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Journal articles on the topic 'Deltaic'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Silva, Vinicius De Amorim, Luca Lämmle, and Archimedes Perez Filho. "Alterações no baixo curso do rio Jequitinhonha e seus impactos geomorfológicos no delta: o caso da Usina Hidrelétrica de Itapebi, Bahia, Brasil." Revista Brasileira de Geografia Física 14, no. 5 (2021): 2840. http://dx.doi.org/10.26848/rbgf.v14.5.p2840-2850.

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O objetivo deste trabalho é demonstrar as alterações na morfologia deltaica e no baixo curso do rio Jequitinhonha a partir da implementação barragem da Usina Hidrelétrica de Itapebi (UHI), analisando a evolução da dinâmica fluvial no baixo curso e morfologia deltaica antes e após a construção da barragem. As alterações antropogênicas na morfologia destes subsistemas permitiram interpretar dinâmicas que o rio Jequitinhonha está submetido em seu baixo curso. A caracterização, identificação e análise no delta, além do padrão de drenagem no canal principal, permitiram a investigação dos seguintes

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2

Korotayev, V. N. "ESTUARY-DELTAIC SYSTEMS." Geomorphology RAS, no. 3 (June 30, 2015): 54. http://dx.doi.org/10.15356/0435-4281-2008-3-54-65.

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3

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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Ogneva, Olga, Gesine Mollenhauer, Bennet Juhls, et al. "Particulate organic matter in the Lena River and its delta: from the permafrost catchment to the Arctic Ocean." Biogeosciences 20, no. 7 (2023): 1423–41. http://dx.doi.org/10.5194/bg-20-1423-2023.

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Abstract. Rapid Arctic warming accelerates permafrost thaw, causing an additional release of terrestrial organic matter (OM) into rivers and, ultimately, after transport via deltas and estuaries, to the Arctic Ocean nearshore. The majority of our understanding of nearshore OM dynamics and fate has been developed from freshwater rivers despite the likely impact of highly dynamic estuarine and deltaic environments on the transformation, storage, and age of OM delivered to coastal waters. Here, we studied particulate organic carbon (POC) dynamics in the Lena River delta and compared them with POC

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Ganguly, J., and B. K. Banerjee. "Halloysite in Deltaic Alluvium." Transactions of the Indian Ceramic Society 45, no. 4 (1986): 100. http://dx.doi.org/10.1080/0371750x.1986.10822799.

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6

Gouw, M. J. P., and G. Erkens. "Architecture of the Holocene Rhine-Meuse delta (the Netherlands) - A result of changing external controls." Netherlands Journal of Geosciences - Geologie en Mijnbouw 86, no. 1 (2007): 23–54. http://dx.doi.org/10.1017/s0016774600021302.

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AbstractThe Holocene Rhine-Meuse delta is formed under the influence of sea-level rise, tectonics, and variations in discharge and sediment supply. This paper aims to determine the relative importance of these external controls to improve our understanding of the evolution of the Rhine-Meuse fluvio-deltaic system. To do this, the geological and lithological composition of the fluvio-deltaic wedge has to be known in detail, both in space and time. This study presents five cross-valley sections in the Holocene Rhine-Meuse delta, based on almost 2000 shallow borings. Over 130 14C dates provide de

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Farooqui, Anjum, T. Karuna Karudu, D. Rajasekhara Reddy, and Ravi Mishra. "Organic matter depositional microenvironment in deltaic channel deposits of Mahanadi river, Andhra Pradesh." Journal of Applied and Natural Science 1, no. 2 (2009): 180–90. http://dx.doi.org/10.31018/jans.v1i2.58.

