Relevant bibliographies by topics / Deltaic Distributary

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

Academic literature on the topic 'Deltaic Distributary'

Author: Grafiati
Published: 5 June 2025
Last updated: 1 August 2025

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Journal articles on the topic "Deltaic Distributary"

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Jin, Chao, LangTao Liu, GuoQiang Hao, and Kuo Cao. "Sandstone bodies sedimentary characteristics of Shanxi formation, at Chengjiazhuang section in Liulin, Shanxi province, China." World Journal of Engineering 12, no. 2 (2015): 177–88. http://dx.doi.org/10.1260/1708-5284.12.2.177.

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Sedimentary facies type of the Shanxi Formation in northeastern Ordos Basin is an ongoing debate. Based on field measurements, sample collection and identification, and laboratory analysis, we systematically evaluated the sedimentary characteristics of the sandstone bodies of Shanxi Formation of Chengjiazhuang section in Liulin. Analysis included identifying sample composition, grain size, texture, sedimentary structure and spatial distribution. We came to the conclusion that the sedimentary environment of Shanxi Formation is deltaic. This deltaic environment included deltaic front and deltaic
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Payenberg, T. H. D., and S. C. Lang. "RESERVOIR GEOMETRY OF FLUVIAL DISTRIBUTARY CHANNELS—IMPLICATIONS FOR NORTHWEST SHELF, AUSTRALIA, DELTAIC SUCCESSIONS." APPEA Journal 43, no. 1 (2003): 325. http://dx.doi.org/10.1071/aj02017.

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The exploration and development of stratigraphically trapped hydrocarbons requires detailed knowledge of the morphologies and reservoir characteristics of the stratigraphic body. Fluvial distributary channels are important exploration targets because they are typically isolated reservoirs, laterally and vertically sealed by delta plain and abandoned channel mudstone, and thus form excellent stratigraphic traps. The morphology and reservoir characteristics of fluvial distributary channels have been confused with fluvial channels in the past. Knowing the characteristics of fluvial distributary c
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Van Yperen, Anna E., John M. Holbrook, Miquel Poyatos-Moré, and Ivar Midtkandal. "Coalesced Delta-front Sheet-like Sandstone Bodies from Highly Avulsive Distributary Channels: The Low-accommodation Mesa Rica Sandstone (Dakota Group, New Mexico, U.S.A.)." Journal of Sedimentary Research 89, no. 7 (2019): 654–78. http://dx.doi.org/10.2110/jsr.2019.27.

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Abstract Low-accommodation deltaic systems are often challenging to interpret due to their condensed, low-gradient nature, which often results in extensive, sheet-like sandstone bodies. As a result, detailed studies of such systems are scarce, and their internal depositional architecture is still poorly understood. We analyze one such system, the Cenomanian deltaic Mesa Rica Sandstone (Dakota Group), which was deposited in the Western Interior Seaway, in east-central New Mexico, USA. A > 20-km-long escarpment, subparallel to the main delta progradation direction, allows a detailed analysis
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Ge, Jiawang, Xiaomin Zhu, Brian G. Jones, Yue Zhang, Handong Huang, and Yu Shu. "Facies delineation and sandstone prediction using seismic sedimentology and seismic inversion in the Eocene Huizhou Depression, Pearl River Mouth Basin, China." Interpretation 6, no. 2 (2018): SD71—SD87. http://dx.doi.org/10.1190/int-2017-0155.1.

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Recently, the rift-related successions in the Eocene Huizhou (HZ) Depression have been considered crucial intervals for hydrocarbon exploration in the Pearl River Mouth Basin, China. However, the facies delineation and sandstone distribution are poorly understood due to the limited well data. Our study area is the HZ25 Block in the HZ Depression, which consists of a typical overlapped synthetic transfer zone connecting the HZ26 and XJ30 Sags. Integrated analysis of seismic and logging data indicates that the Eocene Wenchang Formation can be subdivided into four third-order sequences (SQ1–4). W
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Cao, Tongfeng, Jian Cui, Yingzheng He, Limin Ma, Wei Qiao, and Yuming Liu. "The Influence of Reservoir Architecture on the Connectivity of the Shahejie Formation in the Liuzhong Oilfield." Energies 17, no. 1 (2023): 115. http://dx.doi.org/10.3390/en17010115.

