Auswahl der wissenschaftlichen Literatur zum Thema „Coastal sedimentary depositional environments“
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Zeitschriftenartikel zum Thema "Coastal sedimentary depositional environments"
Stoupakova, Antonina V., Nataliya I. Korobova, Alina V. Mordasova, Roman S. Sautkin, Ekaterina D. Sivkova, Maria A. Bolshakova, Mikhail E. Voronin et al. „Depositional environments as a framework for genetic classification of the basic criteria of petroleum potential“. Georesursy 25, Nr. 2 (30.06.2023): 75–88. http://dx.doi.org/10.18599/grs.2023.2.6.
Der volle Inhalt der QuelleSafaei, Mohammad, Asadollah Mahboubi, Soroush Modabberi und Reza Moussavi-Harami. „Palaeoenvironment, sequence stratigraphy and palaeogeography of the Lower Cretaceous deposits of Mehdi Abad, Yazd Block, Central Iran“. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 295, Nr. 1 (01.01.2020): 61–89. http://dx.doi.org/10.1127/njgpa/2020/0868.
Der volle Inhalt der QuelleKhabidov, A. Sh, L. A. Zhindarev, E. A. Fedorova und K. V. Marusin. „COASTAL ZONE OF LARGE MAN-MADE LAKES (Paper 2. DEPOSITIONAL SEDIMENTARY ENVIRONMENTS)“. Geomorphology RAS, Nr. 3 (18.03.2015): 23. http://dx.doi.org/10.15356/0435-4281-2014-3-23-29.
Der volle Inhalt der QuelleNayak, Ganapati Narayan. „Changing Tropical Estuarine Sedimentary Environments with Time and Metals Contamination, Cest Coast of India“. Journal of The Indian Association of Sedimentologists 38, Nr. 2 (31.12.2021): 63–78. http://dx.doi.org/10.51710/jias.v38i2.141.
Der volle Inhalt der QuelleEzeh, Sunny C., Wilfred A. Mode, Berti M. Ozumba und Nura A. Yelwa. „Sedimentology and ichnology of Neogene Coastal Swamp deposits in the Niger Delta Basin, Nigeria“. Geologos 22, Nr. 3 (01.09.2016): 191–200. http://dx.doi.org/10.1515/logos-2016-0020.
Der volle Inhalt der QuelleCheng, Wufeng, Shenliang Chen, Xiaojing Zhong und Shaohua Zhao. „Identification of Sedimentary Environments through Dynamic Image Analysis of the Particle Morphology of Beach Sediments on the East and West Coasts of Hainan Island in South China“. Water 15, Nr. 15 (25.07.2023): 2680. http://dx.doi.org/10.3390/w15152680.
Der volle Inhalt der QuelleOwens, R., A. Kelman, K. Khider, T. Bernecker und B. Bradshaw. „Late Permian–Early Triassic depositional history in the southern Bonaparte Basin: new biostratigraphic insights into reservoir heterogeneity“. APPEA Journal 61, Nr. 2 (2021): 699. http://dx.doi.org/10.1071/aj20111.
Der volle Inhalt der QuelleH.M.A.Eltayib, Sadam, El Sheikh M. Abdelrahman, Ali S. M. Ibrahim und Omar A. O. Al-Imam. „Sedimentary environments and lithofacies distribution of zeit formation, red sea- Sudan“. International Journal of Advanced Geosciences 7, Nr. 1 (05.05.2019): 10. http://dx.doi.org/10.14419/ijag.v7i1.19712.
Der volle Inhalt der QuelleHtwe, Paike, Sugeng Sapto Surjono, Donatus Hendra Amijaya und Kyuro Sasaki. „DEPOSITIONAL MODEL OF NGRAYONG FORMATION IN MADURA AREA, NORTH EAST JAVA BASIN, INDONESIA“. Journal of Applied Geology 7, Nr. 2 (26.07.2015): 51. http://dx.doi.org/10.22146/jag.26947.
