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Journal articles on the topic 'Sedimentary'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

ANDRÉ, Jefferson Lima Fernandes, Luiza Alves GARCIA, Lucas Dias SANTIAGO, and Aurélio Fagundes SILVA. "FÁCIES SEDIMENTARES DAS ROCHAS AFLORANTES NO NORTE DO ESTADO ESPÍRITO SANTO, PORÇÃO ONSHORE DA BACIA SEDIMENTAR DO ESPÍRITO SANTO." Geosciences = Geociências 43, no. 4 (2024): 497–514. https://doi.org/10.5016/geociencias.v43i4.18373.

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RESUMO - No presente estudo pretende-se contribuir sobre a compreensão geológica da porção onshore Bacia Sedimentar do Espírito Santo, onde há poucos estudos publicados. Identificaram-se fácies sedimentares de maior ocorrência como fácies rudáceas, areníticas e lamíticas, com cores branca a cinza claro, formando depósitos tabulares com gradação normal e interacamadados. Estratificações acanaladas incipientes foram observadas, assim como feições de acresção lateral, escavação e preenchimento de canais. As fácies areníticas e rudáceas são mal selecionadas, matriz-suportadas, constituídas princip

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2

Yue, Shao Fei, De Tian Yan, Xiao Peng Li, and Guang Zeng Song. "The Characteristics of Sedimentary Facies of Tanzhuang Formation of Upper Triassic of Luoyi District." Advanced Materials Research 868 (December 2013): 7–10. http://dx.doi.org/10.4028/www.scientific.net/amr.868.7.

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Based on the observation and description of single well and outcrops and the analysis of reservoir compositions, petrology, clastic structure and sedimentary structure,this paper determines the sedimentaty facies characteristics of Tanzhuang formation. The types of sedimentary facies in late Triassic epoch are delta front,shallow lake and semi-deep lake. The delta front develops subaqueous distributary channel, mouth bar and distal bar. Lacustrine facies develops shallow lake mud, shallow lake sand bar, turbidite sand and semi-deep lake mud.The reservoir rock formations in this area are lithic

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3

Otavio, Jonatas Malaquias, Osvaldo Girão, Tiago Fernando de Holanda, and Wenderson Sávyo Aguiar Da Silva. "FORMAÇÃO E DIAGÊNESE DE ARENITOS DE PRAIA: Uma Revisão Conceitual." CLIO – Arqueológica 32, no. 3 (2017): 88. http://dx.doi.org/10.20891/clio.v32n3p88-106.

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Os arenitos de praia, ou beachrocks, são sedimentos que sofreram um processo de litificação e são encontrados paralelamente à linha de costa na zona intermaré, apresentando uma forma alongada, estreita e cimentados por carbonato de cálcio. O processo de diagênese consiste na formação da rocha sedimentar propriamente dita a partir da compactação, dissolução, cimentação e recristalização. O estudo da formação e diagênese do arenito de praia são relevantes pois possibilita o entendimento de como as rochas sedimentares detríticas são geradas, além de reconhecer como a variação do nível do mar se c

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4

Holanda, Werlem, Anderson Costa dos Santos, Camila Cardoso Nogueira, et al. "EFFECTS OF IGNEOUS INTRUSION ON THE MINERALOGICAL CONTENT OF IRATI FORMATION, PARANÁ BASIN, IN SAPOPEMA (PR), SOUTHERN BRAZIL." Journal of Sedimentary Environments 4, no. 3 (2019): 350–60. http://dx.doi.org/10.12957/jse.2019.45796.

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Igneous intrusions in sedimentary basins are commonly related with mineralogical association changes in host-rock. At Sapopema region (Paraná State, southern Brazil), an extensive diabase sill (associated to Serra Geral Formation) was emplaced in pelitic-carbonate succession during post-Triassic. The sedimentary host-rock association includes mostly shale, siltstone and carbonate of the Permian Irati Formation. X-ray diffraction (XRD), scanning electron microscopy (SEM) and energy dispersive spectroscopy (EDS) data revealed that heat transfer was not enough to cause modifications in mineral as

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5

Pinto de Almeida, Maria Victória Ferreira, Antonio Rodrigues Ximenes Neto, Francisco José Maciel de Moura, Francisco Oricélio Da Silva Brindeiro, and José Ramon Vasconcelos Cavalcante. "CARACTERIZAÇÃO SEDIMENTAR DA PLANÍCIE LITORÂNEA DA PRAIA DO IGUAPE, AQUIRAZ-CE." Revista da Casa da Geografia de Sobral (RCGS) 21, no. 2 (2019): 936–47. http://dx.doi.org/10.35701/rcgs.v21n2.502.