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The lack of research on fine reservoir structure and sand body patterns in the Jidong Oilfield currently restricts the efficient development of the oilfield. Therefore, this article mainly focuses on the study of the main types of facies of the Shahejie Formation, sand body splicing patterns, and the degree of sand-body connectivity. The interpretation and analysis of well-logging, three-dimensional (3D) seismic, and production data were used to lay the foundation for the study and evaluate the remaining oil distribution. The results indicate that the reservoir sandstones in the study area wer
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Olsen, T. "Photogrammetric mapping of fluvial channel sand-bodies in the Atane Formation at Paatuut, Nuussuaq, central West Greenland." Rapport Grønlands Geologiske Undersøgelse 156 (January 1, 1992): 41–46. http://dx.doi.org/10.34194/rapggu.v156.8190.

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Upper Cretaceous deltaic sediments from the Atane Formation are well exposed in a series of steep-sided gullies at Paatuut on the south coast of Nuussuaq. The large exposures within the gullies allowed a large-scale sedimentological investigation of delta stratigraphy, sand-body geometry and fluvial style of the distributary channels. Multi-model photogrammetry was applied in several ways. Photogrammetric mapping of good exposures within the area produced accurate vertical sections up to 2 km long and 0.5 km high. A bed to bed stratigraphy of the delta cycles was established and the sand-bodie
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Phillips, Stephen, and Hudson Hudson. "The Upper Cretaceous Rock Springs Formation of northwest Colorado." Geology of the Intermountain West 8 (January 17, 2022): 45–71. http://dx.doi.org/10.31711/giw.v8.pp45-71.

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The Upper Cretaceous Rock Springs Formation of the Mesaverde Group in northwestern Colorado, southwestern Wyoming, and northeastern Utah is composed of fluvial, deltaic, and marine sediments that record the regression of the Western Interior Seaway during the Early to Middle Campanian. Contemporaneous deposits are present along the eastern and southeastern margins of the Greater Green River Basin in Wyoming, but correlation across the basin is challenging. Analysis of a small (1-km-long), understudied outcrop in northwestern Colorado assists in bridging that gap. The outcrop consists of distal
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Chen, Hehe, Xiaomin Zhu, Ruisheng Shi, and Zili Zhang. "Seismic geomorphology of shoal-water deltaic and mixed carbonate-siliciclastic beach-bar systems in hanging wall of rift basins: Paleogene of the Raoyang Sag, Bohai Bay Basin, China." Interpretation 8, no. 2 (2020): SF1—SF19. http://dx.doi.org/10.1190/int-2019-0108.1.

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Recent studies of ancient rift basins focus on the tectonosedimentary models, which emphasize the control of tectonics on the distribution and evolution of depositional systems in rift basins, whereas these studies seldom address stratigraphic dominated depositional models. Compared to footwall depositional systems, hanging wall depositional systems are especially underexplored due to their fine-grained, thin-layered, and widely distributed features. We integrated seismic data, cores, and well logs to define the dispersal of hanging wall depositional systems that are related to the fluctuation
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Ambrose, William A. "Shelf and Lower-Shoreface Deposits in the Upper Midway Group and the Transition into Fluvial-Dominated Deltaic Deposits in the Hooper Formation (Lower Wilcox Group) in the Southeastern Texas Gulf Coast." Gulf Coast Association of Geological Societies Journal 13 (2024): 34–52. http://dx.doi.org/10.62371/kcuk6360.

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The Paleocene Upper Midway Group in the southeastern Texas Gulf Coast records a stratigraphic succession of shelf and lower-shoreface systems. Four (4) recognition criteria for these systems include (1) thin (<2 ft [<0.6 m]), erosion-based and lenticular, very fine-grained and fine-grained sandstone beds with swaley cross-stratification, (2) a diverse Cruziana trace-fossil assemblage consisting of Teichichnus, Palaeophycus, Planolites, and Schaubcylindrichnus, (3) net-sandstone trends consisting of strike-elongate ribbons and pods that merge updip (north and northwest) into broad, sheet-
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FENG, Congjun, Zhidong BAO, Ling YANG, Xiong SI, Guibin XU, and Xiong HAN. "Reservoir architecture and remaining oil distribution of deltaic front underwater distributary channel." Petroleum Exploration and Development 41, no. 3 (2014): 358–64. http://dx.doi.org/10.1016/s1876-3804(14)60040-9.

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Dissertations / Theses on the topic "Deltaic Distributary"

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Britsch, Louis D. "Geomorphic History of the Atchafalaya Backwater Area: Upper Deltaic Plain Development." ScholarWorks@UNO, 2007. http://scholarworks.uno.edu/td/637.