Der volle Inhalt der QuelleAlshammari, Bassam, Nigel P. Mountney, Luca Colombera und Mohammed A. Al-Masrahy. „Sedimentology and stratigraphic architecture of a fluvial to shallow-marine succession: The Jurassic Dhruma Formation, Saudi Arabia“. Journal of Sedimentary Research 91, Nr. 7 (30.07.2021): 773–94. http://dx.doi.org/10.2110/jsr.2020.077.
Der volle Inhalt der QuelleDissertationen zum Thema "Coastal sedimentary depositional environments"
McCaffrey, Mark A. „Sedimentary lipids as indicators of depositional conditions in the coastal Peruvian upwelling regime“. Thesis, Massachusetts Institute of Technology, 1990. http://hdl.handle.net/1721.1/54963.
Der volle Inhalt der QuelleVita.
Includes bibliographical references. Includes bibliographical references.
by Mark A. McCaffrey.
Ph.D.
Ranasinghage, Pradeep Nalaka. „Holocene Coastal Development in Southeastern-Eastern Sri Lanka: Paleo-Depositional Environments and Paleo-coastal Hazards“. Kent State University / OhioLINK, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=kent1286816740.
Der volle Inhalt der QuelleRaine, Pamela. „Sedimentary processes and depositional environments in Caldera Lakes : Scafell (U.K.) and La Primavera (Mexico) Calderas“. Thesis, University of Liverpool, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.251484.
Der volle Inhalt der QuelleFryer, Rosemarie. „Quantification of the Bed-Scale Architecture of Submarine Depositional Environments and Application to Lobe Deposits of the Point Loma Formation, California“. Thesis, Colorado School of Mines, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10844938.
Der volle Inhalt der QuelleSubmarine-fan deposits form the largest sediment accumulations on Earth and host significant reservoirs for hydrocarbons. While many studies of ancient fan deposits qualitatively describe lateral architectural variability (e.g., axis-to-fringe, proximal-to-distal), these relationships are rarely quantified. In order to enable comparison of key relationships that control the lateral architecture of submarine depositional environments, I digitized published bed-scale outcrop correlation panels from five different environments (channel, levee, lobe, channel-lobe-transition-zone, basin plain). Measured architectural parameters (bed thickness, bed thinning rates, lateral correlation distance, net-to-gross) provide a quantitative framework to compare facies architecture between environments. The results show that sandstone and/or mudstone bed thickness alone or net-to-gross do not reliably differentiate between environments. However, environments are distinguishable using a combination of thinning rate, bed thickness, and correlation distance. For example, channel deposits generally display thicker sandstone beds than mudstone beds whereas levees display the opposite trend. Lobe deposits display the most variability in all parameters, and thus would be the most difficult to identify in the subsurface. I sub-classified lobe deposits to provide a more detailed analysis into unconfined, semiconfined and confined settings. However, the results for semiconfined lobes indicate that the degree of lobe confinement and subenvironment is not easily interpretable at the outcrop scale. This uncertainty could be partially caused by subjectivity of qualitative interpretations of environment, which demonstrates the need for more quantitative studies of bed-scale heterogeneity. These results can be used to constrain forward stratigraphic models and reservoir models of submarine lobe deposits as well as other submarine depositional environments.
This work is paired with a case study to refine the depositional environment of submarine lobe strata of the Upper Cretaceous Point Loma Formation at Cabrillo National Monument near San Diego, California. These fine-grained turbidites have been interpreted as distal submarine lobe deposits. The strike-oriented, laterally-extensive exposure offers a rare opportunity to observe bed-scale architecture and facies changes in turbidites over 1 km lateral distance. Beds show subtle compensation, likely related to evolving seafloor topography, while lobe elements show drastic compensation. This indicates more hierarchical method of compensational stacking as the degree of bed compensation is small compared to the degree of element compensation. Thinning rates and bed thicknesses are not statistically different between lobe elements. This signifies that the lateral exposure is necessary to distinguish lobe elements and it would be extremely difficult to accurately interpret elements in the subsurface using 1D data (e.g., core). The grain size, mudstone to sandstone bed thicknesses, element/bed compensation, and lack of erosion observed in the Cabrillo National Monument exposures of the Point Loma Formation are most similar to values of semiconfined lobe deposits; hence, I reinterpret that these exposures occupy a more medial position, perhaps with some degree of confinement.
