Academic literature on the topic 'Stratigraphic Geology Facies (Geology)'

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Journal articles on the topic "Stratigraphic Geology Facies (Geology)"

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Cross, Timothy, and Yohan Kusumanegara. "Stratigraphic Controls on Petrophysical Attributes and Fluid-Flow Pathways in an Exhumed Fluvial Reservoir." Mountain Geologist 54, no. 3 (2017): 129–45. http://dx.doi.org/10.31582/rmag.mg.54.3.129.

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Fluvial, floodplain and lake strata of the Green River Formation (Eocene) occur within an exhumed oil reservoir exposed in a quarry near Sunnyside, Utah. Strata in the quarry highwalls define three, asymmetrical, 15- to 20-m thick, base-level-rise genetic sequences arranged in a long-term base-level-rise (landward stepping) stacking pattern. Variable intensity of oil stain on rock surfaces is a qualitative measure of pore volumes, as all permeable facies are fully saturated with oil. Visual estimates of oil-stain intensity, combined with petrophysical measurements and petrographic analysis of
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Munsterman, D. K., R. M. C. H. Verreussel, H. F. Mijnlieff, N. Witmans, S. Kerstholt-Boegehold, and O. A. Abbink. "Revision and update of the Callovian-Ryazanian Stratigraphic Nomenclature in the northern Dutch offshore, i.e. Central Graben Subgroup and Scruff Group." Netherlands Journal of Geosciences - Geologie en Mijnbouw 91, no. 4 (2012): 555–90. http://dx.doi.org/10.1017/s001677460000038x.

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AbstractExploration in a mature basin requires a detailed classification and standardisation of rock stratigraphy to adequately comprehend the depositional history and prospect architecture. The pre-Quaternary Stratigraphic Nomenclature of the Netherlands compiled by Van Adrichem Boogaert & Kouwe in 1993 provided a consistent framework for use by the Dutch geological community. Over the past twenty years, new biostratigraphic techniques and continued exploration in the Netherlands have provided additional stratigraphic information. Based on this information the Late Jurassic lithostratigra
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Vacek, František, Jindřich Hladil, and Petr Schnabl. "Stratigraphic correlation potential of magnetic susceptibility and gamma-ray spectrometric variations in calciturbiditic facies (Silurian-Devonian boundary, Prague Synclinorium, Czech Republic)." Geologica Carpathica 61, no. 4 (2010): 257–72. http://dx.doi.org/10.2478/v10096-010-0015-2.

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Stratigraphic correlation potential of magnetic susceptibility and gamma-ray spectrometric variations in calciturbiditic facies (Silurian-Devonian boundary, Prague Synclinorium, Czech Republic)Magnetic susceptibility (MS) and gamma-ray spectrometry (GRS) stratigraphy were used for correlation and characterization of eight Silurian-Devonian (S-D) sections in the Prague Synclinorium (Czech Republic). They represent two different facies developments: lower subtidal to upper slope deposits and slope-to-basin-floor distal calciturbidites. Sections from relatively shallow- and deep-water sections ar
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Isla, Manuel F., Ernesto Schwarz, Gonzalo D. Veiga, Jerónimo J. Zuazo, and Mariano N. Remirez. "Discriminating intra-parasequence stratigraphic units from two-dimensional quantitative parameters." Journal of Sedimentary Research 91, no. 8 (2021): 887–911. http://dx.doi.org/10.2110/jsr.2020.203.

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ABSTRACT The intra-parasequence scale is still relatively unexplored territory in high-resolution sequence stratigraphy. The analysis of internal genetic units of parasequences has commonly been simplified to the definition of bedsets. Such simplification is insufficient to cover the complexity involved in the building of individual parasequences. Different types of intra-parasequence units have been previously identified and characterized in successive wave-dominated shoreface–shelf parasequences in the Lower Cretaceous Pilmatué Member of the Agrio Formation in central Neuquén Basin. Sediment
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Kontorovich, A. E., A. I. Varlamov, A. S. Efimov, et al. "Stratigraphic Scheme of Cambrian Deposits, South of the Cis-Yenisei Area of West Siberia." Russian Geology and Geophysics 62, no. 03 (2021): 357–76. http://dx.doi.org/10.2113/rgg20204317.