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Earlier researchers have produced conceptual models of Mississippi River delta plain development which divide the deltaic plain into upper and lower reaches. The upper deltaic plain has been described as an area composed mainly of lacustrine, lacustrine delta, backswamp, and crevasse channels, with minimal distributary development. The lower deltaic plain is characterized by numerous distributaries forming distributary systems and lobes. Detailed geomorphic mapping and chronologic reconstruction within the Atchafalaya Backwater Area of the upper deltaic plain of the Mississippi River has
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Bertoli, Giuseppe Colonnello. "The environmental impact of flow regulation in a tropical delta : the case of the Manamo distributary in the Orinoco Delta, Venezuela." Thesis, Loughborough University, 2001. https://dspace.lboro.ac.uk/2134/8947.

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The regulation of the Manama river, one of the major Orinoco distributary channels, has instigated changes in the hydrological and sedimentological regimes of its channel and surrounding wetlands, covering one-third of the Delta area. The dam has altered the hydrodynamics of the Manama. While the average flow of its channel was reduced from 10% to 0.5% (200 m3/s), of the annual discharge of the Orinoco River. The adjacent Macareo distributary, which is not regulated, discharges 11% (4,000 m3/s) annually. During the seasonal high-water period, the water level in the Macareo rises approximately
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Conti, Matteo. "Studio morfo-batimetrico dei canali distributori del delta del Po di Pila." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2015. http://amslaurea.unibo.it/8247/.

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In questa tesi sono state analizzate, a partire da dati batimetrici ad alta risoluzione ottenuti tramite tecnologia multibeam, le morfologie caratteristiche dei tre canali tributari del Delta del Po di Pila: Busa di Dritta, Busa di Tramontana, Busa di Scirocco. Lo studio è stato effettuato col software Global Mapper, che ha permesso la mappatura e l’analisi morfometrica dei principali elementi morfologici osservati, ovvero aree depresse, zone con presenza di forme di fondo, zone a fondo piano e depositi da instabilità gravitativa sulle sponde dei canali. La loro distribuzione nei vari tratti
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Wiweko, Agung. "Sedimentary facies and depositional geometry of distributary mouth bars in Tunu Field Miocene Kutei Basin and comparison with modern Mahakalm Delta." Thesis, Queensland University of Technology, 1998.

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Edmonds, Douglas A. Slingerland Rudy. "The growth and evolution of river-dominated deltas and their distributary networks." 2009. http://etda.libraries.psu.edu/theses/approved/PSUonlyIndex/ETD-3744/index.html.

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Shaw, John Burnham. "The kinematics of distributary channels on the Wax Lake Delta, coastal Louisiana, USA." Thesis, 2013. http://hdl.handle.net/2152/25220.

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The Wax Lake Delta (WLD) is a sandy, modern river delta prograding rapidly into Atchafalaya Bay. This dissertation uses field data to improve the understanding of channel kinematics that dictate river delta geometry and stratigraphy, while providing a framework for coastal restoration efforts. The studies presented here show that the distributary channel network of the WLD is erosional. In the first study, analyses of the feeder channel to the WLD and the channel network within the sub-aerially emergent delta show that the channel bed has incised into the consolidated muds that act as bedrock.
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Michaud, Kain. "Facies Architecture and Stratigraphy of Tidal Ridges in the Eocene Roda Formation, Northern Spain." Thesis, 2011. http://hdl.handle.net/1974/6486.

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ABSTRACT The Eocene Roda Formation in northern Spain documents the deposits from a range of coastal depositional environments. These include alluvial plains, distributary channels, mouth bars, upper to lower-shorefaces, and tidal shelf ridges. Eighteen progradational sand tongues that are interpreted as parasequences compose two third-order sequences. Sequence 1 accumulated in an environment with strong tidal currents and high rates of progradation, while Sequence 2 was deposited under relatively weaker currents and higher rates of aggradation, which produced a higher mudstone:sandstone ra
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Books on the topic "Deltaic Distributary"

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Andrén, Hans. Development of the Laitaure Delta, Swedish Lappland: A study of growth, distributary forms and processes. Uppsala University, Institute of Earth Sciences, 1994.

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Book chapters on the topic "Deltaic Distributary"

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Moiola, Richard J., Joann E. Welton, John B. Wagner, et al. "Integrated Analysis of the Upper Ferron Deltaic Complex, Southern Castle Valley, Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c4.

