their application as probes into the processes of petroleum formation are described.In chapter 2 the use of permethylated cyclodextrin capillary gas chromatography columns to separate hydrocarbon racemates are reported. Chapter 3 reports the synthesis of 1,2,2,5-tetramethyltetralin and 1,2,2,5,6-pentamethyltetralin and identifies them as racemates in crude oil. They are proposed as intermediates in the formation of sedimentary alkylnaphthalenes (identified in chapters 6 and 7).The identification of isodihydro-ar-curcumene in sedimentary organic matter is described in chapters 4 and 5. It co-occurs in crude oil with dihydro-ar-curcumene and is suggested to originate from this compound via a sedimentary rearrangement process. Chiral GC-MS techniques have been used to show the presence of both enantiomers of these compounds in crude oils. The elution order of the enantiomers has been established using reference compounds of known configuration. The effects of maturity and biodegradation on dihydro-ar-curcumene and isodihydro-ar-curcumene enantiomers is reported. Optically pure dihydro-ar-curcumene from natural products undergoes rapid racemisation in the subsurface, yielding a racemic mixture before the onset of significant oil formation. 1,2-Alkyl shifts on the aromatic ring also begin at an early stage to yield isodihydro-ar-curcumene and these processes continue with increasing maturity. Laboratory experiments using proton and clay catalysts (Lewis acid catalyst) show that the alkyl shift reaction is catalysed by both proton and Lewis acids, and racemisation is only catalysed by Lewis acids. A moderately biodegraded crude oil has been shown to be depleted in the R enantiomer of dihydro-ar-curcumene and an extensively degraded oil has dihydro-ar-curcumene depleted relative to isodihydro-ar-curcumene.The identification of a number alkylnaphthalenes and their possible origins in sedimentary organic matter is described in chapters 6 and 7. In chapter 6 a previously unreported tetramethylnaphthalene (TeMN) was identified in petroleum. This compound is structurally similar to bicyclic compounds of microbial origin and these are suggested as a likely source, via a tetralin intermediate identified in chapter 3. In chapter 7 isomeric pentamethylnaphthalenes previously unreported in sedimentary organic matter are reported. These isomeric pentamethylnaphthalenes (PMNs) were identified in a number of crude oils and sediments, ranging in age from Proterozoic to Tertiary. 1,2,3,5,6-PMN is suggested to form predominantly from the aromatisation of drimanoid precursors via 1,2,2,5,6-pentamethyltetralin identified in chapter 3. In laboratory experiments, the other pentamethylnaphthalenes were generated from 1,2,3,5,6-PMN in proportions that reflect the relative stability of the isomers. By analogy, the other PMNs in sediments are suggested to arise via acid catalysed isomerisation or transalkylation processes. A maturity parameter was developed based on laboratory experiments in conjunction with observed distributions of pentamethylnaphthalenes.The formation of alkylnaphthalenes and alkylphenanthrenes through a methylation process is discussed in chapters 8-10. Several crude oils and shales which contain anomalously high concentrations of 1,6-dimethylnaphthalene, 1,2,5-trimethylnaphthalene, 1,2,7-trimethylnaphthalene, 1,2,3,5-tetramethylnaphthalene, 1,2,3,5,6-pentamethylnaphthalene, 2-methyl-6-isopropyl-1(4-methylpentyl)naphthalene, phenanthrene, 1-methylphenanthrene, 1,7-dimethylphenanthrene and retene have been shown to contain relatively high concentrations of their corresponding methylated counterparts. In laboratory experiments carried out under mild conditions, each of the alkylnaphthalenes and alkylphenanthrenes have been shown to be methylated in specific positions when heated with a methyl donor in the presence of a clay catalyst. These observations have been interpreted as evidence for a sedimentary methylation process.The effect of biodegradation on alkylnaphthalenes and alkylphenanthrenes formed from sedimentary methylation is described in chapter 11. Land-plant-derived aromatic hydrocarbons with a range of susceptibilities to reservoir biodegradation have been identified in crude oils. These compounds are the result of reactions of natural products involving aromatisation, rearrangement and methylation in the sediments (chapters 9 and 10). They are therefore suggested as markers for land-plants in severely biodegraded oils in which most of the other biologically derived compounds cannot be recognised. The order of biodegradability of these compounds has been assessed relative to their non-methylated counterparts namely 6-isopropyl-2-methyl-1-(4-methylpentyl)naphthalene and retene. The order of degradation of the four compounds is : retene < 9-methylretene ~ 6-isopropyl-2-methyl-1-(4-methylpentyl)naphthalene > 6-isopropyl-2,4-dimethyl-1-(4-methylpentyl)naphthalene. These results have been used to assess that a crude oil is a mixture of severely biodegraded and less biodegraded crude oil.
10