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Abstract ––In this paper we present a stratigraphic scheme for the subdivision and correlation of the Cambrian deposits in the south of the cis-Yenisei area of West Siberia, which was adopted as a current scheme by the decision of the Interdepartmental Stratigraphic Committee in 2018. This scheme is based on the data from stratigraphic test wells (Lemok-1, Averinskaya-150, Tyiskaya-1, Vostok-1, Vostok-3, Vostok-4, etс.). In the study area, two structure-facies zones were identified: Kas (Lemok-1, Averinskaya-150, Tyiskaya-1, Vostok-4, and Eloguiskaya-1 wells), where sedimentary complexes accum
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Sharpe, David R., and Peter J. Barnett. "Significance of Sedimentological Studies on the Wisconsinan Stratigraphy of Southern Ontario." Géographie physique et Quaternaire 39, no. 3 (2007): 255–73. http://dx.doi.org/10.7202/032607ar.

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ABSTRACTDetailed facies mapping along Lake Erie and Lake Ontario Bluffs, plus other studies illustrate that sedimentological studies, especially those with geomorphic or landform control, have had three main effects on the Wisconsinan stratigraphy of Ontario: (1) improved understanding of depositional processes and environments of several major rock stratigraphic units, without altering the stratigraphic framework, (2) aided correlation of drift sequences, and (3) questioned previous interpretations and stratigraphic correlations of drift sequences. Thus sedimentological analysis can not be se
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Alsop, G. I. "The geometry and structural evolution of a crustal-scale Caledonian fold complex: the Ballybofey Nappe, northwest Ireland." Geological Magazine 131, no. 4 (1994): 519–37. http://dx.doi.org/10.1017/s0016756800012139.

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AbstractThe gross geometries exhibited by crustal-scale fold nappes are considered a consequence of both original stratigraphic relationships associated with sub-basin configuration, coupled with the nature of the structural regime and tectonic processes involved in the generation of the nappe pile. The Neo-Proterozoic Dalradian metasediments of northwestern Ireland provide a well-constrained and correlatable stratigraphy which defines a sequence of sub-reclined, tight-isoclinal Caledonian (c. 460 Ma) fold nappes. Within this fold complex, the dominant structure is the crustal-scale Ballybofey
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Rigueti, Ariely L., Patrick Führ Dal' Bó, Leonardo Borghi, and Marcelo Mendes. "Bioclastic accumulation in a lake rift basin: The Early Cretaceous coquinas of the Sergipe–Alagoas Basin, Brazil." Journal of Sedimentary Research 90, no. 2 (2020): 228–49. http://dx.doi.org/10.2110/jsr.2020.11.

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ABSTRACT Coquinas constitute widespread deposits in lacustrine, estuarine, and shallow marine settings, where they are a valuable source of information on environmental conditions. Thick coquina successions were deposited in a series of lacustrine rift basins that formed along the Brazilian Continental Margin during the early stages of the opening of the South Atlantic Ocean, in the Early Cretaceous. In the Sergipe–Alagoas Basin, the coquina sequence, equivalent to the Morro do Chaves Formation, crops out in the Atol Quarry, and is considered a relevant analog for the economically important hy
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Lin, Wen, David Kynaston, Curtis Ferron, Janok P. Bhattacharya, and William Matthews. "Depositional and sequence stratigraphic model of transgressive shelf sandstone: The Late Cretaceous Tocito Sandstone, San Juan Bain, New Mexico, U.S.A." Journal of Sedimentary Research 91, no. 4 (2021): 415–32. http://dx.doi.org/10.2110/jsr.2020.121.

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ABSTRACT There has long been debate about the origin of long, linear, isolated shallow marine sandstones. In the 1980s these were routinely interpreted as wave- or tide-modulated shelf sandstones. With the advent of sequence stratigraphy, many of these sandstones were reinterpreted as top-truncated forced-regressive to lowstand delta or shoreface, inviting the question regarding whether the concept of a shelf sandstones remain a viable depositional model. More recent syntheses demonstrate that shelf sands tend to be derived by reworking of underlying sediment through transgressive erosion and
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Diez, José B., Sylvie Bourquin, Jean Broutin, and Javier Ferrer. "The Iberian Permian Triassic ‘Buntsandstein’ of the Aragonian branch of the Iberian range (Spain) in the West-European sequence stratigraphical framework: a combined palynological and sedimentological approach." Bulletin de la Société Géologique de France 178, no. 3 (2007): 179–95. http://dx.doi.org/10.2113/gssgfbull.178.3.179.