Baville, Paul. „Stratigraphic correlation uncertainty : On the impact of the sediment transport direction in computer-assisted multi-well correlation“. Electronic Thesis or Diss., Université de Lorraine, 2022. http://www.theses.fr/2022LORR0111.
Der volle Inhalt der QuelleSubsurface modeling is a way to predict the structure and the connectivity of stratigraphic units by honoring subsurface observations. These observations are commonly be sampled along wells at a large and sparse horizontal scale (kilometer-scale) but at a fine vertical scale (meter-scale). There are two types of well data: (1) well logs, corresponding to quasi-continuous (regular sampling) geophysical measurements along the well path (e.g., gamma ray, sonic, neutron porosity), and (2) regions, corresponding to categorical reservoir properties and defined by their top and bottom depths along the well path (e.g., biozones, structural zones, sedimentary facies). Markers are interpreted along the well path and can be associated in order to generate a consistent set of marker associations called well correlations. These well correlations may be generated manually (deterministic approach) by experts, but this may be prone to biases and does not ensure reproducibility. Well correlations may also be generated automatically (deterministic or probabilistic approach) by computing with an algorithm a large number of consistent well correlations and by ranking these realizations according to their likelihood. The likelihood of these computer-assisted well correlations are directly linked to the principle of correlation used to associate markers. This work introduces two principles of correlation, which tend to reproduce the chronostratigraphy and the depositional processes at the parasequence scale: (1) "a marker (described by facies and distality taken at the center of an interval having a constant facies and a constant distality) cannot be associated with another marker described by a depositionally deeper facies at a more proximal position, or a depositionally shallower facies at a more distal position", and (2) "the lower the difference between a chronostratigraphic interpolation (in between markers) and a conceptual depositional profile, the higher the likelihood of the marker association". These two principles of correlation are first benchmarked with analytical solutions and applied on synthetic cases. They have then been used (1) to predict the connectivity of stratigraphic units from well data without strong knowledge on depositional environments by inferring the correlation parameters, or (2) to evaluate the likelihood of a hypothetical depositional environment by generating stochastic realizations and assessing the uncertainties. The methods are applied on a siliciclastic coastal deltaic system targeting a Middle Jurassic reservoir in the South Viking Graben in the North Sea.This work enables (1) to define two specific principles of correlation defined by a few parameters that can be used to generate stochastically well correlations within coastal deltaic systems, and (2) to open the path towards a simple combination of specific principles of correlation to obtain a better characterization of coastal deltaic systems by assessing the uncertainties
Sidi, Franciscus Hasan. „Sequence stratigraphy, depositional environments, and reservoir geology of the middle-Miocene fluvio-deltaic succession in Badak and Nilam Fields, Kutai Basin, East Kalimantan, Indonesia“. Thesis, Queensland University of Technology, 1998.
Den vollen Inhalt der Quelle findenDelpomdor, Franck. „Sedimentology, geochemistry and depositional environments of the 1175-570 Ma carbonate series, Sankuru-Mbuji-Mayi-Lomami-Lovoy and Bas-Congo basins, Democratic Republic of Congo: new insights into late Mesoproterozoic and Neoproterozoic glacially- and/or tectonically-influenced sedimentary systems in equatorial Africa“. Doctoral thesis, Universite Libre de Bruxelles, 2013. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/209486.