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Abstract The Upper Ferron Sandstone in southern Castle Valley, Utah, is a river-dominated deltaic complex made up of seaward-stepping, vertically stacked, and landward-stepping cycles. These cycles, which consist of delta plain, delta front, and prodelta/offshore facies associations, are partitioned by flooding surfaces that detailed biostratigraphic analysis indicates lack an open marine signature. They are thought to be abandonment flooding surfaces associated with delta lobe switching. The abundance of distributary channel belts associated with all cycles suggests that riverine processes co
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Bhattacharya, Janok P., and Robert S. Tye. "Searching for Modern Ferron Analogs and Application to Subsurface Interpretation." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c2.

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Abstract A quantitative approach to selecting modern-depositional settings analogous to those of the Cretaceous Ferron Sandstone is presented as well as an approach to using these analogs to improve subsurface interpretations. Paleotectonic, paleogeographic, and climatic setting of the U.S. Western Interior are integrated to estimate the size of the Ferron drainage network to be 50,000 km 2(19,000 mi 2). Estimates of flow depths, flow velocities, and channel cross-sectional areas suggest maximum trunk river paleo-discharge was on the order of 50 × 10 9m 3/year (250 × 10 9ft 3/year).
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Anderson, Paul B., Thomas C. Chidsey, Thomas A. Ryer, Roy D. Adams, and Kevin McClure. "Geologic Framework, Facies, Paleogeography, and Reservoir Analogs of the Ferron Sandstone in the Ivie Creek Area, East-Central Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c13.

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Abstract The Ferron Sandstone of east-central Utah has world-class outcrops of dominantly fluvial-deltaic, Turonian-Coniacian-aged strata deposited along the margins of the rapidly subsiding Cretaceous foreland basin. The Ferron consists of a series of stacked, transgressive-regressive cycles which form an eastward-thinning wedge. The Ivie Creek area contains abrupt facies changes in two of these cycles referred to as Kf-1 and Kf-2. Kf-1 consists of unusual river-dominated delta deposits that prograde southeast to northwest across the Ivie Creek area. Progradation is parallel or onshore to the
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Bergh, T. C. V. van den, and James R. Garrison. "The Geometry, Architecture, and Sedimentology of Fluvial and Deltaic Sandstones Within the Upper Ferron Sandstone Last Chance Delta." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c18.

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Abstract The Turonian-Coniacian Upper Ferron Sandstone Last Chance Delta was deposited along the western margin of the Western Interior Seaway as a wave-modified, river-dominated deltaic system. The Last Chance Delta was deposited during a slow relative sea-level rise whose rate of rise decreased with time. The sedimentation rate progressively decreased throughout the deposition of the Last Chance Delta. Architectural and sedimentological data for deltaic near-marine sandstones indicate that primary deltaic depositional style is directly correlated with degree of wave-modification, which is co
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Corbeanu, Rucsandra M., Michael C. Wizevich, Janok P. Bhattacharya, Xiaoxiang Zeng, and George A. McMechan. "Three-Dimensional Architecture of Ancient Lower Delta-Plain Point Bars Using Ground-Penetrating Radar, Cretaceous Ferron Sandstone, Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c17.

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Abstract Accurate three-dimensional description of reservoir architecture using outcrop analogs is hampered by limited exposure of essentially two-dimensional outcrops. This study contains the first fully three-dimensional description of ancient marine-influenced point bar sandstones of lower delta-plain distributary channels and is based on the integration of detailed outcrop and drill-hole data, and two-and three-dimensional ground-penetrating radar data. The studied outcrops are in the Cretaceous Ferron Sandstone of east-central Utah. Point bars deposited in marine-influenced, lower delta-p
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Dewey, John A., and Thomas H. Morris. "Geologic Framework of the Lower Portion of the Ferron Sandstone in the Willow Springs Wash Area, Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c12.

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Abstract Three-dimensional outcrop exposures of the Ferron Sandstone in the Willow Springs Wash area of east-central Utah illustrate the importance of recognizing allocyclic and autocyclic processes in marginal-marine settings. Three chronostratigraphically distinct wave-dominated shoreline sandstone successions display vertical offset at their landward pinchouts. These coarsening upward successions are interpreted to be parasequences produced by allocyclic processes. Fluids trapped within these sandstones may be compartmentalized by this vertical offset. In contrast, a fluvial-dominated coars
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Anderson, Paul B., and Thomas A. Ryer. "Regional Stratigraphy of the Ferron Sandstone." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c8.

