Academic literature on the topic 'Coastal sedimentary depositional environments'

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Journal articles on the topic "Coastal sedimentary depositional environments"

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Li, Haonan, Guangxue Li, Jian Zhang, et al. "Evolution of Stratigraphic Sequence and Sedimentary Environment in Northern Yellow River Delta Since MIS5." Journal of Marine Science and Engineering 13, no. 5 (2025): 832. https://doi.org/10.3390/jmse13050832.

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Quaternary climate has been characterized by pronounced glacial–interglacial cycles, with eustatic sea-level fluctuations directly controlling coastal sedimentary environments. The Yellow River Delta, situated on the southwestern coast of Bohai Bay, bears a distinct stratigraphic imprint of marine–terrestrial environmental transitions. However, critical knowledge gaps persist in reconstructing an integrated continental–marine stratigraphic framework. This study focuses on the nearshore core CB2302, integrating sediment lithology, grain size, foraminiferal assemblages, and geochemical proxies t
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Stoupakova, Antonina V., Nataliya I. Korobova, Alina V. Mordasova, et al. "Depositional environments as a framework for genetic classification of the basic criteria of petroleum potential." Georesursy 25, no. 2 (2023): 75–88. http://dx.doi.org/10.18599/grs.2023.2.6.

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Most classifications of reservoirs, seals and source rocks based on the ability of the rock to generate, accumulate and preserve hydrocarbons, and the genesis of rocks is not always taken into account. The article presents a ranking scheme for continental, coastal-marine and marine sedimentation environments that determine the genesis and properties of the basic criteria of petroleum potential – source rocks, reservoirs, seals and pinch-out traps. Rocks, which can consider as source rock, reservoirs and seals are formed in each depositional environment. However, their structure, mineral compos
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Safaei, Mohammad, Asadollah Mahboubi, Soroush Modabberi, and 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, no. 1 (2020): 61–89. http://dx.doi.org/10.1127/njgpa/2020/0868.

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Four Lower Cretaceous sections in the southern Yazd Block were measured and studied to interpret the palaeoenvironments, synsedimentary tectonics, and sequence stratigraphy. The Early Cretaceous sedimentary record of this block, consisting of the Sangestan, Taft, Abkuh, and Darreh Zanjir formations, was mainly influenced by synsedimentary tectonic activities in a tectonically unstable basin. Field observations and laboratory studies were used to identify lithofacies and microfacies, based on which six depositional environments were identified: upper coastal plain (alluvial fans), shore, tidal
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Nayak, Ganapati Narayan. "Changing Tropical Estuarine Sedimentary Environments with Time and Metals Contamination, Cest Coast of India." Journal of The Indian Association of Sedimentologists 38, no. 2 (2021): 63–78. http://dx.doi.org/10.51710/jias.v38i2.141.

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Estuaries are one of the major sub-environments of the coastal zone wherein freshwaters interact and mix with saline waters, and facilitate deposition of finer sediments, organic matter, and metals. Intertidal mudflat and mangrove sediment cores collected from estuaries along the central west coast of India were investigated for various sedimentological and geochemical parameters to understand the changes in the sedimentary depositional environments and various factors influencing the processes. Additionally, estuarine biota was examined to understand the bioaccumulation of metals with respect
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Owens, R., A. Kelman, K. Khider, T. Bernecker, and B. Bradshaw. "Late Permian–Early Triassic depositional history in the southern Bonaparte Basin: new biostratigraphic insights into reservoir heterogeneity." APPEA Journal 61, no. 2 (2021): 699. http://dx.doi.org/10.1071/aj20111.

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The upper Permian to Lower Triassic sedimentary succession in the southern Bonaparte Basin represents a marginal marine depositional system that hosts several gas accumulations. Of these, the Blacktip gas field has been in production since 2009, while additional gas resources are under consideration for development. The sedimentary succession extends across the Permian–Triassic stratigraphic boundary, and shows a change in lithofacies from the carbonate dominated Dombey Formation to the siliciclastic dominated Tern and Penguin formations. The timing, duration, distribution and depositional env
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Khabidov, A. Sh, L. A. Zhindarev, E. A. Fedorova, and K. V. Marusin. "COASTAL ZONE OF LARGE MAN-MADE LAKES (Paper 2. DEPOSITIONAL SEDIMENTARY ENVIRONMENTS)." Geomorphology RAS, no. 3 (March 18, 2015): 23. http://dx.doi.org/10.15356/0435-4281-2014-3-23-29.