Bastow, Trevor. "Sedimentary Processes Involving Aromatic Hydrocarbons." Curtin University of Technology, School of Applied Chemistry, 1998. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=9379.

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Abstract:
Sedimentary organic matter contains many compounds that have no obvious biogenic precursors, so their formation and occurrence are of geochemical interest. The first part of this thesis (chapters 2-5) discusses the results obtained from studying hydrocarbon racemates. Some of the compounds identified are also suggested as intermediates in the formation of alkylnaphthalenes identified in chapters 6-7. The second part of this thesis (chapters 6-11) covers the identification of a range of alkylnaphthalenes and alkylphenanthrenes in sedimentary organic matter. Possible pathways for the formation of these hydrocarbons are outlined and their application as probes into the processes of petroleum formation are described.In chapter 2 the use of permethylated cyclodextrin capillary gas chromatography columns to separate hydrocarbon racemates are reported. Chapter 3 reports the synthesis of 1,2,2,5-tetramethyltetralin and 1,2,2,5,6-pentamethyltetralin and identifies them as racemates in crude oil. They are proposed as intermediates in the formation of sedimentary alkylnaphthalenes (identified in chapters 6 and 7).The identification of isodihydro-ar-curcumene in sedimentary organic matter is described in chapters 4 and 5. It co-occurs in crude oil with dihydro-ar-curcumene and is suggested to originate from this compound via a sedimentary rearrangement process. Chiral GC-MS techniques have been used to show the presence of both enantiomers of these compounds in crude oils. The elution order of the enantiomers has been established using reference compounds of known configuration. The effects of maturity and biodegradation on dihydro-ar-curcumene and isodihydro-ar-curcumene enantiomers is reported. Optically pure dihydro-ar-curcumene from natural products undergoes rapid racemisation in the subsurface, yielding a racemic mixture before the onset of significant oil formation. ++
1,2-Alkyl shifts on the aromatic ring also begin at an early stage to yield isodihydro-ar-curcumene and these processes continue with increasing maturity. Laboratory experiments using proton and clay catalysts (Lewis acid catalyst) show that the alkyl shift reaction is catalysed by both proton and Lewis acids, and racemisation is only catalysed by Lewis acids. A moderately biodegraded crude oil has been shown to be depleted in the R enantiomer of dihydro-ar-curcumene and an extensively degraded oil has dihydro-ar-curcumene depleted relative to isodihydro-ar-curcumene.The identification of a number alkylnaphthalenes and their possible origins in sedimentary organic matter is described in chapters 6 and 7. In chapter 6 a previously unreported tetramethylnaphthalene (TeMN) was identified in petroleum. This compound is structurally similar to bicyclic compounds of microbial origin and these are suggested as a likely source, via a tetralin intermediate identified in chapter 3. In chapter 7 isomeric pentamethylnaphthalenes previously unreported in sedimentary organic matter are reported. These isomeric pentamethylnaphthalenes (PMNs) were identified in a number of crude oils and sediments, ranging in age from Proterozoic to Tertiary. 1,2,3,5,6-PMN is suggested to form predominantly from the aromatisation of drimanoid precursors via 1,2,2,5,6-pentamethyltetralin identified in chapter 3. In laboratory experiments, the other pentamethylnaphthalenes were generated from 1,2,3,5,6-PMN in proportions that reflect the relative stability of the isomers. By analogy, the other PMNs in sediments are suggested to arise via acid catalysed isomerisation or transalkylation processes. A maturity parameter was developed based on laboratory experiments in conjunction with observed distributions of pentamethylnaphthalenes.The formation of alkylnaphthalenes and alkylphenanthrenes through a ++
methylation process is discussed in chapters 8-10. Several crude oils and shales which contain anomalously high concentrations of 1,6-dimethylnaphthalene, 1,2,5-trimethylnaphthalene, 1,2,7-trimethylnaphthalene, 1,2,3,5-tetramethylnaphthalene, 1,2,3,5,6-pentamethylnaphthalene, 2-methyl-6-isopropyl-1(4-methylpentyl)naphthalene, phenanthrene, 1-methylphenanthrene, 1,7-dimethylphenanthrene and retene have been shown to contain relatively high concentrations of their corresponding methylated counterparts. In laboratory experiments carried out under mild conditions, each of the alkylnaphthalenes and alkylphenanthrenes have been shown to be methylated in specific positions when heated with a methyl donor in the presence of a clay catalyst. These observations have been interpreted as evidence for a sedimentary methylation process.The effect of biodegradation on alkylnaphthalenes and alkylphenanthrenes formed from sedimentary methylation is described in chapter 11. Land-plant-derived aromatic hydrocarbons with a range of susceptibilities to reservoir biodegradation have been identified in crude oils. These compounds are the result of reactions of natural products involving aromatisation, rearrangement and methylation in the sediments (chapters 9 and 10). They are therefore suggested as markers for land-plants in severely biodegraded oils in which most of the other biologically derived compounds cannot be recognised. The order of biodegradability of these compounds has been assessed relative to their non-methylated counterparts namely 6-isopropyl-2-methyl-1-(4-methylpentyl)naphthalene and retene. The order of degradation of the four compounds is : retene < 9-methylretene ~ 6-isopropyl-2-methyl-1-(4-methylpentyl)naphthalene > 6-isopropyl-2,4-dimethyl-1-(4-methylpentyl)naphthalene. These results have been used to assess that a crude oil is a mixture of severely biodegraded and ++
less biodegraded crude oil.
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Books on the topic "Sedimentary":

