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Relevant bibliographies by topics / Fluvial environments

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Academic literature on the topic 'Fluvial environments'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Fluvial environments"

1

Lee, Young-Hoon. "Three-Dimensional Simulation of Fluvial Environments." Geoinformatics 6, no. 2 (1995): 81–96. http://dx.doi.org/10.6010/geoinformatics1990.6.2_81.

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Wing, Scott L. "Depositional Environments of Plant Bearing Sediments." Paleontological Society Special Publications 3 (1988): 1–13. http://dx.doi.org/10.1017/s2475262200004858.

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Plants can become incorporated into the sediments of virtually any environment, from the oozes of abyssal plains to the silts and sands of delta fronts to brecciated mudflows of volcanic origin. However there is a much narrower range of sedimentary environments in which identifiable plant remains are found in abundance. Generally speaking these are the very shallow or subaerial portions of deltas and estuaries, the channels and floodplains of fluvial systems, lakes of all sizes, ash-falls, and mass-flow deposits such as mudflows. For the purposes of this paper peat swamps are considered as unusual subtypes of deltaic and fluvial environments in which clastic input is low relative to organic accumulation.

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Boechat Albernaz, Marcio, Lonneke Roelofs, Harm Jan Pierik, and Maarten G. Kleinhans. "Natural levee evolution in vegetated fluvial‐tidal environments." Earth Surface Processes and Landforms 45, no. 15 (2020): 3824–41. http://dx.doi.org/10.1002/esp.5003.

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Power, G., and M. Power. "Ecotones and fluvial regimes in arctic lotic environments." Hydrobiologia 303, no. 1-3 (1995): 111–24. http://dx.doi.org/10.1007/bf00034049.

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Bullard, Joanna E., and Grant H. McTainsh. "Aeolian-fluvial interactions in dryland environments: examples, concepts and Australia case study." Progress in Physical Geography: Earth and Environment 27, no. 4 (2003): 471–501. http://dx.doi.org/10.1191/0309133303pp386ra.

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Over the past 10 to 15 years there has been a rising interest in interactions between aeolian and fluvial processes from geomorphologists and sedimentologists. This reflects recognition of the limitations of a reductionist perspective examining single process systems in understanding landform and landscape development. This paper focuses on the rise of aeolian-fluvial interaction research in dryland environments. We first explore the background to the contemporary situation then review existing research on aeolian-fluvial interactions at global/regional and local scales. From this review it is suggested that landscape sensitivity, or the effectiveness of links between the process systems, spatial environmental transitions and temporal environmental change are the three main driving forces determining the geomorpho-logical significance of aeolian-fluvial interactions. The importance of the first two of these driving forces is explored in more detail using Australia as a case study. We conclude by highlighting some future possible research directions in this field.

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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 grain size parameters, total organic matter, carbonate and clay mineralogyand structural analysis to: (a) determine the pattern of sedimentation in sub-environments and (b)create a fluvial/wave-type deltaic depositional model, and distinguish between delta-plain, delta-front and pro-delta environments. The Pliocene-Pleistocene, fluvial/wave-dominated delta model inthis study can be used to predict deltaic sedimentation in analogous basins.

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Shaw, John. "Geomorphic Evidence of Postglacial Terrestrial Environments on Atlantic Canadian Continental Shelves." Géographie physique et Quaternaire 59, no. 2-3 (2007): 141–54. http://dx.doi.org/10.7202/014752ar.

