Academic literature on the topic 'Delta plain'

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Journal articles on the topic "Delta plain"

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Zeng, Zhiwei, Wei Wang, Hongtao Zhu, Xianghua Yang, and Dan Li. "The Facies Analysis, Evolution, and Coal-Bearing Source Rock Features of the Middle–Late Triassic Shallow-Water Delta in the North Carnarvon Basin, Northwest Shelf of Australia." Energies 16, no. 5 (2023): 2265. http://dx.doi.org/10.3390/en16052265.

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The sedimentary facies, architecture, and depositional mechanism of deltaic systems have been one of the global research hotspots in recent decades; however, the detailed distribution, sedimentary evolution, source rock potential, and major control factors of the coal-bearing shallow-water delta are still unclear. A typical shallow-water braided delta with coal-bearing source rocks developed in the Middle–Late Triassic Mungaroo Formation of the North Carnarvon Basin, which can be a good study area for an analysis of coal-bearing source rocks. In this study, the sedimentary facies, distribution
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UMITSU, Masatomo. "FLOOD AND TSUNAMI FLOW IN RELATION TO THE LANDFORMS OF COASTAL AND ALLUVIAL LOWLANDS-CASE STUDY IN HAT YAI AND BANDA ACEH PLAINS." Science and Technology Development Journal 12, no. 9 (2009): 68–77. http://dx.doi.org/10.32508/stdj.v12i9.2288.

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Flood control is a very important issue of the environmental management in the alluvial and coastal plains. For the detail management, it is necessary to know the behavior of the flooding on the plains. Micro landforms of these plains are closely related to the flow and inundation depth of floods. Landforms of an alluvial plain are roughly classified into three units. alluvial fan, floodplain and delta. Landforms of these units are further classified into micro landforms as natural levee, flood basin, paleo-river channel, beach ridges and so on. The places on a higher micro landforms are gener
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Gürbüz, Kemal. "An example of river course changes on a delta plain: Seyhan Delta (Çukurova plain, southern Turkey)." Geological Journal 34, no. 1-2 (1999): 211–22. http://dx.doi.org/10.1002/(sici)1099-1034(199901/06)34:1/2<211::aid-gj822>3.0.co;2-0.

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Alizai, Anwar, Stephen Hillier, Peter D. Clift, et al. "Clay mineral variations in Holocene terrestrial sediments from the Indus Basin." Quaternary Research 77, no. 3 (2012): 368–81. http://dx.doi.org/10.1016/j.yqres.2012.01.008.

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We employed X-ray diffraction methods to quantify clay mineral assemblages in the Indus Delta and flood plains since ~ 14 ka, spanning a period of strong climatic change. Assemblages are dominated by smectite and illite, with minor chlorite and kaolinite. Delta sediments integrate clays from across the basin and show increasing smectite input between 13 and 7.5 ka, indicating stronger chemical weathering as the summer monsoon intensified. Changes in clay mineralogy postdate changes in climate by 5–3 ka, reflecting the time needed for new clay minerals to form and be transported to the delta. S
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Melehan, Sean, Chrysanthos Botziolis, Angelos G. Maravelis, et al. "Sedimentology and Stratigraphy of an Upper Permian Sedimentary Succession: Northern Sydney Basin, Southeastern Australia." Geosciences 11, no. 7 (2021): 273. http://dx.doi.org/10.3390/geosciences11070273.

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This study integrates sedimentological and stratigraphic insights into the Upper Permian sedimentary rocks of the Wittingham, Tomago and Newcastle Coal Measures in the Northern Sydney Basin, Australia. Facies analysis documented fifteen facies that belong to seven facies associations. These facies associations correspond to different depositional environments and sub-environments including prodelta, delta-front, upper, lower delta-plain and fluvial. The stratigraphic development points to a shallowing upward trend and is reflected with fluvial deposits sitting on top of the deltaic deposits. T
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Dola, Shahpara Sheikh, Khairul Bahsar, Mazeda Islam, and Md Mizanur Rahman Sarker. "Hydrogeological Classification and the Correlation of Groundwater Chemistry with Basin Flow in the South-Western Part of Bangladesh." Journal of Bangladesh Academy of Sciences 42, no. 1 (2018): 41–54. http://dx.doi.org/10.3329/jbas.v42i1.37831.