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Alshammari, Bassam, Nigel P. Mountney, Luca Colombera, and 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, no. 7 (2021): 773–94. http://dx.doi.org/10.2110/jsr.2020.077.

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ABSTRACT The interaction of fluvial, tidal, and wave processes in coastal and paralic environments gives rise to sedimentary successions with highly varied styles of facies architecture; these are determined by the morphology and evolutionary behavior of the range of coastal sub-environments, which may be difficult to diagnose in subsurface sedimentary successions with limited well control. This study presents depositional models to account for stratigraphic complexity in a subsurface fluvial to shallow-marine succession, the Middle Jurassic Dhruma Formation, Saudi Arabia. The study achieves t
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Ezeh, Sunny C., Wilfred A. Mode, Berti M. Ozumba, and Nura A. Yelwa. "Sedimentology and ichnology of Neogene Coastal Swamp deposits in the Niger Delta Basin, Nigeria." Geologos 22, no. 3 (2016): 191–200. http://dx.doi.org/10.1515/logos-2016-0020.

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Abstract Often analyses of depositional environments from sparse data result in poor interpretation, especially in multipartite depositional settings such as the Niger Delta. For instance, differentiating channel sandstones, heteroliths and mudstones within proximal environments from those of distal facies is difficult if interpretations rely solely on well log signatures. Therefore, in order to achieve an effective and efficient interpretation of the depositional conditions of a given unit, integrated tools must be applied such as matching core descriptions with wireline log signature. In the
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Cheng, Wufeng, Shenliang Chen, Xiaojing Zhong, and 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, no. 15 (2023): 2680. http://dx.doi.org/10.3390/w15152680.

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Particle morphology is an important feature of sediments that reflects their transport history and depositional environment. In this study, we used dynamic image analysis (DIA) to measure the size and shape of beach sediments on the east and west coasts of Hainan Island in South China Sea. DIA is a fast and accurate method that can capture and analyze a large number of sediment particles in real-time. We extracted morphological descriptors of each particle, such as equivalent diameter, sphericity, aspect ratio and symmetry, and their distributions based on volume and number. We performed multi
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Bellais, Kaylyn C., Samuel T. Barber, Donald A. Beebe, and Murlene W. Clark. "Lake or Estuary? Sedimentary and Benthic Foraminiferal Characterization of a Gulf of Mexico Coastal Dune Lake." Gulf and Caribbean Research 31 (2020): SC46—SC52. http://dx.doi.org/10.18785/gcr.3101.18.

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Coastal dune lakes are shallow estuaries located within dune environments that share a permanent or intermittent connection with the sea. Because coastal dune lakes are found in few locations worldwide (e.g. Australia, New Zealand, Florida, etc.) they represent unique environments worthy of protection. However; there is a distinct lack of scientific data related to the function and ecology of coastal dune lakes, especially in the Gulf of Mexico. Therefore, the purpose of this study was to characterize the sedimentology and foraminifera of a representative coastal dune lake in Walton County, FL
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Dissertations / Theses on the topic "Coastal sedimentary depositional environments"

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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.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, and Woods Hole Oceanographic Institution, 1990.<br>Vita.<br>Includes bibliographical references. Includes bibliographical references.<br>by Mark A. McCaffrey.<br>Ph.D.
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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.

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Raine, 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.

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Fryer, 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.

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<p> Submarine-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).
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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.

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La modélisation du sous-sol est un moyen de prédire la structure et la connectivité des unités stratigraphiques en honorant les observations de subsurface. Ces observations sont en général échantillonées le long de puits à grande échelle horizontale (kilomètre) mais à petite échelle verticale (mètre). Il y a deux types de données de puits : (1) les diagraphies, qui correspondent à des acquisitions géophysiques quasi-continus (échatillonage régulier) le long du puits (e.g., gamma ray, sonic, porosité neutron), et (2) les régions, qui correspondent à des propriétés réservoir discrètes définies p
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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.

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Delpomdor, 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.