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Abstract The Permo-Triassic ‘Buntsandstein’ facies was studied from outcrops in the Aragonian branch of the Iberian range (Zaragoza, Spain). Using an integrated analysis of sedimentological and palynological data, we propose a sequence stratigraphic analysis for the Permo-Triassic deposits in this area. A comparison with the stratigraphical cycles of other parts of the Iberian domain and other peri-Tethyan basins enables us to specify the stratigraphic context of the Lower Triassic in the western European domain and characterize the importance of the Lower Triassic hiatus. The ‘Buntsandstein’
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Dissertations / Theses on the topic "Stratigraphic Geology Facies (Geology)"

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Moukhsil, Abdelali. "Géochimie, pétrologie structurale et mode de mise en place du pluton de Father, zone volcanique nord, sous-province de l'Abitibi, Canada /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1996. http://theses.uqac.ca.

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Lichtblau, Andreas. "Stratigraphy and facies at the south margin of the Archean Noranda Caldera." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1989. http://theses.uqac.ca.

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Xu, Jingqi. "Facies and sequence stratigraphic analyses of the Upper Ordovician shales in northeast Indiana and northwest Ohio." Thesis, Indiana University, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=10142334.

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<p> The Upper Ordovician Maquoketa Group equivalent strata in Indiana and Ohio were part of a westward-thinning shale-dominant succession. Large amounts of fine-grained siliciclastics were shed from the eastern highlands during the Taconic Orogeny. </p><p> The detailed lithofacies analysis of the Upper Ordovician shales has yielded recognition of a series of genetically related sequences in a seemingly homogenous succession. The lower succession is pyritic laminated/banded organic-rich mudstone that accumulated after the onset of a major flooding event. Cryptobioturbation, bottom current rip
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Klute, Margaret Anne. "Sedimentology, sandstone petrofacies, and tectonic setting of the Late Mesozoic Bisbee Basin, southeastern Arizona." Diss., The University of Arizona, 1991. http://hdl.handle.net/10150/185723.

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The Late Mesozoic Bisbee basin of southeastern Arizona was an intracratonic back-arc rift basin. Extension was coupled with seafloor spreading in the Gulf of Mexico and back-arc extension behind a magmatic arc along the convergent Pacific continental margin. Tectonostratigraphic evolution of the basin occurred in three phases. Initial mid-Jurassic rifting of the basin, marked by eruption of the Canelo Hills Volcanics, may have been complicated by sinistral strike-slip motion along the Mojave-Sonora megashear. During continued rifting, from latest Jurassic to Early Cretaceous time, the Glance C
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Davis, Laurence H. M. "Allostratigraphic interpretation of a modern coarse clastic barrier complex : depositional facies, processes and relative sea level relationships /." Internet access available to MUN users only, 2003. http://collections.mun.ca/u?/theses,60897.

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Hill, Robert E. (Robert Einar). "Stratigraphy and sedimentology of the Middle Proterozoic Waterton and Altyn Formations, Belt-Purcell Supergroup, southwest Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63330.

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Martin, Keithan. "Integrating depositional facies and sequence stratigraphy in characterizing carbonate reservoirs: Mississippian limestone, western Kansas." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/20478.

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Master of Science<br>Geology<br>Matthew W. Totten<br>The Mississippian-aged St. Louis Limestone of Western Kansas is a carbonate resource play that has been producing oil, gas, and natural gas liquids (NGL) for over 50 years. The Mississippian Limestone is made up of heterogeneous limestones with interbedded layers of porous and non-porous units, abrupt facies changes, and diagenetic alterations. These factors combine to characterize the St. Louis Limestone's internal complexity, which complicates hydrocarbon exploration. This study focuses on improving the understanding of the geometry, distr
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Dalton, Edward. "Sedimentary facies and diagenesis of the Lower Devonian Temiscouata and Fortin Formations, Northern Appalachians, Quebec and New Brunswick." Thesis, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63856.