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Abstract Changes in the geography of Atlantic Canada since the last glacial maximum (LGM) are grouped into three phases. The first phase (LGM – ca. 13 ka BP) commences with glaciers at the edge of the continental shelves, and ends with the glaciers having retreated to near modern coasts. In the second phase (ca. 13 ka BP‑10 ka BP), glaciers were mainly on land; on the continental shelves there were scattered small ice caps and an outer-shelf archipelago. Early in phase three, beginning ca. 10 ka BP, glaciers were largely absent, and the archipelago was gradually submerging; elsewhere, falling relative sea levels caused emergence. Multibeam sonar mapping has revealed the geomorphic evidence of submerged terrestrial environments of phases II and III, including fluvial, deltaic, and coastal systems. The best-preserved fluvial systems are in Northumberland Strait and the Bras d’Or Lakes. Elsewhere, multibeam bathymetric data allow discrimination between fluvial and non-fluvial channels. Deltas were mainly preserved in the special circumstances of Newfoundland fjords. Submerged coastal systems are common in the Bras d’Or Lakes, but rare elsewhere. Landscape preservation is ascribed to special circumstances. Paleogeographic reconstructions have applications in the field of evolutionary biology and archaeology.

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Hossain, Sushmita, Takashi Ishiyama, Shoichi Hachinohe, and Chiaki T. Oguchi. "Leaching Behavior of As, Pb, Ni, Fe, and Mn from Subsurface Marine and Nonmarine Depositional Environment in Central Kanto Plain, Japan." Geosciences 9, no. 10 (2019): 435. http://dx.doi.org/10.3390/geosciences9100435.

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The leaching behavior of arsenic (As), lead (Pb), nickel (Ni), iron (Fe), and manganese (Mn) was investigated from subsurface core sediment of marine and nonmarine depositional environments in central Kanto Plain, Japan. A four-step sequential extraction technique was adopted to determine the chemical speciation, potential mobility, and bioavailability of metals under natural conditions in variable depositional environments. In addition, a correlation of these properties with pore water and total metal content was carried out. The concentration of As in pore water was found to be 2–3 times higher than the permissible limit (10 µg/L) for drinking water and leachate in fluvial, transitional, and marine environments. The trend of potential mobile fractions of As, Pb, and Ni showed Fe–Mn oxide bound > carbonate bound > ion exchangeable bound > water soluble in the fluvial environment. However, in the marine environment, it showed Fe–Mn oxide bound > water soluble > carbonate bound > ion exchangeable bound for As. The leaching of As in this fluvial environment is due to the organic matter-mediated, reductive dissolution of Fe–Mn oxide bound, where Mn is the scavenger. The amount of total content of As and sulfur (S) in transitional sediment reflects an elevated level of leachate in pore water, which is controlled by S reduction. However, the leaching of As in marine sediment is controlled by pH and organic matter content.

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Badgley, Catherine. "Counting Individuals in Mammalian Fossil Assemblages from Fluvial Environments." PALAIOS 1, no. 3 (1986): 328. http://dx.doi.org/10.2307/3514695.

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Beevers, Lindsay, Ioana Popescu, Quan Pan, and Douglas Pender. "Applicability of a coastal morphodynamic model for fluvial environments." Environmental Modelling & Software 80 (June 2016): 83–99. http://dx.doi.org/10.1016/j.envsoft.2016.02.016.

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Dissertations / Theses on the topic "Fluvial environments"

1

Grashion, Anton R. "Computer aided analysis of ancient fluvial depositional environments." Thesis, Staffordshire University, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.241509.

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Newell, Andrew John. "Sedimentological controls on vertebrate taphonomy in Triassic fluvial environments." Thesis, Queen's University Belfast, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.317467.

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Dawson, Martin. "Late Devensian fluvial environments of the Lower Severn Basin, U.K." Thesis, University of Leicester, 1986. http://hdl.handle.net/2381/34480.