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Este trabalho teve como objetivo a caracterização dos aspectos sedimentares da planície costeira da praia do Iguape através da análise de dados estatísticos, levando em consideração, também os impactos socioambientais decorrentes do uso e ocupação. A área de estudo se encontra em Aquiraz, Região Metropolitana de Fortaleza (RMF). Historicamente o município começou a se evidenciar após a integração do município na RMF em 1973, onde passou a se destacar devido ao turismo. A faixa de praia do município possui aproximadamente 29 km de extensão, onde se encontram as praias do Batoque, Barro Preto, I

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6

SANDY, MICHAEL R. "Sedimentary microrhythms." Nature 318, no. 6041 (1985): 81. http://dx.doi.org/10.1038/318081a0.

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7

Tankard, Anthony J. "Sedimentary Petrology." Sedimentary Geology 152, no. 1-2 (2002): 159–60. http://dx.doi.org/10.1016/s0037-0738(01)00254-8.

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8

Föllmi, Karl B. "Sedimentary condensation." Earth-Science Reviews 152 (January 2016): 143–80. http://dx.doi.org/10.1016/j.earscirev.2015.11.016.

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9

Rickard, David, Marc Mussmann, and Jeffrey A. Steadman. "Sedimentary Sulfides." Elements 13, no. 2 (2017): 117–22. http://dx.doi.org/10.2113/gselements.13.2.117.

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10

Postma, George. "Sedimentary basins." Earth-Science Reviews 34, no. 4 (1993): 276–77. http://dx.doi.org/10.1016/0012-8252(93)90064-e.

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11

Postma, George. "Sedimentary petrology." Sedimentary Geology 84, no. 1-4 (1993): 249. http://dx.doi.org/10.1016/0037-0738(93)90064-c.

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12

Morad, Sadoon. "Sedimentary petrography." Sedimentary Geology 92, no. 3-4 (1994): 292–94. http://dx.doi.org/10.1016/0037-0738(94)90114-7.

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13

Zhang, Lei, Bing Dai, Xue Juan Zhang, and Xiao Dong Yi. "The Analysis of Sedimentary System and Provenance of Saertu Reservoir in Jiangqiao-Pingyang Area in Northern of Songliao Basin." Advanced Materials Research 734-737 (August 2013): 194–98. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.194.

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Through the studying of heavy mineral assemblages and ZTR index variation features, this paper analyses the provenances and sedimentary systems of Saertu reservoir in Cretaceous of Jiangqiao-Pingyang area, western slope zone in northern of Songliao basin. It is concluded that there are three major sedimentary systems in the Saertu reservoir depositional period, named the Nehe-Yian sedimentary system in Northeast, Yingtai sedimentary system in Southwest, Qiqihaer sedimentary system in Northwest. The intensity and influence scope of the sedimentary systems in sedimentary period of SaII+III, SaIa

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14

Xiang, Jianbo, Xianghui Zhang, Jiale Liu, Qinghao Meng, Yu Zhang, and Xinglu Li. "Characterization and Modernization of the Depositional System in Modern Ebinur Lake Basin, Northwest China." Applied Sciences 14, no. 11 (2024): 4425. http://dx.doi.org/10.3390/app14114425.

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The Ebinur Lake Basin is a typical terrestrial sedimentary Basin in Northwest China that has developed a piedmont distributive fluvial system (DFS) sedimentary environment, lake sedimentary environment, and desert sedimentary environment. The Ebinur Lake receives the sediments carried by the rivers in the basin and is the regional sedimentary center. In this study, a division scheme of modern sedimentary system tracts in the Ebinur Lake Basin was proposed. According to the landform, sedimentary environment, structure, and sedimentary system types, the Ebinur Lake Basin was divided into five sy

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15

Yu, Sheng Yun, Qing Yun Meng, and Hai Ying Xu. "Study of the Fluvial Facies Reservoir Sedimentary Characteristics of an Oil Field in China." Advanced Materials Research 753-755 (August 2013): 66–69. http://dx.doi.org/10.4028/www.scientific.net/amr.753-755.66.