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The one of the most important Eras of the Earth history, i.e. Neoproterozoic (1000-542 Ma),<p>was an enigmatic period characterized by the development of the first stable long-lived ~1.1-<p>0.9 Ga Rodinia and 550-500 Ma Gondwana supercontinents, global-scale orogenic belts,<p>extreme climatic changes (cf. Snowball Earth Hypothesis), the development of microbial<p>organisms facilitating the oxidizing atmosphere and explosion of eukaryotic forms toward the<p>first animals in the terminal Proterozoic. This thesis presents a multidisciplinary study of two<p>Neoproterozoic basins, i.e. Bas-Congo an
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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.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior<br>A 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 s
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WANG, SHI-WEI, and 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.

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Choh, 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.

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Books on the topic "Coastal sedimentary depositional environments"

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Davis, Richard A., ed. Coastal Sedimentary Environments. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4.

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1937-, Davis Richard A., ed. Coastal sedimentary environments. 2nd ed. Springer Verlag, 1985.

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1937-, Davis Richard A., and Basan Paul B, eds. Coastal sedimentary environments. 2nd ed. Springer Verlag, 1985.

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pétrole, Institut français du, ed. Sedimentary geology: Sedimentary basins, depositional environments, petroleum formation. Editions Technip, 2002.

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1940-, Curran H. Allen, and Society of Economic Paleontologists and Mineralogists., eds. Biogenic structures: Their use in interpreting depositional environments. Society of Economic Paleontologists and Mineralogists, 1985.

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Bill, Carter, and International Sedimentological Congress, (13th : 1990 : Nottingham, England), eds. Coastal sedimentary environments of southern England, South Wales and southeast Ireland. British Sedimentological Research Group, 1991.

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Dale, Nations, Eaton Jeffrey G. 1948-, and Geological Society of America. Meeting, eds. Stratigraphy, depositional environments, and sedimentary tectonics of the western margin, Cretaceous Western Interior Seaway. Geological Society of America, 1991.

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Dubiel, Russell F. Depositional environments of the Upper Triassic Chinle Formation in the eastern San Juan Basin and vicinity, New Mexico. U.S. G.P.O., 1989.

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Morton, Robert A. Middle-Upper Miocene depositional sequences of the Texas Coastal Plain and Continental Shelf: Geologic framework, sedimentary facies, and hydrocarbon plays. University of Texas at Austin, 1988.

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Morton, Robert A. Middle-Upper Miocene depositional sequences of the Texas Coastal Plain and Continental Shelf: Geologic framework, sedimentary facies, and hydrocarbon plays. Bureau of Economic Geology, University of Texas at Austin, 1988.

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Book chapters on the topic "Coastal sedimentary depositional environments"

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Bao-can, Wang, and D. Eisma. "Mudflat Deposition along the Wenzhou Coastal Plain in Southern Zhejiang, China." In Tide-Influenced Sedimentary Environments and Facies. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-015-7762-5_19.

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Hahn, Annette, Enno Schefuß, Nicole Burdanowitz, et al. "Catchment and Depositional Studies for the Reconstruction of Past Environmental Change in Southern Africa." In Sustainability of Southern African Ecosystems under Global Change. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-10948-5_28.

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AbstractTerrestrial signals in marine sedimentary archives are often used for reconstructing past environments, vegetation and climate, as well as for determining sediment fluxes, pathways, and depositional sites and changes in erosional runoff. It is therefore important to understand the origin, transport, and depositional processes of the various terrestrial sedimentary components in a depositional system. In this chapter, we use examples from southern Africa to show how source-to-sink studies have led to a clearer interpretation of downcore proxy records. Twelve rivers in four river catchme
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Einsele, Gerhard. "Special Depositional Environments and Sediments." In Sedimentary Basins. Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_6.

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Einsele, Gerhard. "Special Depositional Environments and Sediments." In Sedimentary Basins. Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5_6.

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Goldsmith, Victor. "Coastal Dunes." In Coastal Sedimentary Environments. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4_5.

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Diessel, Claus F. K. "Coal-Producing Sedimentary Environments." In Coal-Bearing Depositional Systems. Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-75668-9_7.

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Fox, William T. "Modeling Coastal Environments." In Coastal Sedimentary Environments. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4_10.

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Einsele, Gerhard. "Basin Classification and Depositional Environments (Overview)." In Sedimentary Basins. Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_1.

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Einsele, Gerhard. "Basin Classification and Depositional Environments (Overview)." In Sedimentary Basins. Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5_1.