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Quantitative and qualitative variations in microscopic plant organic matter assemblages and its preservation state in deltaic channel deposits of Mahanadi River was correlated with the depositional environment in the ecosystem in order to prepare a modern analogue for use in palaeoenvironment studies. For this, palynological and palynofacies study was carried out in 57 surface sediment samples from Birupa river System, Kathjodi-Debi River system and Kuakhai River System constituting Upper, Middle and Lower Deltaic part of Mahanadi river. Theapex of the delta shows dominance of Spirogyra algae

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Krina, Anastasia, Fotios Xystrakis, Kostas Karantininis, and Nikos Koutsias. "Monitoring and Projecting Land Use/Land Cover Changes of Eleven Large Deltaic Areas in Greece from 1945 Onwards." Remote Sensing 12, no. 8 (2020): 1241. http://dx.doi.org/10.3390/rs12081241.

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Wetlands are areas of high biodiversity and provide many ecosystem services of high value. However, they are under constant threat from intense anthropogenic pressures, mainly agriculture intensification, urbanization, pollution, and climate change. The temporal and spatial patterns of land use/land cover (LULC) changes within eleven large wetlands in Greece were analyzed based on thematic maps generated from aerial orthophotos taken in 1945, 1975, and 2007. Socio-economic developments and the consequent need for more arable land and utilization of water resources are among the factors that ma

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9

Syaifuddin, Muhammad. "Organic Geochemical Characteristic Of Crude Oils From Orange Graben, South Sumatra Basin." Journal of Geoscience, Engineering, Environment, and Technology 1, no. 1 (2016): 25. http://dx.doi.org/10.24273/jgeet.2016.11.3.

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Lemat Formation in the Orange Graben in the South Sumatra basin has been considered as syn-rift sediments consist of fluvio-lacustrine sediments, create source rock with fluvio-lacustrine characterize. Based on existing publications, showing that the oils from Orange Graben have fluvio-deltaic characterization and generated by source rock from Talangakar Formation with fluvio-deltaic depositional environment. This paper emphasizes geochemistry methods. Source rock analysis, consist of 26 samples for carbon isotope and 14 samples for biomarker, while oil analysis, consist of 15 samples fo

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10

Zagare, Verónica, and Diego Andres Sepulveda Carmona. "Delta Challenges under Nature-Based Solutions Perspectives." Journal of Delta Urbanism, no. 3 (October 8, 2022): 4–7. https://doi.org/10.59490/jdu.3.2022.7294.

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Deltaic areas and coasts tend to be extremely vulnerable as aresult of the fusion of high-density urban agglomerations,overexploitation, and degradation of natural resources and theincrease of climate events. The complexity of the combination ofnatural coastal and deltaic processes and human-madeactivities requires an integral perspective regarding planning,design, and governance (Meyer, 2009; Zagare, 2018).

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11

Nienhuis, Jaap H., Andrew D. Ashton, and Liviu Giosan. "Littoral steering of deltaic channels." Earth and Planetary Science Letters 453 (November 2016): 204–14. http://dx.doi.org/10.1016/j.epsl.2016.08.018.

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12

Dyke, Arthur S., and John V. Matthews. "Stratigraphy and Paleoecology of Quaternary Sediments Along Pasley River, Boothia Peninsula, Central Canadian Arctic." Géographie physique et Quaternaire 41, no. 3 (2007): 323–44. http://dx.doi.org/10.7202/032689ar.

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ABSTRACT Quaternary sediments exposed along Pasley River consist of a lower marine deltaic sand overlain in succession by complexly interbedded tills and glaciomarine sediments (the lower glacigenic assemblage), by a mid-section fluvial gravel, by an upper marine deltaic sand, and by glaciomarine sediment and till (the upper glacigenic assemblage). The midsection fluvial gravels contain plant and insect fossils indicating a climate as warm as and perhaps warmer than present. The top of the gravel is more than 55 000 years old ; the unit is probably of Sangamonian age (>75 000 ka) and separa

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Rohmana, Rian Cahya, Iqbal Fardiansyah, Leon Taufani, and Dicky Harishidayat. "DEPOSITIONAL PROCESSES AND FACIES ARCHITECTURE OF BALIKPAPAN SANDSTONE FORMATION, APPLICATION OF 3D DIGITAL OUTCORP MODEL (DOM) TO IDENTIFY RESERVOIR GEOMETRY AND DISTRIBUTION IN DELTAIC SYSTEM." Scientific Contributions Oil and Gas 42, no. 1 (2020): 35–42. http://dx.doi.org/10.29017/scog.42.1.379.