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Coarse grained, late-Devensian, fluvial deposits underlie river terraces along the lower River Severn and in tributary valleys. Borehole evidence indicates that individual terrace features may be correlated downstream, supporting previous stratigraphic interpretations. Examinations of the terrace sediments were carried out at 10 major sections enabling comparisons to be made between 'paraglacial' and 'periglacial' deposits. Interpretations of the depositional environments are based upon detailed descriptions of the sediments and considerations of genetic relationships between lithofacies types, determined through Markov chain and architectural element analyses. Five depositional sub-environments may be identified; channel zone units, overbank deposits, unitary channel forms, slope and alluvial fan deposits. The occurrence of the latter two sub-environments depends on the pre-existing valley topography, whilst the characteristics of the channel-zone and overbank deposits vary in relation to the local aggradation rate, discharge regime, proximal to distal controls on the sediment size distribution and channel slope. The fluvial sequences were predominantly deposited by low sinuosity gravel bed rivers, often with braided planforms. However, the Worcester Terrace aggraded partly under sandy braided conditions. Channel zone lithofacies in a modern braided river are shown to develop through the formation and agglomeration of complex lateral and medial bar forms. These comprise bar-platform units representing primary, in-channel (unit-bar), sedimentation, and supra-platform sediments which are superimposed on, and modify, the bar-platform deposition. Mean annual flood discharges in the basin, and possible error limits, are estimated using palaeohydraulic and morphometric techniques. Palaeodischarges in the Severn and Avon are shown to have been similar, with maxima occurring during deglaciation. Avon discharges may have been up to 25 times present values, although in the lower Severn mean annual floods may only have reached 4 times present. The development and preservation of Pleistocene terrace deposits is considered within a model emphasizing differences apparent in the sedimentary sequences. A similar model explains the development of channel zone depositional features, and the origins of gravel stratification types are discussed in relation to observations of terrace and modern sediments.

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Crimes, Angela C. "Modelling of thin bed sands in fluvial-deltaic environments of the Southern Cooper Basin, South Australia /." Title page, abstract and contents only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbc929.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, National Centre for Petroleum Geology and Geophysics, 1996?<br>Volume 2 is boxed and consists of 1 folded map and 9 folded correlations. Includes bibliographical references (leaves 39-40).

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Lee, Mui-fa Alison, and 李梅花. "Sedimentary facies of fluvial-marine transition environments in Hong Kong: Ting Kok and Pak Nai Deltas." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31221270.

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Lee, Mui-fa Alison. "Sedimentary facies of fluvial-marine transition environments in Hong Kong : Ting Kok and Pak Nai Deltas /." Hong Kong : University of Hong Kong, 1999. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21021211.

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Calvani, Giulio [Verfasser], Hans Matthias [Akademischer Betreuer] Schöniger, and Luca [Akademischer Betreuer] Solari. "Riparian vegetation in fluvial environments : linking timescales through flow uprooting / Giulio Calvani ; Hans Matthias Schöniger, Luca Solari." Braunschweig : Technische Universität Braunschweig, 2021. http://d-nb.info/1225038294/34.

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Workman, Terry W. "PALEOWETLANDS AND FLUVIAL GEOMORPHOLOGY OF QUEBRADA MANI: RECONSTRUCTING PALEO-ENVIRONMENTS AND HUMAN OCCUPATION IN THE NORTHERN ATACAMA DESERT." Miami University / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=miami1345055481.

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Sousa, Eliete dos Santos. "Fluxo evasivo de CO2 em ambientes fluviais no sudoeste da Amazônia, Acre, Brasil." Universidade de São Paulo, 2013. http://www.teses.usp.br/teses/disponiveis/64/64135/tde-04092013-142901/.