Der volle Inhalt der Quellewas an enigmatic period characterized by the development of the first stable long-lived ~1.1-
0.9 Ga Rodinia and 550-500 Ma Gondwana supercontinents, global-scale orogenic belts,
extreme climatic changes (cf. Snowball Earth Hypothesis), the development of microbial
organisms facilitating the oxidizing atmosphere and explosion of eukaryotic forms toward the
first animals in the terminal Proterozoic. This thesis presents a multidisciplinary study of two
Neoproterozoic basins, i.e. Bas-Congo and Sankuru-Mbuji-Mayi-Lomami-Lovoy, in and around the Congo Craton including sedimentology, geochemistry, diagenesis, chemostratigraphy and radiometric dating of carbonate deposits themselves.
The Mbuji-Mayi Supergroup sequence deposited in a SE-NW trending 1500 m-thick siliciclastic-carbonate intracratonic failed-rift basin, extends from the northern Katanga Province towards the centre of the Congo River Basin. The 1000 m-thick carbonate succession is related to the evolution of a marine ramp submitted to evaporation, with ‘deep’ shaly basinal and low-energy carbonate outer-ramp environments, marine biohermal midramp (MF6) and ‘very shallow’ restricted tide-dominated lagoonal inner-ramp (MF7-MF9) settings overlain by lacustrine (MF10) and sabkha (MF11) environments, periodically
submitted to a river water source with a possible freshwater-influence. The sequence stratigraphy shows that the sedimentation is cyclic in the inner ramp with plurimetric ‘thin’ peritidal cycles (± 4 m on average) recording a relative sea level of a maximum of 4 m, with fluctuations in the range of 1-4 m. The outer/mid ramp subtidal facies are also cyclic with ‘thick’ subtidal cycles characterized by an average thickness of ± 17 m, with a probable sealevel
fluctuations around 10 to 20 m. The geochemistry approach, including isotopic and major/trace and REE+Y data, allows to infer the nature of the dolomitization processes operating in each carbonate subgroup, i.e dolomitization may be attributed to evaporative reflux of groundwater or to mixing zones of freshwater lenses. The latest alteration processes occured during the uplift of the SMLL Basin. New ages, including LA-ICP-MS U-Pb laser ablation data on detrital zircon grains retrieved in the lower arenaceous-pelitic sequence (BI group), combined with carbon and strontium isotopic analyses, yielded a new depositional time frame of the Mbuji-Mayi Supergroup between 1176 and 800 Ma reinforcing the formerly suggested correlation with the Roan Group in the Katanga Province.
In the Democratic Republic of Congo, the Sturtian-Marinoan interglacial period was previously related to pre-glacial carbonate-dominated shallow marine sedimentation of the Haut-Shiloango Subgroup with stromatolitic reefs at the transition between greenhouse (warm) and icehouse (cold) climate periods, commonly marked by worldwide glacigenic diamictites and cap carbonates. This thesis highlights that these deposists record as a deepening-upward evolution from storm-influenced facies in mid- and outer-ramps to deepwater environments, with emplacement of mass flow deposits in toe-of-slope settings controlled by synsedimentary faults. In absence of diagnostic glacial features, the marinoan Upper Diamictite Formation is interpreted as a continuous sediment gravity flow deposition along carbonate platform-margin slopes, which occurred along tectonically active continental margins locally influenced by altitude glaciers, developed after a rift–drift transition. The maximum depth of the deepening-upward facies is observed in the C2a member. The
shallowing-upward facies exibit a return of distally calcareous tempestites and semi-restricted to restricted peritidal carbonates associated with shallow lagoonal subtidal and intertidal zones submitted to detrital fluxes in the upper C2b to C3b members.
The geochemistry highlights (i) the existence of a δ13C-depth gradient of shallow-water and deep-water carbonates; (ii) the carbonate systems were deposited in oxic to suboxic conditions; and (iii) all samples have uniform flat non-marine shale-normalized REE+Y distributions reflecting
continental detrital inputs in nearshore environments, or that the nearshore sediments were
reworked from ’shallow’ inner to mid-ramp settings in deep-water slope and outer-ramp
environments, during the rift-drift transition in the basin. The pre-, syn- and post-glacial
carbonate systems could record a distally short-lived regional synrift freshwater-influenced
submarine fan derived from nearshore sediments, including gravity flow structures, which are
attributed to regional tectonic processes due to a sudden deepening of the basin caused by
differential tilting and uplifting of blocks, related to the 750-670 Ma oceanic spreading of the
central-southern Macaúbas Basin.