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In recent years, digitalization of the outcrop technique is a powerful tool - for detailed analysis on the geo-software. Thus, the integration between outcrops and subsurface data for reducing the subsurface uncertainties. This provides the impetus to propose and accomplish a holistic understanding of the architecture and geometry of the deltaic system and to provide an exhaustive analysis of their sedimentary processes. This study investigates the temporal and spatial distribution of deltaic sandstone using a combination of 3D Digital Outcrop Model (DOM) application and traditional geologic m

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Shtyrkova, Yelena I., and Yelena I. Polyakova. "Fossil diatoms from the Volga Delta Holocene sediments (Damchik region) as indicators of the paleoecological conditions of sedimentation." Issues of modern algology (Вопросы современной альгологии), no. 2(20) (2019): 270–73. http://dx.doi.org/10.33624/2311-0147-2019-2(20)-270-273.

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The results of fossil diatoms investigation from the deltaic sediments are presented. Samples were obtained from the core DM-1 and two Holocene outcrops from the Damchik region of the Astrakhan Nature Reserve. In the core samples eight periods of sedimentation based on diatom analysis were identified: the sediments formed in shallow freshwater basins and deltaic channels. The samples from the outcrops were investigated in much greater detail.

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Wang, Zhanghua, Hao Xu, Qing Zhan, et al. "Lithological and Palynological Evidence of late Quaternary Depositional Environments in the Subaqueous Yangtze Delta, China." Quaternary Research 73, no. 3 (2010): 550–62. http://dx.doi.org/10.1016/j.yqres.2009.11.001.

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AMS 14C ages of post-glacial core sediments from the subaqueous Yangtze delta, along with sedimentary structures and distributions of grain size, pollen spores, and dinoflagellate cysts, show an estuarine depositional system from 13 to 8.4 cal ka BP and a deltaic system from 5.9 cal ka BP to the present. The estuarine system consists of intertidal to subtidal flat, estuarine, and estuarine-front facies, characterized by sand"mud couplets and a high sedimentation rate. The deltaic system includes nearshore shelf and prodelta mud featured by lower sedimentation rate, markedly fewer coastal wetla

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Zelilidis, Abraham, and Nikolaos Kontopoulos. "Pliocene–Pleistocene fluvial/wave-dominated deltaic sedimentation: the Pamisos delta, southwest Peloponnesus, Greece." Geological Magazine 131, no. 5 (1994): 653–68. http://dx.doi.org/10.1017/s0016756800012449.

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AbstractA fluvial /wave-dominated delta was formed during late Pliocene times in southwestPeloponnesus, influenced by NNW—SSE and ENE—WSW trending faults. The depositional patternremained unchanged through early Pleistocene times, when the pre-existing active faults with WNW—ESE extension were combined with an eastward asymmetrical subsidence of the graben. Inthe deltaic environment, marshes, lakes and lagoons were created in the western parts, whereas largequantities of sediments were deposited in the central and eastern parts adjacent to basin marginsof steeper relief.This study combines gra

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MacLaurin, Catherine I., J. Brian Mahoney, James W. Haggart, J. Russell Goodin, and Peter S. Mustard. "The Jackass Mountain Group of south-central British Columbia: depositional setting and evolution of an Early Cretaceous deltaic complex1This article is one of a series of papers published in this Special Issue on the theme of New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia.2Earth Science Sector (ESS) Contribution 20100280." Canadian Journal of Earth Sciences 48, no. 6 (2011): 930–51. http://dx.doi.org/10.1139/e11-035.