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In this paper, 6 kinds of reservoir sedimentary microfacies distribution model-conceptual model have been established by the use of reservoir sedimentology theory and methods, namely, large sandy braided river sand body sedimentary model, large meandering river sand body sedimentary model, low bending-straight distributary channel sedimentary model, crevasse splay (crevasse river) sedimentary model, heart beach sedimentary model, flood plain and distributary plain sheet sand body sedimentary model. On this basis, the sedimentary facies figures of four sedimentary units have been painted, putti

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16

Crook, Keith A. W. "Sedimentary geology: An introduction to sedimentary rocks and stratigraphy." Sedimentary Geology 107, no. 3-4 (1997): 304–6. http://dx.doi.org/10.1016/s0037-0738(97)84049-3.

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17

Morin, Guillaume, Thierry Allard, Etienne Balan, Philippe Ildefonse, and Georges Calas. "Native Cd+ in sedimentary fluorapatite." European Journal of Mineralogy 14, no. 6 (2002): 1087–94. http://dx.doi.org/10.1127/0935-1221/2002/0014-1087.

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18

Wei, Jiangwei, Fawang Li, Shikuo Zhang, Hanlie Cheng, Qiang Qin, and David Cadasse. "Characteristics of Sedimentary Microfacies of Late Triassic Yanchang Formation in North-Central Ordos Basin." Journal of Chemistry 2022 (September 22, 2022): 1–10. http://dx.doi.org/10.1155/2022/1513503.

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Sedimentary microfacies refer to the smallest unit with unique rock structure, structure, thickness, rhythm, and other sedimentary characteristics and certain plane configuration rules in the subfacies zone. Sedimentary microfacies research is the most basic sedimentary unit formed in the same or basically the same sedimentary background. Sedimentary microfacies marks are the key to the division of sedimentary microfacies. If we cannot find effective marks, we cannot correctly divide sedimentary microfacies. These marks are mainly obtained from detailed observation of cores. On the premise of

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19

Motoki, Akihisa, Luiz Carlos Chaves Novais, Kenji Freire Motoki, Leonardo Costa de Oliveira, Ricardo De Souza Fasolo, and Adrienne Brito Lima. "SATELLITE-DERIVED GRAVIMETRY FOR ABROLHOS CONTINENTAL SHELF, STATES OF ESPÍRITO SANTO AND BAHIA, BRAZIL, AND ITS RELATION TO TECTONIC GENESIS OF SEDIMENTARY BASINS." Revista Brasileira de Geofísica 32, no. 4 (2014): 735. http://dx.doi.org/10.22564/rbgf.v32i4.554.

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ABSTRACT. This paper presents the results of satellite-derived gravimetry for Abrolhos Continental Shelf and the adjacent areas, States of Esp´ırito Santo and Bahia,Brazil, and discusses tectonic genesis of the sedimentary basins. The free-air and Bouguer anomalies on the continental shelf show a gradual increase from coast tocontinental shelf break. The total difference of 135 mGal indicates crust thinning of 4.5 km. The Bouguer anomaly increases beyond the shelf break and continues upto the abyssal plane. The total difference of 260 mGal suggests crustal thinning of 9.0 km. The studied area

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20

Zhiguo, Wang. "Study on sedimentary facies characteristics of Xujiahe Formation in Sichuan Basin." E3S Web of Conferences 290 (2021): 02022. http://dx.doi.org/10.1051/e3sconf/202129002022.

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Sedimentary facies is the summation of all primary sedimentary features in a sedimentary unit, which is the product of sedimentation in a specific environment. It emphasizes the material performance of sediment formation conditions, including mineralogy, petrology, paleontology, geochemistry and geophysics. Therefore, it has unique sedimentary features in this environment. In this paper, the types and units of sedimentary facies which can reflect the basic characteristics and geometry of sedimentary system are established, and based on the comprehensive analysis of rock types, lithological ass

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21

Kuznetsov, V. G. "L. V. Pustovalov and the establishment of sedimentary research in Russia." Proceedings of higher educational establishments. Geology and Exploration, no. 2 (June 21, 2023): 92–99. http://dx.doi.org/10.32454/0016-7762-2023-65-2-92-99.