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Attempt has been made to find the relationship between the basin groundwater flow and the current water chemistry of south-western part of Bangladesh considering their lithological distribution and aquifer condition. The correlation of water chemistry and basin groundwater flow is depicted in the conceptual model. The water-types of shallow groundwater are predominantly Mg-Na-HCO3 and Ca- Mg-Na-HCO3 type. In the deep aquifer of upper delta plain is predominately Na-Cl, Ca-HCO3 and Mg- HCO3 type. In the lower delta plain Na-Cl type of water mainly occurs in the shallow aquifer and occasionally
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Kirschbaum, Mark A. "Depostional [sic] Environments of the Rock Springs Formation, Southwest Flank of the Rock Springs Uplift, Wyoming." Mountain Geologist 23, no. 2 (1986): 63–75. http://dx.doi.org/10.31582/rmag.mg.23.2.63.

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A record at an ancient delta system Is preserved in outcrops along the flanks of the Rock Springs Uplift, southwestern Wyoming. The deltaic Upper Cretaceous Rock Springs Formation of the Mesaverde Group was deposited during early Campanian time near the end of the regressive phase of the Niobrara cyclothem. On the southwest end of the Uplift, part of the delta system is exposed near the seaward edge of a series of transgressive/regressive sequences, which consist of intertonguing prodelta, delta-front, and delta-plain deposits. Eight major delta-front sandstones are vertically stacked and late
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Dewan, P. K. "Godavari Delta System - A Wave-Dominated Delta System as Interpreted from Seismic Data has Hydrocarbon Potential." Journal Geological Society of India 33, no. 2 (1989): 189–93. http://dx.doi.org/10.17491/jgsi/1989/330210.

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Abstract Modern deltas can be classified mainly into three types: fluvial dominated, wave dominated and tide-dominated delta. Geometry of shoreline and palaeoshore line, dominance of strand-plain environment and other geomorphological and sedimentological features indicate the present Godavari delta to be wave dominated delta system. Seismic reflection patterns are predominantly parallel to subparallel, indicative of delta plain environments. Progradational shingled and oblique (parallel) reflection configuration is observed in different seismic sequences. Stratigraphic hydrocarbon reservoirs
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Klausen, Tore Grane, Björn Nyberg, and William Helland-Hansen. "The largest delta plain in Earth’s history." Geology 47, no. 5 (2019): 470–74. http://dx.doi.org/10.1130/g45507.1.

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Gaki-Papanastassiou, K., E. Karymbalis, and H. Maroukian. "RECENT GEOMORPHIC CHANGES AND ANTHROPOGENIC ACTIVITIES IN THE DELTAIC PLAIN OF PINIOS RIVER IN CENTRAL GREECE." Bulletin of the Geological Society of Greece 43, no. 1 (2017): 409. http://dx.doi.org/10.12681/bgsg.11192.

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The Pinios river delta is a Late Holocene arcuate type delta, located in the southern Thermaikos gulf (Central Greece). In order to determine the processes which contributed in the recent configuration of the delta, a detailed geomorphic map at the scale of 1:5000 has been prepared showing both the deltaic plain and the coastal zone features using GIS techniques. Comparative examinations of aerial photographs taken in different dates and reliable maps of the last two centuries along with field observations depict recent changes of the delta morphology. The most important factors for the develo
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Dissertations / Theses on the topic "Delta plain"

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Boyes, Donald M. "Morphometry, spatial analysis and development of lakes on the Mackenzie Delta plain." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0014/NQ40245.pdf.

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Schlegel, Melissa Eileen. "Evaluation of Paleo-climate for the Boise Area, Idaho, from the last Glacial Maximum to the Present Based on delta 2H and delta 18O Groundwater Composition." BYU ScholarsArchive, 2005. https://scholarsarchive.byu.edu/etd/317.

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There are four distinguishable groundwater systems in the Boise area, Idaho, U.S.A., identified as modern batholith, thermal batholith, Boise frontal fault, and Nampa-Caldwell systems (Figure 1). Modern batholith and thermal batholith groundwaters are located in Tertiary to Cretaceous aged granites and granodiorites of the Atlanta lobe of the Idaho Batholith. The frontal fault system near Boise, ID defines the southeastern edge of the Idaho Batholith, and divides the batholith from the western Snake River Plain. The Nampa-Caldwell system is in the volcanic, fluvial and pluvial sediments of the
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Torres, Julie A. "Geomorphic and temporal evolution of a Mississippi delta flanking barrier island: Grand Isle, LA." ScholarWorks@UNO, 2019. https://scholarworks.uno.edu/td/2649.