1

Collinson, J. D. Sedimentary structures. 2nd ed. London: Unwin Hyman, 1989.

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Stokes, William Lee. Sedimentary rocks. [s.l: s.n.], 1985.

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Oxlade, Chris. Sedimentary rocks. Chicago: Heinemann Library, 2011.

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Oxlade, Chris. Sedimentary rock. Oxford: Raintree, 2012.

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Einsele, Gerhard. Sedimentary Basins. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5.

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Einsele, Gerhard. Sedimentary Basins. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4.

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Stewart, Melissa. Sedimentary rocks. Oxford: Heinemann Library, 2003.

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Faulkner, Rebecca. Sedimentary rock. Oxford: Raintree, 2007.

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Oxlade, Chris. Sedimentary rocks. Chicago: Heinemann Library, 2011.

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Collinson, J. D. Sedimentary structures. 3rd ed. Harpenden, Hertfordshire: Terra, 2006.

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Book chapters on the topic "Sedimentary":

1

Scheffers, Anja M., Sander R. Scheffers, and Dieter H. Kelletat. "Sedimentary Coasts." In Coastal Research Library, 125–80. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-0738-2_5.

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Scheck-Wenderoth, Magdalena. "Sedimentary Basins." In Encyclopedia of Solid Earth Geophysics, 1–13. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10475-7_216-1.

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Bjørlykke, Knut Olav. "Sedimentary Facies." In Sedimentology and Petroleum Geology, 55–111. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-72592-0_5.

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Bjørlykke, Knut. "Sedimentary Geochemistry." In Petroleum Geoscience, 87–111. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-02332-3_3.

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Boggiani, Paulo César. "Sedimentary Rocks." In Encyclopedia of Earth Sciences Series, 1–3. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-12127-7_253-1.

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Arndt, Nicholas. "Sedimentary Rock." In Encyclopedia of Astrobiology, 1495. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_1416.

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Kendall, Christopher George St Clement. "Sedimentary Sequence." In Encyclopedia of Marine Geosciences, 768–73. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_177.

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Leavitt, Peter R., and Dominic A. Hodgson. "Sedimentary Pigments." In Tracking Environmental Change Using Lake Sediments, 295–325. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/0-306-47668-1_15.