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This article is dedicated to the role of L.V. Pustovalov in creating the theoretical foundations of sedimentary research in Russia, including determination and substantiation of the most important regularities governing sedimentary processes and their stages. The constituting stages of sedimentary processes, such as weathering, transport, and deposition, were identified and described. These stages lead to the differentiation of sedimentary material and the formation of sedimentary rocks of different composition and structure. The concepts of the stages of diagenesis and epigenesist (catagenesi

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22

Friedman, Barry, and Scott B. Smith. "The Sedimentary Constitution." University of Pennsylvania Law Review 147, no. 1 (1998): 1. http://dx.doi.org/10.2307/3312757.

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23

Dunne, Sean, Michael Longley, Maurice Hayes, and Ken Bloomfield. "Volcanic and Sedimentary." Irish Review (1986-), no. 16 (1994): 133. http://dx.doi.org/10.2307/29735763.

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24

Korotayev, V. N. "SEDIMENTARY MOUTH SYSTEMS." Geomorphology RAS, no. 4 (July 23, 2015): 12. http://dx.doi.org/10.15356/0435-4281-2012-4-12-21.

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25

Clemmey, H. "Sedimentary ore deposits." Geological Society, London, Special Publications 18, no. 1 (1985): 229–47. http://dx.doi.org/10.1144/gsl.sp.1985.018.01.11.

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26

Haughton, P. D. W., S. P. Todd, and A. C. Morton. "Sedimentary provenance studies." Geological Society, London, Special Publications 57, no. 1 (1991): 1–11. http://dx.doi.org/10.1144/gsl.sp.1991.057.01.01.

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27

Gluyas, J. "Sedimentary facies analysis." Marine and Petroleum Geology 13, no. 7 (1996): 856–57. http://dx.doi.org/10.1016/0264-8172(96)83696-8.

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28

Elderfield, H. "Glacial sedimentary environments." Marine Geology 76 (January 1987): 334. http://dx.doi.org/10.1016/0025-3227(87)90043-0.

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29

Seminara, G. "Fluvial Sedimentary Patterns." Annual Review of Fluid Mechanics 42, no. 1 (2010): 43–66. http://dx.doi.org/10.1146/annurev-fluid-121108-145612.

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30

Rieber, Alfred J. "The Sedimentary Society." Russian History 16, no. 1 (1989): 353–76. http://dx.doi.org/10.1163/187633189x00176.

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AbstractThe great historian V. O. Kliuchevskii found the key to Russian society in the relative simplicity of its social forms in comparison with Western Europe. But in writing his magisterial Course in Russian History he revealed a degree of complexity that belied his disarming formula. The apparent contradiction stems from the standard of comparison. There were elements of complexity in Russian society that had no counterparts in the experience of the West. Moreover, the definition of society in nineteenth-century social history may have been too confining. If we make the effort to explore t

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31

Alderson, Danielle M., Martin G. Evans, James J. Rothwell, and Stephen Boult. "Classifying sedimentary organics:." Progress in Physical Geography: Earth and Environment 40, no. 3 (2016): 450–79. http://dx.doi.org/10.1177/0309133315625864.

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Sediments are crucial to the understanding of environmental processes and conditions in a variety of systems. The study of sediments often focuses on quantity, but should involve more emphasis on the quality of the organic component, by utilising commonplace techniques employed by other disciplines. We provide a classification scheme that will allow those interested in organic matter quality to decide on appropriate techniques to apply, and discuss a variety of applications of the investigation of organic matter quality in diverse areas of Physical Geography. Firstly, this paper conceptualises

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32

Klein, George de V. "Chinese sedimentary basins." Earth-Science Reviews 32, no. 3 (1992): 187–88. http://dx.doi.org/10.1016/0012-8252(92)90025-o.