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Cassle, Christopher F. "Petrographic Analyses of Late Pennsylvanian Limestones within the Northern Appalachian Basin, USA." Ohio University / OhioLINK, 2005. http://www.ohiolink.edu/etd/view.cgi?ohiou1121435271.

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Pickett, Clarence. "A sedimentary facies analysis of the >2.8 Ga Beniah and Bell Lake formations, Slave Province, Northwest Territories." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2002. http://theses.uqac.ca.

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Books on the topic "Stratigraphic Geology Facies (Geology)"

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Qing Zang Gaoyuan ji lin qu Gangwana xiang di ceng di zhi xue. Di zhi chu ban she, 1997.

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Horsthemke, Ewald. Fazies der Karoosedimente in der Huab-Region, Damaraland, NW-Namibia. Im Selbstverlag der Geologischen Institute der Georg-August-Universität Göttingen, 1992.

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Oschmann, Wolfgang. Faziesentwicklung und Provinzialismus in Nordfrankreich und Südengland zur Zeit des obersten Jura (Oberkimmeridge-Portland). F. Pfeil, 1985.

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Zubrzycki, Adam. Analiza facjalna i rozwój pułapek litologicznych w utworach miocenu autochtonicznego zapadliska przedkarpackiego między Rzeszowem a Pilznem. Zakład Narodowy im. Ossolińskich, 1986.

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B, Edwards Marc, and Hansen, T. A. (Tor Arne), eds. Neoproterozoic glacial and associated facies in the Tanafjord-Varangerfjord area, Finnmark, north Norway. The Geological Society of America, 2012.

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Rice, A. H. N. Neoproterozoic glacial and associated facies in the Tanafjord-Varangerfjord area, Finnmark, north Norway. The Geological Society of America, 2012.

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Berthou, Pierre-Yves. Stratigraphic correlation by microfacies of the Cenomanian-Coniacian of the Sergipe Basin, Brazil. Universitetsforlaget, 1988.

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Herrmann, Regina. Entwicklung einer oberjurassischen Karbonatplattform: Biofazies, Riffe und Sedimentologie im Oxfordium der Zentralen Dobrogea (Ost-Rumänien). Fachbereich Geowissenschaften. FU Berlin, 1996.

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Reuter, Anselm. Analyse eines regradierenden Deltas im Mittel-Devon des Rheinischen Schiefergebirges. Im Selbstverlag der Geologischen Institute der Georg-August-Universität Göttingen, 1993.

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Armstrong, Augustus K. Facies, diagenesis, and mineralogy of the Jurassic Todilto Limestone Member, Grants uranium district, New Mexico. New Mexico Bureau of Mines & Mineral Resources, 1995.

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Book chapters on the topic "Stratigraphic Geology Facies (Geology)"

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Sarkar, Subir, and Santanu Banerjee. "Facies, Paleogeography and Sequence Stratigraphy." In Springer Geology. Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-32-9551-3_2.

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Dimuccio, Luca Antonio, Luís Vítor Duarte, and Lúcio Cunha. "Facies and Stratigraphic Controls of the Palaeokarst Affecting the Lower Jurassic Coimbra Group, Western Central Portugal." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_148.

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Wilmsen, Markus, Marisa Storm, Franz Theodor Fürsich, and Mahmoud Reza Majidifard. "Integrated Stratigraphy and Facies Analysis of the Upper Albian–Turonian (Cretaceous) Debarsu Formation (Yazd Block, Central Iran)." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_120.

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Wilmsen, Markus, and Emad Nagm. "Integrated Stratigraphy (Bio- and Sequence Stratigraphy) and Facies Analysis of the Upper Cenomanian–Turonian (Lower Upper Cretaceous) in the Eastern Desert, Egypt." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_119.

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Niebuhr, Birgit, Nadine Richardt, and Markus Wilmsen. "Cenomanian–Turonian (Early Late Cretaceous) Facies Development and Sequence Stratigraphy of the Danubian Cretaceous Group (Bavaria, Southern Germany)." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_107.