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Abstract The Ferron Sandstone Member of the Mancos Shale is divided informally into upper and lower units. The upper Ferron has been divided by earlier workers into seven or eight delta-front units. These units correspond to parasequence sets. We suggest one additional delta-front or parasequence set, bringing the total to nine for the upper Ferron. The opportunity to study many of these stratal units in detail on outcrop has led to the further division into numerous parasequences. These parasequences often contain distinct, mappable genetically related packages of beds which are clearly not b
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Gardner, Michael H., Timothy A. Cross, and Mark Levorsen. "Stacking Patterns, Sediment Volume Partitioning, and Facies Differentiation in Shallow-Marine and Coastal-Plain Strata of the Cretaceous Ferron Sandstone, Utah." In Regional to Wellbore Analog for Fluvial-Deltaic Reservoir Modeling. American Association of Petroleum Geologists, 2004. https://doi.org/10.1306/st50983c5.

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Abstract Fluvial-deltaic strata of the Upper Cretaceous Ferron Sandstone, Western Interior Seaway, form a clastic wedge consisting of eight short-term stratigraphic cycles. The cycles are arranged consecutively in a seaward-stepping, vertically stacked, and landward-stepping stacking pattern. The stacking pattern is a product of fluctuations in accommodation-to-sediment supply (A/S) regimes described by intermediate-term, base-level cycles. Each short-term stratigraphic cycle is a progradational/aggradational unit comprising a spectrum of coastal-plain, bay/lagoon/estuary, shoreface, and shelf
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"delta distributary." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_40958.

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Bianchi, Thomas S. "The Ever-Changing Delta." In Deltas and Humans. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780199764174.003.0007.

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After his visit to Egypt in the year 500 B.C.E., Herodotus compared the triangular shape of the lowland region, where the Nile and sea meet, to the Greek letter Δ, thereby introducing the term delta to the geographic literature. In Chapter 1, we defined a delta as “a discrete shoreline protuberance formed where a river enters an ocean or lake … a broadly lobate shape in plain view narrowing in the direction of the feeding river, and a significant proportion of the deposit … derived from the river.” Coastal deltas are geologic structures that are also subcomponents of an estuary, which is commo
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Conference papers on the topic "Deltaic Distributary"

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Dutu, Florin, Laura Dutu, Irina Catianis, and Gabriel Iordache. "MORPHOLOGY AND WATER DYNAMICS OF CHANNEL BIFURCATION IN DELTAIC ENVIRONMENT." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/1.1/s01.003.

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The study presents a detailed analyse of the morpho-dynamic processes of the main two bifurcations of the Danube River within its delta, at Ceatal Izmail and Ceatal St. George. The first bifurcation of the Danube, called Ceatal Izmail; here the river divides into two distributaries: a northern one, the Chilia (Kilia), and a southern one, the Tulcea. Forking to the right at Ceatal Izmail (Mile 43), the Tulcea distributary stretches further to 17 km to the second main hydrographic knot Ceatal Sfantu Gheorghe (St. George) at Mile 33.84 (km 62.2). Here, the Tulcea branch divides into two main dist
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Espinoza, Savanna, and Aaron Yoshinobu. "DELTAIC DISTRIBUTARY CHANNELS AND LOBES IN THE PERMO-TRIASSIC QUARTERMASTER FORMATION, WEST TEXAS; PALEOCURRENT ANALYSIS AND DEPOSITIONAL EVIDENCE." In GSA Connects 2024 Meeting in Anaheim, California. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024am-401410.

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"Depositional Environment Based on Palynological and Foraminiferous Analysis of The Klasaman Formation in The Salawati Basin Klayili Area Klayili District Sorong Regency West Papua Province." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-sg-114.

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The Salawati Basin, West Papua is a mature basin producing oil. One of these basins was filled by sediments from the Klasaman Formation consisting of shale, claystone, sandstone, especially in the northern part there are conglomerates, rarely coral reef limestone deposited in a deltaic to fluvial environment. An a analysis of the depositional environment in the Klasaman Formation provides knowledge on the facies development and depositional environment in the study area. The study was carried out by using the surface geological data such as measured stratigraphy section (MS) with approaches of
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Mahanti, G., M. Al Kalbani, S. Lawati, S. Kindi, A. Al-ghaithi, and A. L. Ryba. "Revitalizing the Oldest Well in a South Oman Field Using Hydraulic Fracturing: A Case Study." In SPE International Hydraulic Fracturing Technology Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/215665-ms.