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The Lower Cretaceous Jackass Mountain Group of southwestern British Columbia records a complex history of deltaic and proximal marine sedimentation in a tectonically active area of the Canadian Cordillera. Two Jackass Mountain Group successions, exposed in the Camelsfoot Range and Chilko Lake regions and separated by ∼125 km across the northwest–southeast-trending Yalakom fault, provide details of stratigraphy, sedimentology, petrography, and geochemistry of the group. Restoring dextral movement across the Yalakom fault indicates that these locales were adjacent to one another during depositio

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18

Ganguly, Dipnarayan, Anirban Mukhopadhyay, Rahul Krishna Pandey, and Debasish Mitra. "Geomorphological study of sundarban deltaic estuary." Journal of the Indian Society of Remote Sensing 34, no. 4 (2006): 431–35. http://dx.doi.org/10.1007/bf02990928.

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19

Islam, Muhaiminul, and Hasan Muntasir. "Tropicality of Colonial Heritage Buildings in a Deltaic Landscape: British Colonial Architecture in Khulna." eTropic: electronic journal of studies in the tropics 19, no. 2 (2020): 72–96. http://dx.doi.org/10.25120/etropic.19.2.2020.3762.

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During the 17th-18th century colonial period on the Indian subcontinent, British colonial architecture flourished – including in the Bengal Delta. Although colonial architecture was inherently different from the traditional architecture of this tropical region, the monsoon climate and deltaic landscape forced colonial style buildings to incorporate a number of tropical architectural features to ensure climatic comfort. In the contemporary period, due to pressure from population density, many colonial buildings have been demolished and replaced with multi-story buildings. However, the tropical

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Meselhe, Ehab, Kazi Sadid, and Ashok Khadka. "Sediment Distribution, Retention and Morphodynamic Analysis of a River-Dominated Deltaic System." Water 13, no. 10 (2021): 1341. http://dx.doi.org/10.3390/w13101341.

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River deltas have received considerable attention due to coastal land loss issues caused by subsidence, storms, and sea level rise. Improved understanding of deltaic processes and dynamics is vital to coastal restoration efforts. This paper describes the application of process-based morphodynamic models to a prograding river delta. The analysis focuses on the flow and sediment dynamics amongst the interconnected channel network of the delta. The models were validated against observations of velocity and sediment concentrations for the Wax Lake Delta (WLD) of the Atchafalaya River system in Lou

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21

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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Marquis, Robert, and P. Stephen Kumarapeli. "An Early Cambrian deltaic–fluvial model for an Iapetan rift-arm drainage system, southeastern Quebec." Canadian Journal of Earth Sciences 30, no. 6 (1993): 1254–61. http://dx.doi.org/10.1139/e93-107.

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Based on the model that during the rifting stage beginning at ca. 590 Ma, the Ottawa Graben, an Iapetan failed arm, localized a large river that flowed into the nascent Iapetus, a search was made for the related fluvial and deltaic deposits. The search led to the identification of fluvial deposits as predicted by the model. Deltaic deposits were also identified despite complications brought about by deformation, metamorphism, and thrusting, although they probably belong to a late phase of delta buildup in the Early Cambrian. Older deltaic deposits of the river probably lie buried beneath a vol

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Abdullah, Md Sadaf, Sara Nowreen, Rashed Uz Zzaman, Sakib Hasnat, Susmita Majumder Satu, and Md Enayet Chowdhury. "Urbanising Delta: What Lessons Dhaka Offers to Face Challenges." Journal of Policy & Governance 01, no. 02 (2021): 1–21. http://dx.doi.org/10.33002/jpg010201.