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AL-Ghamdi, Nasser, and Mike Pope. "High-Resolution Stratigraphic Architectures, Facies Anatomies of the Lower Cretaceous Biyadh and Shu’aiba Formations, and Their Implications on Platform Evolution and Global Correlation." In Regional Geology Reviews. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-21874-4_1.

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Pacht, Jory A., Bruce Bowen, Bernard L. Shaffer, and William R. Pottorf. "Systems Tracts, Seismic Facies, and Attribute Analysis Within a Sequence-Stratigraphic Framework—Example from the Offshore Louisiana Gulf Coast." In Frontiers in Sedimentary Geology. Springer New York, 1993. http://dx.doi.org/10.1007/978-1-4757-0160-9_2.

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De Castro, Joel Carneiro. "Facies, Reservoirs and Stratigraphic Framework of the Mossoró Member (Latest Cenomanian-Earliest Turonian) in Potiguar Basin, NE Brazil: An Example of a Tide and Wave Dominated Delta." In Frontiers in Sedimentary Geology. Springer New York, 1993. http://dx.doi.org/10.1007/978-1-4757-0160-9_8.

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Sarmiento-Rojas, Luis Fernando. "Cretaceous Stratigraphy and Paleo-Facies Maps of Northwestern South America." In Geology and Tectonics of Northwestern South America. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-76132-9_10.

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Brancolini, Giuliano, Alan K. Cooper, and Franco Coren. "Seismic Facies and Glacial History in the Western Ross Sea (Antarctica)." In Geology and Seismic Stratigraphy of the Antarctic Margin. American Geophysical Union, 2013. http://dx.doi.org/10.1029/ar068p0209.

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Conference papers on the topic "Stratigraphic Geology Facies (Geology)"

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Sharp, I. R., J. C. Embry, D. W. Hunt, et al. "Sequence Stratigraphic, Facies & Reservoir Framework for the Bangestan Group, Lurestan, Zagros Mountains, Iran." In Second Arabian Plate Geology Workshop 2010. EAGE Publications BV, 2010. http://dx.doi.org/10.3997/2214-4609.20145342.

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Ye, Q., K. D. Kelsch, D. Angstadt, K. Sukhdarshan, and R. Corley. "Sequence-stratigraphic Framework and Depositional Facies Interpretations in Late Jurassic to Early Cretaceous Section in Saudi Arabia/Kuwait Partitioned Zone (PZ)." In Fourth Arabian Plate Geology Workshop. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142789.

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Lubeseder, S., J. Kuss, and M. Zahran. "Mid Cretaceous Stratigraphy, Facies and Carbon-Isotope Curves of Northwest-Qatar." In Second Arabian Plate Geology Workshop 2010. EAGE Publications BV, 2010. http://dx.doi.org/10.3997/2214-4609.20145348.

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Memesh, A. M. S., Y. M. Le Nindre, S. M. Dini, and D. Vaslet. "Pre-Buwaib and Late Valanginian Unconformities in Outcrop: Inherited Concepts, Facts, and Stratigraphic Consistency." In Fourth Arabian Plate Geology Workshop. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142795.

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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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Neog, N., N. S. Rao, A. Al. Darmi, M. Y. M. Al.Dousiri, T. De Keyser, and C. G. S. C. Kendall. "Complex Carbonate Evaporite Reservoir Description Using Isotope Geo-chemistry and Ichno-facies to Fine-tune a High Resolution Sequence Stratigraphic Framework Model of Marrat Reservoirs." In Fifth EAGE Arabian Plate Geology Workshop 2015. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201411945.

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Gaillot, Jérémie, A. Virgone, B. Caline, and G. Frébourg and F. Gisquet. "The Khuff Formation in the Middle East: New Insight into Regional Stratigraphy and Palaeoenvironmental Reconstruction using Bio-assemblages and Facies Analysis." In Third Arabian Plate Geology Workshop. EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144045.

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Granath, James, Rolf Rango, Pete Emmet, Colin Ford, Robert Lambert, and Michael Kasli. "New Viewpoint on the Geology and Hydrocarbon Prospectivity of the Seychelles Plateau." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2556681-ms.