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Frey, Robert W., and Paul B. Basan. "Coastal Salt Marshes." In Coastal Sedimentary Environments. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5078-4_4.

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Conference papers on the topic "Coastal sedimentary depositional environments"

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Livanov, Oliver, Alexandru Banescu, Adrian Burada, Paula Pindic, and Ciprian Anore. "THE PARTICLE SIZE OF THE BOTTOM SEDIMENTS IN SOME CANALS OF THE FLUVIAL-MARINE DANUBE DELTA." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s01.17.

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In deltaic environments like the Danube Delta, sedimentary particles can range from clay and silt to sand and gravel. The proximity to the Black Sea introduces marine processes into the deltaic system that can be translated as a mixture of fine-grained sediments derived from the fluvial delta along with marine sediments from the Black Sea. This region is of particular importance for the ecology and hydrology of the Danube Delta due to the presence of sandy deposits that cause a major change in both natural and anthropogenic habitats. The emergence of artificial canals dug in sandy deposits had
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Nanda, Jagannath, Sourav Bhardwaj, G. Purushotham, Pratik Kumar, Udham Singh Yadav, and U. Chukkasseri. "Characterization of Gas Hydrate Deposits in Probable Sandy Facies and Its Related Depositional Processes, East Coast Deep Water Basin, India." In Offshore Technology Conference. OTC, 2025. https://doi.org/10.4043/35997-ms.

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Abstract Gas Hydrates represent vast energy resources and are considered to be a potential clean fuel of the future. Under the National Gas Hydrate Program (NGHP), DGH and ONGC have been carrying out research work for exploration and development of the gas hydrates in Indian Offshore. Based on the geological, geophysical and geochemical studies, coring/drilling/logging which were carried out during NGHP-01, 2006 and NGHP-02, 2015, several gas hydrate prospective areas have been identified in Krishna-Godavari (KG) and Mahanadi (MN) deep offshore. During the year 2016-17, the studies have been c
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Almalki, F., and 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. EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201900216.

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Chen, Eric, Cecilia McHugh, Jamie Asan, Frank Nitsche, and 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.

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Immenhauser, A. "The Albian Sedimentary Record of Southeast Arabia - Facies, Sequence Stratigraphy and Depositional Environments." In Second Arabian Plate Geology Workshop 2010. EAGE Publications BV, 2010. http://dx.doi.org/10.3997/2214-4609.20145630.

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Hasiotis, S. T., J. G. McPherson, and 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.

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Hasiotis, S. T., J. G. McPherson, and 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.

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Farkas, Juraj, Alan Collins, Stefan Löhr, et al. "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.

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The Centralian Superbasin (CSB) is a ~ 2 million km2 Neoproterozoic to early Palaeozoic (ca. 850−400 Ma) intracratonic depositional system, which stretches across four states (WA, NT, SA and QLD) and is of fundamental scientific and economic significance to Australia. Sedimentary sequences within the CSB, comprising the Amadeus/Warburton, Georgina and Officer Basins, record a critical phase of Earth history, encompassing the Neoproterozoic rise of atmospheric oxygen, major reorganisations in the global carbon cycle and the emergence of the first complex life.
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Wainman, Carmine C., and 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.

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The late Carboniferous to Middle Triassic Cooper Basin is Australia’s premier onshore petroleum province hosting a range of conventional and unconventional resources (Hall et al., 2019). Despite being considered a mature petroleum basin with over 1900 wells drilled and over 104,000 km of seismic surveys shot (Resources, 2022), many aspects of the Cooper Basin remain enigmatic with very different structural and sedimentary histories between the eight troughs and intervening ridges (Kulikowski et al., 2022).
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Fechet, 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.

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Reports on the topic "Coastal sedimentary depositional environments"

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Keen, Timothy R., and K. T. Holland. The Coastal Dynamics of Heterogeneous Sedimentary Environments: Numerical Modeling of Hydrodynamics and Mass Transport in Estuaries. Defense Technical Information Center, 2010. http://dx.doi.org/10.21236/ada528744.

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D'Spain, Gerald, and 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. Defense Technical Information Center, 2009. http://dx.doi.org/10.21236/ada496176.