Combining sedimentology, isotopes and trace elemental geochemistry, the thesis highlights
that the δ13C variations in the Neoproterozoic carbonates are complex to interpret, and can be
related to: (i) the existence of a δ13C-depth gradient; (ii) the exchange between isotopically
light carbon in meteoric waters and carbonate during lithification and early diagenesis; and
(iii) isotopic perturbations due to regional metamorphism. Considering the possible englaciation of the Earth (Snowball Earth hypothesis), the Mbuji-Mayi Supergroup and West
Congolian Group seem reflected the intimate relationship between glaciations and tectonic
activity during the break-up of the Rodinia supercontinent, followed by the rift–drift
transition, and finally the pre-orogenic period on the passive continental margin.
Doctorat en Sciences
info:eu-repo/semantics/nonPublished
Friederichs, Yasmin Lima. „O sistema fluvio-estuarino da Baía de Sepetiba preservado na estratigrafia rasa da plataforma continental interna adjacente (RJ)“. Universidade do Estado do Rio de Janeiro, 2012. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=4307.
Der volle Inhalt der QuelleA análise de dados de reflexão sísmica monocanal boomer (Hz ~ 700-4,000; penetração ~ 70 ms) adquiridos na plataforma continental interna-média (até ~ 50-60 m de profundidade) ao largo do sistema estuarino baía de Sepetiba, no Estado do Rio de Janeiro, Brasil, revelou a ocorrência de uma sucessão sedimentar preservada 15-20 m, sismicamente interpretada como representando ambientes fluvio-estuarinos para marinhos rasos. Estas séries são sotopostas à inconformidade regional mais superior reconhecida na escala de plataforma, chamada superfície S3. Esta superfície é erodida por numerosas incisões fluviais, que sugerem processos erosivos associados à prolongada exposição subaérea da plataforma continental durante o estágio isotópico marinho 2 (MIS 2), globalmente datada em ~ 20 ka A.P.. A preservação de tais unidades de corte e preenchimento estuarinho presumíveis Pleistoceno Superior-Holoceno na plataforma interna-média (até ~ 30 km da costa) evidencia pela primeira vez na área a existência de um paleo sistema fluvial bastante desenvolvido e processos dominantes de denudação na bacia hidrográfica a montante que atualmente alimenta a baía de Sepetiba. Bem como que, uma série de elementos arquiteturais sísmicos dentro desta sucessão estuarina, como canais de maré retrogradantes, registram a evolução do paleo sistema estuarino de um sistema aberto à um sistema parcialmente protegido durante a transgressão Holocênica. A formação e erosão de uma sucessão de ilhas barreira isoladas e canais de maré durante a transgressão persistiu até o desenvolvimento de uma superfície estratigráfica superior na área, interpretada como a superfície de máxima inundação (MFS) no registro estratigráfico. A ilha barreira atual (restinga da Marambaia) prograda sobre a MFS como uma feição deposição regressiva, apontando para uma idade mais jovem do que cerca de ~ 5 ka A. P., idade da transgressão máxima na área, de acordo com a literatura disponível.