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Na maior bacia hidrográfica do Planeta, o rio Amazonas transporta para os oceanos grande quantidade de carbono particulado e dissolvido. Esta visão tradicional dos rios, como carreadores de carbono para os oceanos, tem sido revista nas últimas décadas, em função de novos resultados que mostram emissões de CO2 destes sistemas para atmosfera superiores ao transporte na descarga em até uma ordem de grandeza. Diversos trabalhos já foram realizados com o objetivo de avaliar os processos que controlam essas emissões. No entanto, os mesmos ainda permanecem como uma grande fonte de incertezas. O objetivo principal deste trabalho foi quantificar os fluxos de CO2 em rios e igarapés do sudoeste da Amazônia (bacia do rio Purus, estado do Acre), levando em consideração as características químicas e físicas de cada sistema, bem como a sazonalidade da região e, assim, contribuir para melhorar as estimativas das emissões de carbono em toda a bacia Amazônica. Os resultados mostraram que durante o período de estiagem os rios apresentam águas com concentrações relativamente elevadas de bicarbonato, indicando a importância do intemperismo de carbonatos como fonte de carbono. Análises da composição isotópica do carbono inorgânico dissolvido corroboraram estes resultados. Nos igarapés, no entanto, a principal fonte de carbono é a matéria orgânica do solo. A sazonalidade exerce forte influência na pCO2 e, consequentemente, nos fluxos de CO2, com os maiores valores ocorrendo no período chuvoso. No entanto, não foi encontrada variabilidade sazonal nas taxas respiratórias o que mostra que, além da respiração, outros fatores também estão influenciando os fluxos de CO2. No período seco, o aumento significativo das concentrações de clorofila a pode indicar que processos fotossintéticos também desempenham um papel importante no balanço de C destes sistemas<br>In the largest basin of the planet, the Amazon river carries large amounts of particulate and dissolved carbon to the oceans. This traditional view of rivers as carriers of carbon to the oceans has been reviewed in the last decades due to new results showing that CO2 emissions to the atmosphere from these systems can surpass C transport in discharge in one order of magnitude. Several studies have been conducted to evaluate the processes controlling these emissions. However they still remain a major source of uncertainty. The main objective of this study was to quantify CO2 evasive fluxes in rivers and streams of Southwestern Amazon (Purus river basin, Acre state), taking into account chemical and physical characteristics of each system, as well as seasonality in this region and, thus, contribute to improve estimates of carbon emissions throughout the Amazon basin. The results showed that during low water the rivers have relatively high bicarbonate concentrations, indicating that carbonate weathering is an important carbon source. Dissolved inorganic carbon isotopic composition corroborated these results. However, in streams the main carbon source is soil organic matter. Seasonality has a strong influence on pCO2 and consequently on CO2 fluxes, with the highest values occurring in the rainy season. However there was no seasonal variability in respiration rates, which shows that other factors than respiration are also influencing CO2 fluxes. During the dry period, increases in chlorophyll a indicate that photosynthetic processes also play an important role in the C balance of these systems.

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Bartz, Melanie [Verfasser], Helmut [Gutachter] Brückner, and Olaf [Gutachter] Bubenzer. "Quaternary fluvial environments in NE Morocco inferred from geochronological and sedimentological investigations / Melanie Bartz ; Gutachter: Helmut Brückner, Olaf Bubenzer." Köln : Universitäts- und Stadtbibliothek Köln, 2017. http://d-nb.info/1151298247/34.

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Books on the topic "Fluvial environments"

1

Maccaferri. Maccaferri: For the restoration and draining of fluvial environments. River & Sea Gabions Ltd, 1995.

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McLaurin, Brett T. Reconstructing Human-Landscape Interactions - Volume 1: Interpreting Desert and Fluvial Environments. Springer Berlin Heidelberg, 2012.

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G, Brown A., and Quine T. A, eds. Fluvial processes and environmental change. J. Wiley, 1999.

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Rowiński, Paweł, and Artur Radecki-Pawlik, eds. Rivers – Physical, Fluvial and Environmental Processes. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-17719-9.

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International, Conference on Monitoring Simulation Prevention and Remediation of Dense and Debris Flows (2nd 2008 New Forest England). Monitoring, simulation, prevention and remediation of dense debris flows II. WIT, 2008.

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International Conference on Monitoring, Simulation, Prevention and Remediation of Dense and Debris Flows (3rd 2010 Milan, Italy). Monitoring, simulation, prevention and remediation of dense and debris flows III. WIT Press, 2010.

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International Conference on Monitoring, Simulation, Prevention, and Remediation of Dense and Debris Flows (4th 2012 Milan, Italy). Monitoring, simulation, prevention, and remediation of dense and debris flows IV. Edited by De Wrachien D. editor, Brebbia C. A. editor, and Mambretti S. editor. WIT Press, 2012.