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Cities built on deltaic regions are always prone to environmental risks like aggravated flooding, wetland reduction, compromised water quality, continuing water scarcity, and tainted air and these have been remarkable as the challenges while urbanizing deltas. On top of that, rapid urbanization adds more to the deterioration of ecosystem functions. Drawing insights from Bangladesh's capital Dhaka lying in the Ganges, Brahmaputra, and Meghna basin, this study basically appraises the common concerns of deltaic megapolises through a systematic literature review. The current literature has been br

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CONSTANTINESCU, Ștefan, and Mihnea TĂNĂSESCU. "Simplifying a deltaic labyrinth: anthropogenic imprint on river deltas." Revista de Geomorfologie 20, no. 1 (2018): 66–78. http://dx.doi.org/10.21094/rg.2018.023.

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The information contained by historical maps provides a good source of understanding the complex transformation of a deltaic environment by human activity. Using the Danube delta as an example, here we show that a artographic diagnosis for river deltas is based on four main steps that outline the learning stages for every similar area: 1) exploring coasts (for the early stages of the portolan and Ptolemaic maps); 2) exploring depths (for the succeeding imperial and military maps which focused on the access along the deltaic distributaries); 3) exploring deltaic networks (when economic and ecol

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Joseph, Jaquilin K., and Satish J. Patel. "Facies characterisation of a shallow-water deltaic succession: the Upper Jurassic Wagad Sandstone Formation of Kachchh, western India." Geologos 24, no. 2 (2018): 137–50. http://dx.doi.org/10.2478/logos-2018-0013.

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Abstract Ancient deltaic facies are difficult to differentiate from tidally influenced shallow-marine facies. The Wagad Sandstone Formation of the Wagad Highland (eastern Kachchh Basin) is typified by offshore and deltaic facies with sedimentary characteristics that represent different conditions of hydrodynamics and related depositional processes. The study area, the Adhoi Anticline, constitutes a ~154-m-thick, shale-dominated sequence with progressive upward intercalations of bioturbated micritic sandstone and quartz arenite. Two thick Astarte beds (sandy allochemic limestone), with an erosi

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Hakro, Asghar A. A. D., Aijaz Ali Halepoto, Muhammad Soomar Samtio, et al. "THE COMPARATIVE DEPOSITIONAL HETEROGENEITY OF MANCHHAR FORMATION (SIWALIK GROUP), SOUTHERN INDUS BASIN, PAKISTAN." Journal of Mountain Area Research 9 (January 13, 2024): 1. http://dx.doi.org/10.53874/jmar.v9i0.177.

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Present study is carried out for detailed description, distribution and interpretation of lithofacies and textural analysis of Manchhar Formation from Gaj River, Manchhar Lake and Lal Bagh Sections of Southern Indus Basin Pakistan. Four different clastic lithofacies are identified during present study, which are conglomeratic sandstone (Gt), shale (Fm), fine to coarse grain flat bedded sandstone (Sh) and fine to coarse grain trough cross-bedded sandstone (St). These Facies suggest that Manchhar Formation is deposited in the Beach to shallow agitated water and fluvial system. Twenty-nine (29) u

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Rey, Tony, David Lefevre, and Claude Vella. "Deltaic plain development and environmental changes in the Petite Camargue, Rhone Delta, France, in the past 2000 years." Quaternary Research 71, no. 3 (2009): 284–94. http://dx.doi.org/10.1016/j.yqres.2008.10.007.

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AbstractThe deltaic plain of the Petite Camargue which constitutes the western part of the Rhone Delta, began its main progradation around 2000 yr ago. Several delta lobes follow each other and have participated in the deltaic evolution. The deltaic lobes have distinct morphologies which reflect the dynamic fluvial and marine processes under the influence of climatic and human controls. Two delta lobe systems were built by the Daladel and Peccaïs channels, after which a deflected wave-influenced delta lobe was formed by the La Ville and Saint-Roman channels. The latest channel, the Rhone Vif c

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28

Md., Sadaf Abdullah, Nowreen Sara, Uz Zzaman Rashed, Hasnat Sakib, Majumder Satu Susmita, and Enayet Chowdhury Md. "Urbanising Delta: What Lessons Dhaka Offers to Face Challenges." Urbanising Delta: What Lessons Dhaka Offers to Face Challenges 01, no. 02 (2021): 21. https://doi.org/10.33002/jpg010201.