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Abstract Siliciclastic Ghariff reservoirs in Southern Oman fields are prolific reservoirs of fluvio-deltaic origin. These reservoirs are classified into Upper, Middle and Lower Ghariff sands depending on the geological environment of deposition. These reservoirs are developed via an initial primary depletion phase followed by secondary recovery techniques of water flood (Al Kalbani, Al Barwani, et al., 2023). One aspect of the field's development history is that the most promising reservoirs; the middle and upper parts of Lower Ghariff were given the highest drilling and development priority.
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Wu, Ivan Zhia, Sarvagya Parashar, Banu Andhika, et al. "Sand Body Trend Delineation Decrypting from Stratigraphic Dip Pattern Analysis: Case Study within a Fluvio-Deltaic Setting, East Kalimantan, Indonesia." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21466-ms.

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Abstract During field development, a detailed understanding of reservoir geometry and associated sedimentary features within the sand sequence plays an important role in the effective recovery of hydrocarbon resources. Most aging fields encounter the common problem in well placement for effective production of the remaining hydrocarbon resources. The current example—onshore formation from Late Miocene in East Kalimantan—includes seismic data acquired during the 1970s and 1980s. Considering advancements and breakthroughs provided by current technology, the older information could provide a grea
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Pojar, Iulian, Bogdan Ispas, Laura Dutu, Andrei Briceag, and Florin Dutu. "SEDIMENTOLOGICAL INVESTIGATIONS ON ST. GEORGE DISTRIBUTARY, DANUBE DELTA, ROMANIA." In 21st SGEM International Multidisciplinary Scientific GeoConference Proceedings 2021. STEF92 Technology, 2021. http://dx.doi.org/10.5593/sgem2021/1.1/s01.017.

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Zallum, Ibrahim, and Diane Kamola. "DIFFERENTIATING BETWEEN TIDAL CHANNELS, DISTRIBUTARY CHANNELS AND INCISED VALLEYS IN TIDAL DELTAS." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-381950.

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Akbi, H., S. Aidarbayev, M. Qiu, and A. Al-Wadi. "Static and Dynamic Reservoir Rock Typing of Highly Heterogeneous Fluvial Delta Marine Sands Deposited in Mesopotamian Basin." In ADIPEC. SPE, 2024. http://dx.doi.org/10.2118/222526-ms.

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Abstract Geological reservoir study is a crucial step to understand the reservoir properties that drive hydrocarbon flow behavior as part of reservoir life cycle. Among them, sandstone reservoirs have a lot of challenges when the data is scarce to integrate and link between the different disciplines. Nevertheless, a collaboration between geologists and petrophysicists paved a way to systematically fill data gaps which resulted in understanding of petrophysical distributions and the degree of heterogeneity. The methodology starts with a principal component analysis of logs to identify useful da
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Cui, Yunjiang, Hongbing Chen, Bo Liu, Gang Wei, and Yehong Cao. "Innovative Reservoir Quality Delineation in Conglomeratic Fan Delta Sedimentary Facies Using Integrated LWD Technology and Core Data, Bohai Bay, Eastern China." In SPE Conference at Oman Petroleum & Energy Show. SPE, 2025. https://doi.org/10.2118/225129-ms.

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Abstract Sedimentary facies play an important role in controlling reservoir distribution, connectivity, and quality. Insufficient understanding of the controlling effect of sedimentary facies on reservoir quality is quite common in field development stage, and lack of subsequent geological analysis makes the oil recovery under expectation. The target CFD6-4 field in Bohai Bay basin is developed in a fan delta setting and the formation comprises stacked, multi-layered conglomerates and sandstones with rapid vertical variation. Continuous identification and characterization of sedimentary facies
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Dutu, Laura, Florin Dutu, Gabriela Vlad, Iulian Pojar, and Naliana Lupascu. "SUSPENDED SEDIMENT CONCENTRATIONS AND FLUXES OF A MEANDERING SYSTEM, THE ST. GEORGE DISTRIBUTARY,DANUBE DELTA." In 21st SGEM International Multidisciplinary Scientific GeoConference Proceedings 2021. STEF92 Technology, 2021. http://dx.doi.org/10.5593/sgem2021/3.1/s12.42.

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