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Beever, Erik. Integrated monitoring of hydrogeomorphic, vegetative, and edaphic conditions in riparian ecosystems of Great Basin National Park, Nevada. U.S. Geological Survey, 2004.

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Beever, Erik. Integrated monitoring of hydrogeomorphic, vegetative, and edaphic conditions in riparian ecosystems of Great Basin National Park, Nevada. U.S. Geological Survey, 2004.

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Wiejaczka, Łukasz. Wpływ zbiornika wodnego "Klimkówka" na abiotyczne elementy środowiska przyrodniczego w dolinie Ropy: Influence of the Klimkówka water reservoir on the abiotic elements of the natural environment in the Ropa River valley. PAN IGiPZ, 2011.

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Book chapters on the topic "Fluvial environments"

1

Evans, James E. "Fluvial Environments." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73568-9_129.

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Pavlopoulos, Kosmas, Niki Evelpidou, and Andreas Vassilopoulos. "Fluvial Environments." In Mapping Geomorphological Environments. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-01950-0_2.

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Evans, James E. "Fluvial Environments." In Selective Neck Dissection for Oral Cancer. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-12127-7_129-1.

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Fonstad, Mark J. "Hyperspectral Imagery in Fluvial Environments." In Fluvial Remote Sensing for Science and Management. John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781119940791.ch4.

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Carbonneau, Patrice E., Hervé Piégay, Jérôme Lejot, Robert Dunford, and Kristell Michel. "Hyperspatial Imagery in Riverine Environments." In Fluvial Remote Sensing for Science and Management. John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781119940791.ch8.

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Bailly, Jean-Stéphane, Paul J. Kinzel, Tristan Allouis, Denis Feurer, and Yann Le Coarer. "Airborne LiDAR Methods Applied to Riverine Environments." In Fluvial Remote Sensing for Science and Management. John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781119940791.ch7.

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Power, G., and M. Power. "Ecotones and fluvial regimes in arctic lotic environments." In The Importance of Aquatic-Terrestrial Ecotones for Freshwater Fish. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-017-3360-1_11.

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Benda, Lee. "Confluence Environments at the Scale of River Networks." In River Confluences, Tributaries and the Fluvial Network. John Wiley & Sons, Ltd, 2008. http://dx.doi.org/10.1002/9780470760383.ch13.

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Johnson, Peter G. "Proglacial and Paraglacial Fluvial and Lacustrine Environments in Transition." In Landscapes of Transition. Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-017-2037-3_3.

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O’Farrell, Inés. "Comparative analysis of the phytoplankton of fifteen lowland fluvial systems of the River Plate Basin (Argentina)." In Phytoplankton in Turbid Environments: Rivers and Shallow Lakes. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-017-2670-2_10.

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Conference papers on the topic "Fluvial environments"

1

Maue, Anthony D., Devon M. Burr, Joseph S. Levy, and Erica Nathan. "LINKING COBBLE-RICH FLUVIAL ENVIRONMENTS ON EARTH AND TITAN." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324423.

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Ramirez, Antonio, Maria Morant, and Roberto Llorente. "Underwater Optical Network for Remote Sensing Applications in Fluvial Environments." In 2019 21st International Conference on Transparent Optical Networks (ICTON). IEEE, 2019. http://dx.doi.org/10.1109/icton.2019.8840564.

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Draége, Anders. "Modelling of seismic properties during diagenesis in fluvial depositional environments." In SEG Technical Program Expanded Abstracts 2005. Society of Exploration Geophysicists, 2005. http://dx.doi.org/10.1190/1.2147983.

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Smith, P. E., S. Dunn-Norman, and M. B. Smith. "A Methodology for Statistical Propped Fracture Treatment Design in Fluvial Environments." In SPE Hydraulic Fracturing Technology Conference. Society of Petroleum Engineers, 2014. http://dx.doi.org/10.2118/168595-ms.