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Optically stimulated luminescence (OSL) dating beach ridge sediments is one method for resolving barrier island growth at intermediate scales (decades-centuries), information that is lacking for Louisiana. This research combines OSL, GPR, aerial imagery, and cores to document temporal and spatial evolution of a Louisiana barrier island. Grand Isle is composed of beach ridges organized in distinct, unconformable sets that began forming 0.75 ka until 0.575 ka when deposition ceased, the ridges were partially eroded, and deposition resumed in a more eastward direction. The central ridges formed b
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Blockland, Joseph D. "The Surficial Geology of Fulton County, Ohio: Insight into the Late Pleistocene-Early Holocene Glaciated Landscape of the Huron-Erie Lake Plain, Fulton County Ohio, USA." University of Toledo / OhioLINK, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=toledo1376315550.

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Neidhardt, Harald [Verfasser], and S. [Akademischer Betreuer] Norra. "Impact of groundwater abstraction and of the organic matter on release and distribution of arsenic in aquifers of the Bengal Delta Plain, India / Harald Neidhardt. Betreuer: S. Norra." Karlsruhe : KIT-Bibliothek, 2012. http://d-nb.info/1024312836/34.

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Boudreaux, Lon Jr. "The Mississippi River Delta Basin and Why We are Failing to Save its Wetlands." ScholarWorks@UNO, 2007. http://scholarworks.uno.edu/td/564.

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Every thousand years or so, when the Mississippi River's sediment load lengthened and blocked the River’s route to the Gulf of Mexico, the mother stream changed course completely, finding a shorter route to the sea. Then, it built a new delta, thus spreading the gift of land creation along a wide coastline and creating the bayou region of Louisiana. However, this ancient, natural process was gradually halted by the arrival of man who settled across the River's natural floodplain (delta) and constructed levees and other structures to control the great Mississippi River. Since the 1930s, the M
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Torres-Rondon, Laura. "Etude et modélisation des transferts d'eau et de sel en milieu deltaïque agricole (Camargue-France)." Thesis, Avignon, 2013. http://www.theses.fr/2013AVIG0048/document.

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L’objectif premier de ce travail est l’étude puis la modélisation numérique 3D du fonctionnement hydrogéologique et salin actuel d’une partie de l’aquifère superficiel de la Moyenne Camargue afin de l’utiliser, dans un second temps, pour la prévision qualitative des modifications induites par le changement climatique. La caractérisation de l’aquifère a été mené selon deux approches : une étude structurale, en utilisant des sondages à la tarière et différentes techniques géophysiques (ERT, ES et cartographie EM), et une étude hydrogéologique, intégrée par plusieurs campagnes de pompages, suivi
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Kawashima, Higa Luis Miguel, Vicente Gisella Milagros Maldonado, Martínez César Alejandro Ramos, Castellanos Juan Enrique Sánchez, and Espinoza Ingrid Andrea Venegas. "Plan estratégico 2019-2022 Delta/Signal." Master's thesis, Universidad del Pacífico, 2019. http://hdl.handle.net/11354/2518.

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La presente investigación contiene el Plan Estratégico 2019-2022 para Delta/Signal Corp., que es una empresa fabricante de autopartes eléctricas fundada en Ohio, Estados Unidos, en 1992. Teniendo en cuenta los drásticos cambios que ha sufrido la economía y la política a nivel mundial, la empresa tuvo que realizar cambios en su estrategia a partir del 2014. El objetivo principal de la presente investigación es recomendar el cambio a una nueva estrategia que permitirá el crecimiento y posicionamiento de la empresa. Por esta razón, la dirección de la empresa tomó la decisión de diseñar un nuevo p
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Álvarez, Guillén Joana Patricia, Julián Glen Álvaro Galindo, Carbonel Jorge Antonio Mostajo, Sotil Rocío Pilar Pacheco, and Chumpitaz José Gabriel Zamudio. "Plan estratégico para Delta Signal 2019-2022." Master's thesis, Universidad del Pacífico, 2019. http://hdl.handle.net/11354/2516.