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Jelgersma, Saskia. "Sedimentary Basins." In Encyclopedia of Earth Sciences Series, 1517–23. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_280.

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Fernandes, Isabel, Maarten A. T. M. Broekmans, Maria dos Anjos Ribeiro, and Ian Sims. "Sedimentary Rocks." In Petrographic Atlas: Characterisation of Aggregates Regarding Potential Reactivity to Alkalis, 43–101. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-017-7383-6_3.

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Conference papers on the topic "Sedimentary":

1

O'Sullivan, Gary, J. Daly, John Murray, Aodhán Ó'Gogáin, David Chew, Eszter Badenszki, Brendan Hoare, Paul Guyett, and Foteini Drakou. "Linking sedimentary phosphate U-Pb ages to syn-sedimentary processes." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7024.

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Bartley, Julie K., and Thomas A. Hickson. "LEARNING TO BE A SEDIMENTARY GEOLOGIST BY BEING A SEDIMENTARY GEOLOGIST." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-313055.

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Mboya, V. E. "Sedimentary Basins Prospective for Hydrocarbons." In Third EAGE Eastern Africa Petroleum Geoscience Forum. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201702431.

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Bates, C. Richard. "Transverse Isotropy in Sedimentary Sequences." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 1991. Environment and Engineering Geophysical Society, 1991. http://dx.doi.org/10.4133/1.2921924.

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Borja, Ronaldo I., Pablo F. Sanz, and David D. Pollard. "Ductile Folding of Sedimentary Rocks." In GeoCongress 2006. Reston, VA: American Society of Civil Engineers, 2006. http://dx.doi.org/10.1061/40803(187)187.

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Lawrence, David T., Mark Doyle, Sigmund Snelson, and W. T. Horsfield. "Stratigraphic modeling of sedimentary basins." In SEG Technical Program Expanded Abstracts 1987. Society of Exploration Geophysicists, 1987. http://dx.doi.org/10.1190/1.1891985.

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Wang, Zhijing (Zee). "Seismic anisotropy in sedimentary rocks." In SEG Technical Program Expanded Abstracts 2001. Society of Exploration Geophysicists, 2001. http://dx.doi.org/10.1190/1.1816460.

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Olneva, T. V., and E. Milei. "Reservoir Modelling of Paleochanels Based on Seismic Trend." In Second Conference on Forward Modelling of Sedimentary Systems. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600371.

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Eggenhuisen, J. T., J. de Leeuw, F. Pohl, and M. J. B. Cartigny. "Keynote Speech - Taking Physical Modelling of Deepwater Depositional Systems Forwards." In Second Conference on Forward Modelling of Sedimentary Systems. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600380.

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Mullins, J. R., J. A. Howell, S. J. Buckley, and C. Kehl. "A Novel Workflow for Building Multiple Point Statistics Training Images from Virtual Outcrops." In Second Conference on Forward Modelling of Sedimentary Systems. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600354.

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Reports on the topic "Sedimentary":

1

Hulbert, L. J. Sedimentary nickel sulphides. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/207972.

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Lydon, J. W. Sedimentary exhalative sulphides (Sedex). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/207970.

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Mossop, G. D., K. E. Wallace-Dudley, G. G. Smith, and J. C. Harrison. Sedimentary basins of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215559.

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Yuen, David A. Physical Modelling of Sedimentary Basin. Office of Scientific and Technical Information (OSTI), April 2003. http://dx.doi.org/10.2172/899950.

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Kastaschuk, R. A., J. L. Luternauer, and M. A. Church. Sedimentary processes in the estuary. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/210036.

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Bell, J. S. Stress in Sedimentary Basins Seminar. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/130791.

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Amos, C. L. Chapter 11: Modern Sedimentary Processes. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/132718.

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Vogel, Allan. Some Relationships Between Sedimentary Trace Metal Concentrations and Freshwater Phytoplankton and Sedimentary Diatom Species Composition. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.1294.

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Sangster, D. F. World sedimentary exhalative (Sedex) deposit database. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296423.

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Syvitski, J. P. M. Modelling the sedimentary fill of basins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128089.

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