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ABSTRACT We have reprocessed, re-imaged, and interpreted 10000+ km of legacy 2D seismic data in the Seychelles, particularly in the western part of the Plateau. Seychelles data have been difficult to image, particularly for the Mesozoic section: volcanics are a major attenuator of low frequency signal, and a hard water bottom contributes to signal problems. Enhanced low frequency techniques were applied to improve the signal fidelity in the 4 to 20 Hz range, and to remove spectral notches of shallow geologic origin. These efforts have allowed a reasonable view of the structure of the Plateau t
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Masoud, Mohamed, W. Scott Meddaugh, Masoud Eljaroshi, and Khaled Elghanduri. "Enhanced and Rock Typing-Based Reservoir Characterization of the Palaeocene Harash Carbonate Reservoir-Zelten Field-Sirte Basin-Libya." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/205971-ms.

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Abstract The Harash Formation was previously known as the Ruaga A and is considered to be one of the most productive reservoirs in the Zelten field in terms of reservoir quality, areal extent, and hydrocarbon quantity. To date, nearly 70 wells were drilled targeting the Harash reservoir. A few wells initially naturally produced but most had to be stimulated which reflected the field drilling and development plan. The Harash reservoir rock typing identification was essential in understanding the reservoir geology implementation of reservoir development drilling program, the construction of repr
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Mutti, E., and R. Tinterri. "Facies and Processes of Turbidite Systems." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406005.

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Reports on the topic "Stratigraphic Geology Facies (Geology)"

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Karlstrom, Karl, Laura Crossey, Allyson Matthis, and Carl Bowman. Telling time at Grand Canyon National Park: 2020 update. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2285173.

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Grand Canyon National Park is all about time and timescales. Time is the currency of our daily life, of history, and of biological evolution. Grand Canyon’s beauty has inspired explorers, artists, and poets. Behind it all, Grand Canyon’s geology and sense of timelessness are among its most prominent and important resources. Grand Canyon has an exceptionally complete and well-exposed rock record of Earth’s history. It is an ideal place to gain a sense of geologic (or deep) time. A visit to the South or North rims, a hike into the canyon of any length, or a trip through the 277-mile (446-km) len
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McCuaig, S. Surficial geology and stratigraphic sections, Nass Valley and Kitsault Valley, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214295.

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Hickson, C. J., J. B. Mahoney, and P. Read. Geology of Big Bar map area, British Columbia: facies distribution in the Jackass Mountain Group. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193632.

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Evenchick, C. A., P. S. Mustard, J. S. Porter, and C. J. Greig. Regional Jurassic and Cretaceous facies assemblages, and structural geology in Bowser Lake map area [104A], B.C. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/183861.

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Koopman, E. R., M. R. Patterson, J. M. Franklin, and K. H. Poulsen. Stratigraphic and Structural Geology of the Lyon Lake Massive Sulphide Deposit, Sturgeon Lake, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132358.

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Pugh, D. C. Regional stratigraphic cross-sections of pre-Mesozoic geology, Great Bear River map area, District of Mackenzie. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/130006.

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Mountjoy, E. W., and S. E. Grasby. Geology of the Footwall of the Blackman Thrust and Facies Variations in Middle Miette Group, southern Selwyn Range, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132512.

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Young, M. D., H. Sandeman, F. Berniolles, and P. M. Gertzbein. A preliminary stratigraphic and structural geology framework for the Archean Mary River Group, northern Baffin Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215376.

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Schofield, A., R. A. Cayley, T. Barton, D. H. Taylor, M. Nicoll, and C. P. Cairns. Regional geology and mineral systems of the Stavely region, western Victoria: Data release 1 - Stratigraphic drilling field data. Geoscience Australia, 2015. http://dx.doi.org/10.11636/record.2015.013.

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Schofield, A., J. Clarke, E. N. Bastrakov, et al. Regional geology and mineral systems of the Stavely region, western Victoria: Data release 3 - Stratigraphic drilling lithology logs. Geoscience Australia and Geological Survey of Victoria, 2015. http://dx.doi.org/10.11636/record.2015.030.

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