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33

Young, Grant M. "Chinese sedimentary basins." Sedimentary Geology 72, no. 1-2 (1991): 165–67. http://dx.doi.org/10.1016/0037-0738(91)90132-w.

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34

Fielding, C. R. "Sedimentary facies analysis." Sedimentary Geology 105, no. 1-2 (1996): 105. http://dx.doi.org/10.1016/0037-0738(95)00114-x.

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35

Roberts, D. G. "Sedimentary basins of the world. volume 1: Chinese sedimentary basins." Marine and Petroleum Geology 9, no. 1 (1992): 111. http://dx.doi.org/10.1016/0264-8172(92)90015-7.

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36

Merriman, Richard J. "Clay minerals and sedimentary basin history." European Journal of Mineralogy 17, no. 1 (2005): 7–20. http://dx.doi.org/10.1127/0935-1221/2005/0017-0007.

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37

Vignoles, Philippe, Gilles Dreyfuss, and Daniel Rondelaud. "Decline in the number and size of populations of two Lymnaeidae living in central France over the last decade." International Journal of Limnology 58 (2022): 11. http://dx.doi.org/10.1051/limn/2022011.

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Field investigations in 2013–2014 on acid soils and in 2016–2017 on sedimentary soils showed that populations of two lymnaeids had decreased in number in central France since 1998. As several heat waves occurred in this region in 2018, 2019 and 2020, it was useful to check whether this decline had further increased in recent years. Surveys in 56 farms in the north-west and west of the Haute Vienne department (acid soils) and 37 farms in the south of Indre (sedimentary soils) were therefore carried out in 2020 and 2021 and the results obtained were compared with those recorded by our team in th

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38

Yang, Yepeng, Zaixing Jiang, Jianguo Zhang, Zongxuan Zhang, and Chun Yang. "Control Effect of Deposition Processes on Shale Lithofacies and Reservoirs Characteristics in the Eocene Shahejie Formation (Es4s), Dongying Depression, China." Energies 16, no. 5 (2023): 2200. http://dx.doi.org/10.3390/en16052200.

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The lacustrine fine-grained sedimentary rocks in the upper interval of the fourth member of the Eocene Shahejie Formation (Es4s) in the Dongying Depression are important shale oil exploration targets in Bohai Bay Basin. They are widely distributed and rich in organic matter. In this study, samples were observed under the optical microscope and FESEM, combined with geochemical test and physical property analysis to study the sedimentary characteristics and reservoir characteristics of them. Nine lithofacies are recognized based on the mineral composition, the content of organic matter and the b

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39

Sheng, Jun, Jincheng Liu, Qingshan Qi, et al. "Fine Characterization of Sand Body in the Front of the Fluvial Delta: Taking the VII Oil Group of N21 Reservoir in Gasikule Oilfield as an Example." Geofluids 2021 (February 9, 2021): 1–14. http://dx.doi.org/10.1155/2021/6671855.

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Taking the VII oil group of N21 reservoir in Gasikule Oilfield as an example, the sedimentary time unit was divided into the barrier layer, interbed, and sand bed by analyzing the sedimentary system and sand body development model in this paper. The single sand body was analyzed for the sand bed time unit. The residual muddy intercalation period division theory was proposed for the first time to divide the sedimentary periods of the sedimentary time unit of the sand bed. Finally, a new “sandwich” layer point coincidence modeling technology was proposed to characterize the sedimentary time unit

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40

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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41

Honegger, Belén Viera, Ethel Morales, Matias Soto, and Bruno Conti. "SEISMIC STRATIGRAPHY OF THE EOCENE–LOWER OLIGOCENE IN THE URUGUAYAN CONTINENTAL MARGIN / ESTRATIGRAFIA SÍSMICA DO EOCENO AO OLIGOCENO INFERIOR NA MARGEM CONTINENTAL URUGUAIA." Journal of Sedimentary Environments 3, no. 4 (2018): 290–306. http://dx.doi.org/10.12957/jse.2018.39248.