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El presente trabajo propone el plan estratégico para el período 2019–2022 que permita a Delta Signal afrontar los cambios del sector, recuperar el crecimiento en ventas y asegurar la continuidad de la empresa. En el segundo capítulo, se realiza la evaluación externa e interna de la empresa para encontrar las oportunidades, amenazas, fortalezas, debilidades y otros factores sobre los cuales se definirá la estrategia de la compañía. Como parte de esta evaluación externa, se realiza el análisis del macroentorno, donde se evalúan los aspectos políticos, económicos, sociales, tecnológicos y legales
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Chire, Sarayasi Lino Antonio, Alzate Beatriz Elena Gil, Romero Ángela Zaida Paredes, Siccha Carmen Flor Salinas, and Montesinos Henry Sánchez. "Plan estratégico Delta / Signal Corp. 2019-2022." Master's thesis, Universidad del Pacífico, 2019. http://hdl.handle.net/11354/2477.

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A nivel global, la importancia de la industria automotriz en la economía mundial por su papel como propulsor para el desarrollo de otros sectores de alto valor agregado, ha provocado que tenga como uno de sus principales objetivos el desarrollo y/o fortalecimiento de esta industria. Delta / Signal Corp. es una empresa constituida en 1992 en Ohio, dedicada a la fabricación y distribución de autopartes eléctricas y electrónicas para sus clientes, fabricantes de equipos originales (OEM, por las siglas en inglés de original equipment manufacturer).
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Books on the topic "Delta plain"

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Paul, Ashis Kr. Coastal geomorphology and environment: Sundarban coastal plain, Kanthi coastal plain, Subarnarekha delta plain. ACB Publications, 2002.

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United States. Soil Conservation Service. Flood plain management study: Delta Junction, Alaska. The Service], 1987.

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Suter, John. Nearshore sand resources of the Mississippi River Delta plain--Marsh Island to Sandy Point. Louisiana Geological Survey, 1991.

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Shea, Penland, and Boyd Ron, eds. Transgressive depositional environments of the Mississippi river delta plain: A guide to the barrier islands, beaches, and shoals in Louisiana. Dept. of Natural Resources, Louisiana Geological Survey, 1985.

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Botswana. Dept. of Environmental Affairs., ed. Okavango Delta management plan. Dept. of Environmental Affairs, 2008.

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Binnie & Partners., United Nations Development Programme, World Bank, and Vietnam. Bộ khoa học, công nghệ và môi trường., eds. Red River Delta master plan. Government of Vietnam, Ministry of Science, Technology and Environment, 1995.

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Nigeria. Niger Delta regional development master plan. Niger Delta Development Commission, 2006.

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Binnie & Partners., Vietnam. Bộ khoa học, công nghệ và môi trường., United Nations Development Programme, and World Bank, eds. Red River Delta master plan: Background report. Government of Vietnam, Ministry of Science, Technology and Environment, 1994.

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Botswana. Dept. of Environmental Affairs., ed. Communication strategy for the Okavango Delta Management Plan. Dept. of Environmental Affairs, 2006.

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Ng, Mee Kam. The Pearl River Delta urban system plan: An analysis. Hong Kong Institute of Asia-Pacific Studies, Chinese University of Hong Kong, 1997.

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Book chapters on the topic "Delta plain"

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Woodroffe, Colin D. "Delta Plain." In Encyclopedia of Estuaries. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-8801-4_295.

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Barman, Nilay Kanti, Soumendu Chatterjee, and Ashis Kumar Paul. "Shoreline Dynamics in Subarnarekha Delta Plain." In SpringerBriefs in Geography. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-33575-9_4.

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Barman, Nilay Kanti, Soumendu Chatterjee, and Ashis Kumar Paul. "Beach Morphodynamics in Subarnarekha Delta Plain." In SpringerBriefs in Geography. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-33575-9_5.

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Barman, Nilay Kanti, Soumendu Chatterjee, and Ashis Kumar Paul. "Context and Background of the Subarnarekha Delta Plain." In SpringerBriefs in Geography. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-33575-9_2.

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Mammì, Irene Maria, and Lorenzo Rossi. "Remote sensing for reconstruction of ombrone river delta beach ridges." In Monitoring of Mediterranean Coastal Areas: Problems and Measurement Techniques. Firenze University Press, 2024. https://doi.org/10.36253/979-12-215-0556-6.67.