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Limoges, A., A. Normandeau, J. B R Eamer, et al. 2022William-Kennedy expedition: Nunatsiavut Coastal Interaction Project (NCIP). Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332085.

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The accelerating Arctic cryosphere decline severely impacts the land on which northern communities live through the presence of coastal and marine geohazards and coastal erosion, which further places the cultural heritage of coastal archaeological sites at risks. Sea ice decline also compromises the formation of polynyas, with unknown consequences for the regional ecosystems. From the 10th to the 18th of July 2022, a scientific cruise onboard the research vessel William-Kennedy allowed the collection of a suite of samples and data from the marine coastal environment of Nain, Nunatsiavut. In to
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Kabanov, P. Devonian of the Mackenzie. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/326094.

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This paper reviews the Devonian-Lower Mississippian strata of NTS areas 106 and 96 lying within Geo-mapping for Energy and Minerals (GEM) Mackenzie project area and its vicinity. These strata are usually well in excess of 1 km in non-eroded sections, cropping out extensively in the Cordillera and occurring in the subsurface of adjacent Interior Plains. Major tectonostratigraphic assemblages are the latest Silurian-Eifelian platform carbonates and evaporites, the latest Eifelian-Frasnian basinal mudrocks with isolated carbonate banks bundled in the Horn River Group (HRG), and the thick coarseni
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Clark, Donald L., Stefan M. Kirby, and Charles G. Oviatt. Geologic Map of the Rush Valley 30' X 60' Quadrangle, Tooele, Utah, and Salt Lake Counties, Utah. Utah Geological Survey, 2023. http://dx.doi.org/10.34191/m-294dm.

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The Rush Valley 30' x 60' quadrangle extends southwest and west from the greater Salt Lake City–Provo metropolitan area with land use varied between public, military, Indian reservation, and private. This 1:62,500-scale geologic map will aid the proper management of land, water, and other resources. The map area lies within the eastern Basin and Range Province. Mountain ranges are composed of unexposed basement rocks overlain by exposed Neoproterozoic through Triassic rocks that are about 10.4 miles (16.8 km) thick, and by numerous Tertiary sedimentary and volcanic units (~47 to 20 Ma). The in
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Shaffer, Austin, John-Paul Hodnett, Vincent Santucci, et al. Cuyahoga Valley National Park: Paleontological resource inventory (public version). National Park Service, 2024. http://dx.doi.org/10.36967/2306411.

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Cuyahoga Valley National Park (CUVA) was established as Cuyahoga River National Recreation Area on December 27, 1974, to preserve and protect the Cuyahoga River Valley and its historic, scenic, natural, and recreational values. While not explicitly mentioned in the park?s mission statement, paleontological resources preserved at CUVA are nevertheless of importance, particularly when considering the significant fossil discoveries made elsewhere across northeast Ohio. The upper Paleozoic geologic strata of CUVA encompass sedimentary rocks dating from the Late Devonian to the Early Pennsylvanian,
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Tran, Tut, Alexandra Bonham, Justin Tweet, and Vincent Santucci. Bryce Canyon National Park: Paleontological resource inventory. National Park Service, 2024. http://dx.doi.org/10.36967/2302804.

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Originally designated as a national monument in 1923, Bryce Canyon National Park (BRCA) is recognized for its exceptional pink-orange hoodoo landscapes. Its iconic hoodoos, consisting of the Paleocene?Eocene Claron Formation, are only part of the geology of BRCA, which includes a nearly uninterrupted sequence of Late Cretaceous Western Interior Seaway evolution and diverse depositional environments from approximately 100 to 77 million years ago. This sequence consists of the coastal Naturita Formation, the marine Tropic Shale, the transitional Straight Cliffs Formation, and the terrestrial Wah
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Tran, Tut, Alexandra Bonham, Justin Tweet, and 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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Originally designated as a national monument in 1923, Bryce Canyon National Park (BRCA) is recognized for its exceptional pink-orange hoodoo landscapes. Its iconic hoodoos, consisting of the Paleocene?Eocene Claron Formation, are only part of the geology of BRCA, which includes a nearly uninterrupted sequence of Late Cretaceous Western Interior Seaway evolution and diverse depositional environments from approximately 100 to 77 million years ago. This sequence consists of the coastal Naturita Formation, the marine Tropic Shale, the transitional Straight Cliffs Formation, and the terrestrial Wah
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