The analysis of boomer monochannel seismic reflection data (~700-4.000 Hz; ~70 ms penetration) acquired on the inner-mid shelf (up to ~50-60 m depth) offshore Sepetiba bay estuarine system, Rio de Janeiro State, Brazil, revealed the occurrence of a 15-20 m preserved sedimentary succession, seismically interpreted as representing fluvio-estuarine to shallow marine environments. These series overly the most upper regional unconformity recognized at shelf scale, named surface S3. This surface is eroded by numerous fluvial incisions, which suggest erosive processes associated to prolonged subaerial exposure of the continental shelf during marine isotopic stage 2 (MIS2), globally dated at ~20 ky B.P.. Preservation of such presumable Upper Pleistocene-Holocene cut-and-fill estuarine units on the inner-mid shelf (up to ~30km away from the coast) evidence for the first time in the area the existence of a rather developed paleo river system and dominant denudation processes in the upstream catchment basin that presently nourishes Sepetiba bay. As well as that, a series of seismic architectural elements within this estuarine succession, such as retrogressive tidal channels, record the evolution of the paleo estuarine system from an open to a partially-protected system during the Holocene transgression. The formation and erosion of a succession of isolated barrier islands and tidal channels during transgression persisted until the development of an upper stratigraphic surface in the area, interpreted as the maximum flooding surface (MFS) in the stratigraphic record. The present day barrier island (restinga da Marambaia) progrades over the MFS as a regressive depositional feature, pointing to an age younger than about ~5 ky B. P., dating of the maximum transgression in the area, according to the available literature.
WANG, SHI-WEI, und 王士偉. „Sedimentary environments of the Kangkaol limestone, and biometrical study of Lepidacyclina, coastal range of Taiwan“. Thesis, 1988. http://ndltd.ncl.edu.tw/handle/58079819987366838971.
Der volle Inhalt der QuelleChoh, Suk-Joo Fisher W. L. „Microfacies and depositional environments of selected Pennsylvanian calcareous algal deposits from southern U.S.A., and application of information technology for sedimentary petrology teaching and research“. 2004. http://repositories.lib.utexas.edu/bitstream/handle/2152/1905/chohss042.pdf.
Der volle Inhalt der QuelleBücher zum Thema "Coastal sedimentary depositional environments"
1937-, Davis Richard A., und Basan Paul B, Hrsg. Coastal sedimentary environments. 2. Aufl. New York: Springer Verlag, 1985.
Den vollen Inhalt der Quelle findenDavis, Richard A., Hrsg. Coastal Sedimentary Environments. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4.
Der volle Inhalt der Quelle1937-, Davis Richard A., Hrsg. Coastal sedimentary environments. 2. Aufl. NewYork: Springer Verlag, 1985.
Den vollen Inhalt der Quelle findenpétrole, Institut français du, Hrsg. Sedimentary geology: Sedimentary basins, depositional environments, petroleum formation. Paris: Editions Technip, 2002.
Den vollen Inhalt der Quelle findenBill, Carter, und International Sedimentological Congress, (13th : 1990 : Nottingham, England), Hrsg. Coastal sedimentary environments of southern England, South Wales and southeast Ireland. (Reading): British Sedimentological Research Group, 1991.
Den vollen Inhalt der Quelle findenDubiel, Russell F. Depositional environments of the Upper Triassic Chinle Formation in the eastern San Juan Basin and vicinity, New Mexico. Washington: U.S. G.P.O., 1989.
Den vollen Inhalt der Quelle findenMorton, Robert A. Middle-Upper Miocene depositional sequences of the Texas Coastal Plain and Continental Shelf: Geologic framework, sedimentary facies, and hydrocarbon plays. Austin, TX: University of Texas at Austin, 1988.
Den vollen Inhalt der Quelle findenMorton, Robert A. Middle-Upper Miocene depositional sequences of the Texas Coastal Plain and Continental Shelf: Geologic framework, sedimentary facies, and hydrocarbon plays. Austin, Tex: Bureau of Economic Geology, University of Texas at Austin, 1988.
Den vollen Inhalt der Quelle findenStanesco, John D. Sedimentology and depositional environments of the Lower Permian Yeso Formation, northwestern New Mexico: A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern. Denver, CO: U.S. Geological Survey, 1992.
Den vollen Inhalt der Quelle findenL, Ridgley Jennie, und Armstrong Augustus K, Hrsg. Depositional environments of the Upper Triassic Chinle Formation in the eastern San Juan Basin and vicinity, New Mexico: Evidence for a lacustrine origin / by Jennie L. Ridgley. Stratigraphy, facies, and paleotectonic history of Mississippian rocks in the San Juan Basin of northwestern New Mexico and adjacent areas / by Augustus K. Armstrong and Lee D. Holcomb. Washington: U.S. G.P.O., 1989.