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Cities built on deltaic regions are always prone to environmental risks like aggravated flooding, wetland reduction, compromised water quality, continuing water scarcity, and tainted air and these have been remarkable as the challenges while urbanizing deltas. On top of that, rapid urbanization adds more to the deterioration of ecosystem functions. Drawing insights from Bangladesh's capital Dhaka lying in the Ganges, Brahmaputra, and Meghna basin, this study basically appraises the common concerns of deltaic megapolises through a systematic literature review. The current literature has bee

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Lebedev, Miсhael, Alena Khramtsova, Alexander Vilesov, Marcos Paulo G. Souza, and Аloysio Netto. "New data on depositional environment of Jurua Formation terminal sediments, Solimoes Basin, Brazil." Georesursy 21, no. 3 (2019): 2–13. http://dx.doi.org/10.18599/grs.2019.3.2-13.

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It has been for the first time established on the core taken from two wells that JR10 reservoir sediments (Upper Jurua, Formation Carboniferous) were deposited in the conditions of deltaic and alluvial coast with semiarid climate and in marine-terrigenous settings. JR10 reservoir differs in its lithological composition and structural architecture from the underlying layers of the Jurua formation and the overlying Carauari formation by the absence of carbonate and sulphate rocks and significant content of carbonaceous terrestrial plant fossils. The change of thickness from the south-east to nor

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Wallet, Bradley C., and Oswaldo Davogustto. "Integrating phase into the visualization of spectral decomposition attributes." Interpretation 3, no. 3 (2015): SS73—SS86. http://dx.doi.org/10.1190/int-2014-0281.1.

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Much of the world’s conventional oil and gas production comes from fluvial-deltaic reservoirs. The ability to accurately interpret the architectural elements comprising these systems greatly reduces the risk in exploration and development in these environments. We have evaluated methods for using spectral decomposition attributes to improve the visualization in fluvial-deltaic environments using data from the Middle Pennsylvanian age Red Fork Formation of Oklahoma. We determined how spectral phase and magnitude attributes can be effectively combined using an hue-saturation-value color map to p

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Hulscher, Suzanne J. M. H., Jord J. Warmink, and Bas W. Borsje. "Resilient Flood Defenses." Journal of Marine Science and Engineering 9, no. 4 (2021): 371. http://dx.doi.org/10.3390/jmse9040371.

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32

Selley, R. C. "Deltaic reservoir prediction from rotational dipmeter patterns." Geological Society, London, Special Publications 41, no. 1 (1989): 89–95. http://dx.doi.org/10.1144/gsl.sp.1989.041.01.08.

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Scott, A. C. "Deltaic coals: an ecological and palaeobotanical perspective." Geological Society, London, Special Publications 41, no. 1 (1989): 309–16. http://dx.doi.org/10.1144/gsl.sp.1989.041.01.21.

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Toonen, Willem. "Advances and prospects in deltaic palaeoflood hydrology." Quaternary International 279-280 (November 2012): 496. http://dx.doi.org/10.1016/j.quaint.2012.08.1694.

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NITTROUER, C. A., S. A. KUEHL, D. J. DEMASTER, and R. O. KOWSMANN. "The deltaic nature of Amazon shelf sedimentation." Geological Society of America Bulletin 97, no. 4 (1986): 444. http://dx.doi.org/10.1130/0016-7606(1986)97<444:tdnoas>2.0.co;2.

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SWENSON, J. B., V. R. VOLLER, C. PAOLA, G. PARKER, and J. G. MARR. "Fluvio-deltaic sedimentation: A generalized Stefan problem." European Journal of Applied Mathematics 11, no. 5 (2000): 433–52. http://dx.doi.org/10.1017/s0956792500004198.