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Zulkifli, Nur Azah, Lisa Claire Chisholm, Amy Mawarni M Yusoff, Nur Khairina Kosnon, Mohd Zubair Mohd Azkah, and Mohd Amri M Diah. "Defining Heterogeneity and Compartmentalisation Predictions of Minor Reservoirs in Fluvial Environments: Geological and Dynamic Context." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21225-ms.

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Abstract Reservoirs in MN Field comprise predominantly fluvial delta deposits. A number of reservoir modeling studies have been performed for major reservoirs, however, there are still challenges to be addressed. After 20 plus years of production, a project for minor reservoirs has been crafted based on the understanding and challenges of major reservoirs. The primary objective of this study was to improve the understanding of the uncertainties impacting the well performance and reservoir connectivity; and to find potential infill opportunities. A 2D conceptual modelling approach was used as a practical way to incorporate the static and dynamic data of logs, core, seismic and pressure data. Taking the lessons learned from the major reservoir performances, this study focused on the fluvial reservoir sedimentology to address and decrease the uncertainties through the different scales of heterogeneity. Consequently, depositional facies maps were developed with the integration of geophysical study and interpretation derived from seismic analysis. These integrated depositional facies maps were then further refined with the well production data and scenarios of multiple compartments from multiple iterations to fit into the conceptual models of this field. Refined paleo depositional maps for these minor reservoirs allowed for a better understanding on reservoir heterogeneities and further improved the geological understanding. This fundamental study can show us a more precise distribution and tendency of the sand and the scales of heterogeneity with different depositional facies. However, capturing and preserving the different levels of heterogeneities and compartmentalization is complex for some thin sand reservoirs which are below seismic resolution and have low correlation of reservoir properties-seismic response. Additionally, multiple compartments were inferred due to pressure difference and multiple contacts within a reservoir. This was further complicated by the uncertainty in log interpretation due to inadequacy of high confidence data (DST/fluid sampling), suppressed resistivity from shaly sands and below log resolution of thin beds. Despite of these issues and challenges, with integration of all the data available and rigorous team discussions; the minor reservoirs depo-facies, static and dynamic compartmentalization were finalized, leading to enhancement of reservoir prediction, communication and quality.

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Cuba, Patricia Helena, Jennifer Lynne Miskimins, Donna Schmidt Anderson, and Mary Carr. "Impacts of Diverse Fluvial Depositional Environments on Hydraulic Fracture Growth in Tight Gas Reservoirs." In SPE Hydraulic Fracturing Technology Conference. Society of Petroleum Engineers, 2011. http://dx.doi.org/10.2118/140413-ms.

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Baade, Jussi, and Christiane Schmullius. "High-resolution mapping of fluvial landform change in arid environments using terrasar-X images." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5652020.

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Gatewood, Michael, Maurice P. Testa, and Christopher Knubley. "AN ANALOG COMPARISON BETWEEN THE PAHRUMP HILLS, GALE CRATER, MARS TO VOLCANOGENIC FLUVIAL-LACUSTRINE ENVIRONMENTS IN ICELAND." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327537.

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Buatois, Luis A., Maria Gabriela Mangano, Davinia Díez-Canseco, Euridice Solorzano, and Williams Rodriguez. "ICHNOLOGIC DELINEATION OF THE FLUVIAL-TIDAL TRANSITION AND ITS SIGNIFICANCE FOR FACIES MODELLING OF MARGINAL-MARINE ENVIRONMENTS." In Rocky Mountain Section - 69th Annual Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017rm-293164.

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Gou, Bo, Yan Deng, Jianchun Guo, Cong Lu, Ting Yu, and Xingwen Wang. "3D Fracturing Design With Consideration of the Diverse Fluvial Depositional Environments and Flow Units in Tight Gas Reservoirs." In SPE/IATMI Asia Pacific Oil & Gas Conference and Exhibition. Society of Petroleum Engineers, 2015. http://dx.doi.org/10.2118/176294-ms.

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