Den vollen Inhalt der Quelle findenBuchteile zum Thema "Coastal sedimentary depositional environments"
Bao-can, Wang, und D. Eisma. „Mudflat Deposition along the Wenzhou Coastal Plain in Southern Zhejiang, China“. In Tide-Influenced Sedimentary Environments and Facies, 265–74. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-015-7762-5_19.
Der volle Inhalt der QuelleHahn, Annette, Enno Schefuß, Nicole Burdanowitz, Hayley C. Cawthra, Jemma Finch, Tarryn Frankland, Andrew Green, Frank H. Neumann und Matthias Zabel. „Catchment and Depositional Studies for the Reconstruction of Past Environmental Change in Southern Africa“. In Sustainability of Southern African Ecosystems under Global Change, 815–43. Cham: Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-10948-5_28.
Der volle Inhalt der QuelleEinsele, Gerhard. „Special Depositional Environments and Sediments“. In Sedimentary Basins, 249–90. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_6.
Der volle Inhalt der QuelleEinsele, Gerhard. „Special Depositional Environments and Sediments“. In Sedimentary Basins, 233–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5_6.
Der volle Inhalt der QuelleGoldsmith, Victor. „Coastal Dunes“. In Coastal Sedimentary Environments, 303–78. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4_5.
Der volle Inhalt der QuelleDiessel, Claus F. K. „Coal-Producing Sedimentary Environments“. In Coal-Bearing Depositional Systems, 349–459. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-75668-9_7.
Der volle Inhalt der QuelleFox, William T. „Modeling Coastal Environments“. In Coastal Sedimentary Environments, 665–705. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4_10.
Der volle Inhalt der QuelleEinsele, Gerhard. „Basin Classification and Depositional Environments (Overview)“. In Sedimentary Basins, 3–15. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_1.
Der volle Inhalt der QuelleEinsele, Gerhard. „Basin Classification and Depositional Environments (Overview)“. In Sedimentary Basins, 3–16. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5_1.
Der volle Inhalt der QuelleFrey, Robert W., und Paul B. Basan. „Coastal Salt Marshes“. In Coastal Sedimentary Environments, 225–301. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4_4.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Coastal sedimentary depositional environments"
Almalki, F., und S. Hayton. „Sedimentary facies and depositional environments of an Early Silurian sandstone“. In Seventh Arabian Plate Geology Workshop: Pre-Cambrian to Paleozoic Petroleum Systems in the Arabian Plate. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201900216.
Der volle Inhalt der QuelleChen, Eric, Cecilia McHugh, Jamie Asan, Frank Nitsche und Timothy C. Kenna. „COASTAL AND ESTUARINE SEDIMENTARY ENVIRONMENTS OF EASTERN LONG ISLAND SOUND“. In Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-374499.
Der volle Inhalt der QuelleImmenhauser, A. „The Albian Sedimentary Record of Southeast Arabia - Facies, Sequence Stratigraphy and Depositional Environments“. In Second Arabian Plate Geology Workshop 2010. Netherlands: EAGE Publications BV, 2010. http://dx.doi.org/10.3997/2214-4609.20145630.
Der volle Inhalt der QuelleHasiotis, S. T., J. G. McPherson und M. R. W. Reilly. „Using Ichnofossils to Reconstruct the Depositional History of Sedimentary Successions in Alluvial, Coastal Plain, and Deltaic Settings“. In International Petroleum Technology Conference. International Petroleum Technology Conference, 2013. http://dx.doi.org/10.2523/17016-ms.
Der volle Inhalt der QuelleHasiotis, S. T., J. G. McPherson und M. R. W. Reilly. „Using Ichnofossils to Reconstruct the Depositional History of Sedimentary Successions in Alluvial, Coastal Plain, and Deltaic Settings“. In International Petroleum Technology Conference. International Petroleum Technology Conference, 2013. http://dx.doi.org/10.2523/iptc-17016-ms.