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We present a model of sedimentation in a subsiding fluvio-deltaic basin with steady sediment supply and unsteady base level. We demonstrate that mass transfer in a fluvio-deltaic basin is analogous to heat transfer in a generalized Stefan problem, where the basin's shoreline represents the phase front. We obtain a numerical solution to the governing equations for sediment transport and deposition in this system via an extension of a deforming-grid technique from the phase-change literature. Through modification of the heat-balance integral method, we also develop a semi-analytical solution, wh

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McManus, John. "Deltaic responses to changes in river regimes." Marine Chemistry 79, no. 3-4 (2002): 155–70. http://dx.doi.org/10.1016/s0304-4203(02)00061-0.

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Pillon, P., L. Jocteur-Monrozier, C. Gonzalez, and A. Saliot. "Organic geochemistry of Recent equatorial deltaic sediments." Organic Geochemistry 10, no. 4-6 (1986): 711–16. http://dx.doi.org/10.1016/s0146-6380(86)80007-9.

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Patruno, Stefano, Gary J. Hampson, and Christopher A.-L. Jackson. "Quantitative characterisation of deltaic and subaqueous clinoforms." Earth-Science Reviews 142 (March 2015): 79–119. http://dx.doi.org/10.1016/j.earscirev.2015.01.004.

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Hoogendoorn, Robert M., Irina Overeem, and Joep E. A. Storms. "Process-response modelling of fluvio-deltaic stratigraphy." Computers & Geosciences 34, no. 10 (2008): 1394–416. http://dx.doi.org/10.1016/j.cageo.2008.02.006.

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Plink‐Björklund, Piret. "Shallow‐water deltaic clinoforms and process regime." Basin Research 32, no. 2 (2020): 251–62. http://dx.doi.org/10.1111/bre.12384.

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Johnson, Thomas C., John D. Wells, and Christopher A. Scholz. "Deltaic sedimentation in a modern rift lake." Geological Society of America Bulletin 107, no. 7 (1995): 812. http://dx.doi.org/10.1130/0016-7606(1995)107<0812:dsiamr>2.3.co;2.

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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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JIPA, Dan C., Marius STOICA, Ion ANDREESCU, Alina FLOROIU, and Gabriela MAXIMOV. "Zanclean Gilbert-type fan deltas in the Turnu Severin area (Dacian Basin, Romania). A critical analysis." Geo-Eco-Marina No 17/2011 (December 31, 2011): 123–33. https://doi.org/10.5281/zenodo.56925.

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Abstract. The critical analysis of the Gura Văii – Turnu Severin – Izvoru Bârzii Gilbert-type deltas concentrated on the deltaic architecture and the age of the deltaic deposits, referring especially to the conglomeratic sediments considered the proximal foreset unit of the Gilbert-type fan deltas. It reveals the lack of evidences necessary to demonstrate the existence of the three units (foreset, bottomset and topset beds) which define a Gilbert-type delta. Although there are convincing data for its tectonic origin, the homoclinal structure of these deltaic deposits was cons

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Olsen, Henrik. "Coarsening upward sequences - the products of laterally established river subsystems, M. Devonian, Hornelen Basin, Norway." Bulletin of the Geological Society of Denmark 36 (December 31, 1987): 203–19. http://dx.doi.org/10.37570/bgsd-1988-36-03.

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Investigations of sedimentary sequences in a marginal part of Homelen Basin (M. Devonian, W Norway) have resulted in the interpretation of gradually established fluvial and fluviodeltaic subsystems adjacent to a major river system. A succession of 8 coarsening upward (CU) sequences (4.5---19 m thick) wad studied. Three sequence types are recognized: sequence type A, B and C. The lower part of all sequence types is composed of silty lacustrine flood basin deposits. The upper part of all sequence types is composed of sandy low sinuosity fluvial channel deposits. The middle part of the three sequ

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Paul, Ashis Kumar, and M. K. Bandyopadhyay. "Morphology of Sagar Island, A Part of Ganga Delta." Journal Geological Society of India 29, no. 4 (1987): 412–23. http://dx.doi.org/10.17491/jgsi/1987/290406.