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The study area is the Ombrone River delta (South of Tuscany, Italy), a wave dominated delta, formed during the last 2500 years. Beach ridges, a characteristic depositional landform of wave dominated delta, cross the entire coastal plain. They are associated with ancient shorelines, representing the result of river input and longshore transport variation. The aim of this study is combining different remote sensing data to obtain a very detailed mapping of all the beach ridges present in the area. Satellite images and aerial photos were used to discriminate beach ridges; Unmanned Aerial Vehicle
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Sar, Pinaki, Balaram Mohapatra, Soma Ghosh, Dhiraj Paul, Angana Sarkar, and Sufia K. Kazy. "Geomicrobiology of Arsenic-Contaminated Groundwater of Bengal Delta Plain." In Handbook of Metal-Microbe Interactions and Bioremediation. CRC Press, 2017. http://dx.doi.org/10.1201/9781315153353-23.

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Sar, Pinaki, Balaram Mohapatra, Soma Ghosh, Dhiraj Paul, Angana Sarkar, and Sufia Kazy. "Geomicrobiology of Arsenic-Contaminated Groundwater of Bengal Delta Plain." In Handbook of Metal-Microbe Interactions and Bioremediation. CRC Press, 2017. http://dx.doi.org/10.1201/9781315153353-24.

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Darwish, Kamal Srogy. "Physical Characteristics of the Nile Delta’s Coastal Plain." In Hazard Modeling and Assessment of the Nile Delta Coast. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-44324-4_2.

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Rahman, Mohammad Mahmudur, Khitish Chandra Saha, Subhas Chandra Mukherjee, et al. "Groundwater Arsenic Contamination in Bengal Delta and Its Health Effects." In Safe and Sustainable Use of Arsenic-Contaminated Aquifers in the Gangetic Plain. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16124-2_14.

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Apel, Heiko, Nguyen Nghia Hung, Trinh Thi Long, and Vo Khac Tri. "Flood Hydraulics and Suspended Sediment Transport in the Plain of Reeds, Mekong Delta." In Springer Environmental Science and Engineering. Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-3962-8_8.

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Conference papers on the topic "Delta plain"

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Said, Nahar Said, Purwanto Purwanto, and Muhammad Ramli. "Low Wall Slope Stability Design on Swamp Material Using Bishop and Janbu Simplified Limit Equilibrium Method." In International Conference on Research in Engineering and Science Technology (IC-REST) 2023. Trans Tech Publications Ltd, 2025. https://doi.org/10.4028/p-ncpk4e.

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Coal mine slope stability is an important aspect of mining activities. The research site is located at Pit PQRT in Berau Regency, East Kalimantan. The research area is a freshwater peat swamp area located on a delta plain with tidal influence. The swamp material is located on the low wall side of the mine. Slope stability in the study area, which is composed of soft swamp material needs special attention because it is a major problem in the design of mining slope geometry. However, the availability of mine slope infrastructure in the form of active roads and sediment ponds also needs attention
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Gabriel, Popescu, Costel Ungureanu, Eugen Gavan, and Florin Moruzov. "THE STUDY OF THE INFLUENCE OF THE FORWARD SPEEDS OF A PATROL VESSEL ON THE BANKS OF THE CANALS IN THE DANUBE DELTA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/3.2/s11.18.

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The basic argument of the present study lies in the request of the agency of the Danube Delta Biosphere regarding the regulation of travel speeds of different types of boats. One among the cases of analysis was the one that refers to a patrol vessel. The purpose of this paper aims to follow the creation and study of the displacement of a ship of maritime patrol produced by the Damen company, inside the Danube Delta on 3 channels of different sizes. To carry out this work, the patrol vessel named "Stan Patrol" it was created in the AutoCAD. The results of this study are expressed in graphs that
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C. Cuaves Gozalo, M., M. E. Donselaar, and C. R. Geel. "Recognition and Architecture of Incised Paleovalleys in Delta-Plain Environments." In 57th EAEG Meeting. EAGE Publications BV, 1995. http://dx.doi.org/10.3997/2214-4609.201409613.

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KHALIL, SYED M., RICHARD C. RAYNIE, and BETH M. FORREST. "LOUISIANA SEDIMENT MANAGEMENT PLAN (LASMP): REGIONAL SEDIMENT MANAGEMENT FOR SEDIMENTOLOGICAL RESTORATION OF A DEGRADING DELTA PLAIN." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0257.