Der volle Inhalt der QuelleFarkas, Juraj, Alan Collins, Stefan Löhr, Charles Verdel, Morgan Blades, Chris Holmden, Susanne Schmid, Darwinaji Subarkah, Robert Klaebe und Shaun Yardley. „New metal isotope techniques to explore past depositional environments of the Centralian Superbasin, Australia“. In Central Australian Basins Symposium IV. Petroleum Exploration Society of Australia (PESA), 2022. http://dx.doi.org/10.36404/fiwq4275.
Der volle Inhalt der QuelleWainman, Carmine C., und Peter J. McCabe. „Understanding the interplay between basin architecture, depositional environments and sediment pathways in the Cooper Basin“. In Central Australian Basins Symposium IV. Petroleum Exploration Society of Australia (PESA), 2022. http://dx.doi.org/10.36404/fyfq6280.
Der volle Inhalt der QuelleFechet, Roxana Magdalena. „SEDIMENTARY ROCKS, DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHIC IN BURDIGALIAN AND BADENIAN DEPOSITS OF SLANIC PRAHOVA � ALUNIS (ROMANIA)“. In SGEM2011 11th International Multidisciplinary Scientific GeoConference and EXPO. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2011/s01.134.
Der volle Inhalt der QuelleZavarzina, G. A., D. S. Shapabaeva und O. A. Zakharova. „A Study Into the Depositional Environments of East Arctic Sedimentary Basins Aimed at Evaluating their Hydrocarbon Potential“. In Geomodel 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201950105.
Der volle Inhalt der QuelleBeiranvand, Bijan, Ebrahim Ghasemi Nejad, Abdol Hossein Amini und Mohammad reza Kamali. „Sea Level Changes and Depositional Environments of the Late Cretaceous to Paleocene Sedimentary Succession, Izeh, Zagros Basin, Iran“. In GEO 2010. European Association of Geoscientists & Engineers, 2010. http://dx.doi.org/10.3997/2214-4609-pdb.248.392.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Coastal sedimentary depositional environments"
Keen, Timothy R., und K. T. Holland. The Coastal Dynamics of Heterogeneous Sedimentary Environments: Numerical Modeling of Hydrodynamics and Mass Transport in Estuaries. Fort Belvoir, VA: Defense Technical Information Center, August 2010. http://dx.doi.org/10.21236/ada528744.
Der volle Inhalt der QuelleD'Spain, Gerald, und Scott Jenkins. Hydrodynamic Design of a Dead Weight Anchor Device Optimized for Station Keeping and Suppression of Subsequent Burial on Sedimentary Beds in Coastal Environments. Fort Belvoir, VA: Defense Technical Information Center, März 2009. http://dx.doi.org/10.21236/ada496176.
Der volle Inhalt der QuelleLimoges, A., A. Normandeau, J. B R Eamer, N. Van Nieuwenhove, M. Atkinson, H. Sharpe, T. Audet et al. 2022William-Kennedy expedition: Nunatsiavut Coastal Interaction Project (NCIP). Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332085.
Der volle Inhalt der QuelleKabanov, P. Devonian of the Mackenzie. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/326094.
Der volle Inhalt der QuelleClark, Donald L., Stefan M. Kirby und Charles G. Oviatt. Geologic Map of the Rush Valley 30' X 60' Quadrangle, Tooele, Utah, and Salt Lake Counties, Utah. Utah Geological Survey, August 2023. http://dx.doi.org/10.34191/m-294dm.
Der volle Inhalt der QuelleTran, Tut, Alexandra Bonham, Justin Tweet und Vincent Santucci. Bryce Canyon National Park: Paleontological resource inventory. National Park Service, 2024. http://dx.doi.org/10.36967/2302804.
Der volle Inhalt der QuelleTran, Tut, Alexandra Bonham, Justin Tweet und Vincent Santucci. Bryce Canyon National Park: Paleontological resource inventory (public version). National Park Service, 2024. http://dx.doi.org/10.36967/2303710.
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