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Abstract The deltaic morphology of Sagar island is controlled by the river Hugli to the north and the Bay of Bengal to the south. The seasonal (summer and winter) and diurnal (two high tides and two low tides) fluctuations of sea level and the Hugli discharge with a large amount of silt contribute to the formation of the largest island in Ganga delta. Deposition of sand, silt, clay and mud from south to north is also characteristic of this deltaic island. The 12 km shoreline and its sand ridges are deformed by wind and waves. Mangroves in the swamp, some halophytic plants on the sand dunes and

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Yubero, Maria Teresa, and E. Bonet. "Ground Surface Effect of Earth Pressure Balance Tunnelling in Deltaic Deposits: A Case Study of Line 9 of the Barcelona Metro." Sustainability 16, no. 18 (2024): 8275. http://dx.doi.org/10.3390/su16188275.

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The 47.8 km long Line 9 of the Barcelona Metro is one of Europe’s longest urban metro lines. Its southern section connects the city to the airport, being entirely excavated through soft deltaic deposits, promoting more sustainable mobility by reducing significant road traffic. This study identifies the most accurate method for predicting surface settlements caused by tunnel excavation using ground movement monitoring data. Several methodologies were assessed, with the Mean Absolute Error (MAE) and Mean Relative Error (MRE) calculated to evaluate their performances. The methods considered were

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Keim, Richard F., and J. Blake Amos. "Dendrochronological analysis of baldcypress (Taxodium distichum) responses to climate and contrasting flood regimes." Canadian Journal of Forest Research 42, no. 3 (2012): 423–36. http://dx.doi.org/10.1139/x2012-001.

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Baldcypress (Taxodium distichum (L.) Rich.) has been used extensively for dendrochronological reconstruction of climate and is a key species in globally important wetlands with complex, poorly understood relationships between hydrological and ecological processes. To better understand ecosystem responses to changing climate and hydrology and to test whether hydrological or climatological variables are most reflected in chronologies, we developed tree-ring chronologies for six stagnant or riverine swamps in the Mississippi River deltaic plain and modeled growth responses to historical hydrology

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Tang, Yongjie, Zhuo Zheng, Kangyou Huang, et al. "Holocene Evolution of the Pearl River Delta: Mapping Integral Isobaths and Delta Progradation." Journal of Marine Science and Engineering 11, no. 10 (2023): 1986. http://dx.doi.org/10.3390/jmse11101986.

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The Pearl River Delta (PRD, China) has undergone complex geological development within a multi-island faulted basin, shaped by the interplay of regional tectonic movements, Quaternary sea-level fluctuations, and fluvial-marine interactions. Despite a great number of studies on the Holocene sedimentary sequences and spatial differences of lithofacies and environments, scant attention has been paid to the overarching human influence on deltaic evolution and coastline modifications since the Neolithic epoch. To further elucidate the spatial variation in Holocene sedimentation and its underlying b

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Abiodun, O. Ogunjobi, Akinola Toyin, and Olawoki Muyiwa. "Integrated Exploration Studies in 40-year Mature Acreage: 2200 BOPD Production Reward." International Journal of Geology and Earth Sciences 4, no. 4 (2018): 83–96. https://doi.org/10.32937/IJGES.4.4.2018.83-96.

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The 40-year mature acreage is located in the Northern Delta Depobelt of the Tertiary Niger delta basin. Most of the easy-to-define structural play types and prospects have been tested. In order to optimize the opportunity and existing production facilities, new plays and deep exploration targets were defined. The application of sequence and seismic stratigraphy principles with biostratigraphic data, resulted in well-defined Lowstand (LST), Transgressive (TST) and Highstand (HST) packages, the related 40.1mya, 42.7mya, 44.4mya and 48mya Sequence Boundaries (SB) and their Environments of Deposit

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