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Ortiz, Alejandra, Samapriya Roy, and Douglas A. Edmonds. "MARSH COLLAPSE BY POND EXPANSION ON THE MISSISSIPPI RIVER DELTA PLAIN." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303557.

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Allen, Rachel M., and J. Bradford Hubeny. "GEOPHYSICAL ANALYSIS OF A POORLY DRAINED GLACIAL DELTA PLAIN IN ACWORTH, NEW HAMPSHIRE." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291384.

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Garcia de Figueiredo Jr, Alberto, Cleverson Guizan Silva, Sidney Luiz de Mattos Mello, et al. "GPR investigation on a beach ridge coastal plain, Paraíba do Sul River delta." In 8th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.168.arq_890.

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Vegas-Vilarrúbia, T., P. López, F. Baritto, G. Meleán, M. E. Ponce, and O. Gómez. "Vegetation - soils relationships in a wetland area of the Orinoco delta plain (Venezuela)." In COASTAL ENVIRONMENT 2006. WIT Press, 2006. http://dx.doi.org/10.2495/cenv060301.

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Adhikari, Jishnu, Debashis Chatterjee, Shilajit Barua, and Thomas R. Kulp. "GROUNDWATER ARSENIC IN SHALLOW AQUIFERS OF BENGAL DELTA PLAIN (WEST BENGAL): A MICROBIOLOGICAL APPROACH." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286096.

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MINER, MICHAEL D., IOANNIS Y. GEORGIOU, MARK KULP, and DUNCAN FITZGERALD. "MISSISSIPPI RIVER DELTA PLAIN BARRIER ISLAND SEDIMENT DYNAMICS AND IMPLICATIONS FOR MANAGING COASTAL TRANSGRESSION." In Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0191.

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Reports on the topic "Delta plain"

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McNeil, D. H., J. Dixon, and K. M. Bell. The age, foraminifera, and palynology of the Upper Cretaceous Eagle Plain Group, northern Yukon. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328237.

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A re-evaluation of the age of the formations comprising the Eagle Plain Group of northern Yukon was necessitated by widely disparate age determinations in recent years from various authors. Maximum age estimates for the base of the group have varied from middle Albian to Cenomanian, and age estimates for the uppermost strata varied by an even greater range, from Cenomanian to late Maastrichtian. A re-examination of new and archival foraminiferal and palynological data indicates an age range of Cenomanian to late Maastrichtian for the Eagle Plain Group. The late Maastrichtian age is derived fro
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Midwinter, D., T. Hadlari, and K. Dewing. Upper Triassic to Lower Jurassic stratigraphy along the northeastern margin of the Sverdrup Basin, Axel Heiberg and Ellesmere islands, Nunavut: new data from measured sections. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329398.

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Two stratigraphic sections were measured through Late Triassic - Early Jurassic aged strata in the Blue Mountains map area (NTS 340-B/11) on Ellesmere Island and the Depot Point map area (NTS 049-G/7) on Axel Heiberg Island. These sections are subdivided in terms of established member and formation names based on previous mapping along the north-eastern margin of the Sverdrup Basin. The lowermost strata in the Heiberg Formation, the Romulus Member (510-575 m thick), is a coarsening-upward succession of mudstone to fine-grained sandstone from a prodelta to delta plain environment. The overlying
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Alexander, Chris. PR652-184505-R01 Evaluating Installation Techniques for Pipeline Repair Methods. Pipeline Research Council International, Inc. (PRCI), 2021. http://dx.doi.org/10.55274/r0012029.

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A testing program was conducted to evaluate the effects of internal pressure during the installation of composite and steel sleeves repair systems on pipelines with plain dents. The testing program included cyclic pressure testing a group of 12.75-inch OD x 0.188-inch WT, Grade X42 pipe samples with plain dents having residual dent depths on the order of 3% to 4% of the pipe's outside diameter. The dent samples were repaired using four (4) different composite repair systems, type-A steel sleeves, and steel thermal compression sleeves. The composite repair systems included a carbon fiber wet-la
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Kerr, D. E. Reconnaissance surficial geology, Beechey Lake, Nunavut, NTS 76-G. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329669.

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Preliminary mapping studies of Beechey Lake map area, through aerial photograph interpretation and limited legacy data, improve our understanding of surficial sediments and glacial history. The area is dominated by glacially and meltwater-scoured bedrock, hummocky moraine, till of varying thickness occasionally streamlined, and thin ridged till. Glacial lake sediments are predominantly in river valley lowlands. Glaciolacustrine delta and raised beach elevations range from 410 m to 230 m and 440 m to 290 m, respectively. Glaciofluvial deposits consist of eskers, ice-contact mounds, proglacial o
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Kerr, D. E. Reconnaissance surficial geology, Arctic Sound, Nunavut, NTS 76-N. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321440.

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The Arctic Sound map area consists primarily of glacially scoured bedrock, minor till in the southwest, and postglacial marine sediments in coastal lowlands and inland along river valleys. The till deposits are cut to bedrock by subglacial meltwater corridors defined by eskers and other glaciofluvial sediments. Glacial lakes occupied the James River valley where retreating or stagnant ice blocked drainage to the east. Glaciolacustrine deltas record falling lake levels, from 310 m to 290 m and 260 m elevation. Striations and streamlined landforms indicate ice flow to the north-northwest, and la
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Kerr, D. E. Reconnaissance surficial geology, Tinney Hills, Nunavut, NTS 76-J. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321821.

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The Tinney Hills map area consists primarily of glacially and meltwater scoured bedrock, discontinuous till in the southwest and central-east, and postglacial marine sediments in coastal lowlands and along river valleys inland. The boundaries of many till deposits are cut to bedrock by widespread subglacial meltwater erosion. Ridged till in particular, is often associated with eskers and other glaciofluvial sediments and meltwater erosion. Striations and streamlined till landforms indicate regional ice flow towards the north-northwest and northwest, and later crosscutting relationships recordi
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Smith, I. R., R. C. Paulen, and G W Hagedorn. Surficial geology, northeastern Cameron Hills, Northwest Territories, NTS 85-C/3, 4, 5, and 6. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328129.

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The northeastern Cameron Hills comprise a Cretaceous bedrock upland, rising &amp;amp;gt;550 m above the regional boreal plains. It was inundated by the Laurentide Ice Sheet and includes much of a prominent 60 by 20 km southwest-oriented mega-scale glacial lineation field, formed in thick till. Subsequent ice flow on northeast Cameron Hills occurred north to south, and a series of lobate and ice-thrust moraines suggest glacial surging. Rotational bedrock slumps cover the eastern and northern flanks of Cameron Hills, and extensive alluvial fan deposits draining from these slopes blanket the surr
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Kerr, D. E. Reconnaissance surficial geology, Bloody River, Northwest Territories-Nunavut, NTS 96-P. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329457.

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Preliminary surficial geology, based on airphoto interpretation and limited legacy field data of Bloody River map area, records a dynamic Late Wisconsin glacial landscape. Streamlined till and bedrock landforms, relating to Laurentide ice originating east of the map region, indicate regional westward flow diverged northwestward and southwestward at the eastern end of two topographic highs. Ice then converged between and south of these two highs, then diverged at the western end of these highlands. During deglaciation, ice stagnated in northwestern and central highland regions, forming extensiv
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McKean, Adam P., and Zachary W. Anderson. Interim Geologic Map of the Salt Lake City North Quadrangle, Salt Lake and Davis Counties, Utah. Utah Geological Survey, 2024. http://dx.doi.org/10.34191/ofr-768dm.

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The Salt Lake City North 7.5′ quadrangle is located in Salt Lake and Davis Counties from downtown Salt Lake City on the east to the Salt Lake International Airport on the west and extends north into Davis County to include the southern parts of the City of Bountiful and City of Woods Cross. The southern boundary of the quadrangle is at approximately 900 South Street in Salt Lake City. The quadrangle contains downtown Salt Lake City, the State Capitol building, the City of North Salt Lake, agricultural land, a number of oil refineries, a part of the Farmington Bay Waterfowl Management Area, and
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Joint Transboundary Action Plan In the Sesan and Srepok River Basin and the Mekong Delta of Cambodia and Viet Nam. Mekong River Commission Secretariat, 2019. http://dx.doi.org/10.52107/mrc.ajg671.

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The Joint Transboundary Action Plan sets out management arrangements to support transboundary cooperation between Cambodia and Viet Nam to strengthen sustainable water resources management and development of the Sesan and Srepok River Basins (2S River Basins) and Mekong Delta.
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