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The Uruguayan continental margin was generated following the fragmentation of the Gondwana supercontinent and the subsequent opening of South Atlantic Ocean. It constitutes an extensive sedimentation area in which three sedimentary basins can be found: the Punta del Este Basin, the southernmost portion of the Pelotas Basin, and the poorly defined Oriental del Plata Basin. The aim of this work was the identification and characterization of the different seismic units (seismic facies, systems tracts, depositional sequences) for the sedimentary interval assigned to the Eocene in the Uruguayan con

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42

Mueller, W., and J. A. Donaldson. "Development of sedimentary basins in the Archean Abitibi belt, Canada: an overview." Canadian Journal of Earth Sciences 29, no. 10 (1992): 2249–65. http://dx.doi.org/10.1139/e92-177.

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Sedimentation in the Archean Abitibi greenstone belt occurred during four depositional episodes: (i) sedimentary cycle 1, 2730–2720 Ma; (ii) sedimentary cycle 2, 2715–2705 Ma; (iii) sedimentary cycle 3, 2700–2687 Ma; and (iv) sedimentary cycle 4, 2685–2675 Ma. Records of the first two sedimentary cycles are preserved in basins within the northern volcanic zone, whereas basins formed during the latter two sedimentary cycles are located within the southern volcanic zone of the Abitibi belt. Sedimentary cycles 1 and 3 represent deep-water facies, as indicated by turbidites, resedimented conglomer

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43

Xiao, Bin, Jun Li, and Yu Hua Fan. "Analysis of Sedimentary Facies Model - The Cretaceous Bottom Conglomerate of Xinjiang Junggar Basinludong Area as an Example." Applied Mechanics and Materials 522-524 (February 2014): 1289–92. http://dx.doi.org/10.4028/www.scientific.net/amm.522-524.1289.

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This paper aims to Cretaceous bottom conglomerate facies of Xinjiang Ludong area of China research to elucidate the deposition pattern analysis phase, as well as the use of methods. Methods first take logging combined with tectonic pattern and sedimentary background, division comparing in Ludong area of Cretaceous basal conglomerate unit. Secondly, the application of modern sedimentology theory, method, system analysis of lithologic characteristics of this area and sedimentary structure feature. According to the logging facies analysis, summarized the various sedimentary facies marks, distingu

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44

Li, Huan, and Xiao-Shuang Xi. "Sedimentary fans: A new genetic model for sedimentary exhalative ore deposits." Ore Geology Reviews 65 (March 2015): 375–89. http://dx.doi.org/10.1016/j.oregeorev.2014.10.001.

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45

O'Brien, P. E. "Subglacial sedimentary features in Late Palaeozoic sedimentary rocks, central Victoria, Australia." Sedimentary Geology 61, no. 1-2 (1989): 1–15. http://dx.doi.org/10.1016/0037-0738(89)90038-9.

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46

KHALIFA-ZADEH, CH M., Z. JA EFENDIYEVA, N. G. VALIEV, and S. YA HAMASHAYEVA-MURADOVA. "COMPARATIVE ANALYSIS OF CATAGENESIS IN SCREEN CLAY ROCKS IN AINCIENT TRIAS-PALEOZOIC AND YOUNG LOWER PLIRCENE DEPOSITS OF SOUTH MANGISHLAK AND WESTERN BOART OF SOTHIN CASPIAN DEPRESSION." News of the Tula state university. Sciences of Earth 3, no. 1 (2023): 33–49. http://dx.doi.org/10.46689/2218-5194-2023-3-1-33-49.

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The event of catagenesisi in stratisfere is plays main role in alteration and formation of sedimentary rocks and sedimentary useful minerals. The first of all under subsidence sedimentary fasins and sedimentary rocks lost petrophysics puculdrity under oction of thermobar-ic factors. Rockformation minerals as quartz feldshpats an carbonate take plays is erosive and distructive and in same time in contrary direction is condacts transformation terrigenous and carbonate minerals to new minerals. Under catagenesis in the intensive catagenic processes determine role plays primery composition of sedi

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47

Pan, Xuemei. "Preliminary analysis of sedimentary characteristics and facies model of M-II layer in Kazakhstan Oilfield A." E3S Web of Conferences 352 (2022): 01041. http://dx.doi.org/10.1051/e3sconf/202235201041.

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The lithologic melange accumulation of areskum formation in akshabluk area is one of the key strata in exploration. Its basement inheritance controls the whole process of Jurassic sedimentation, and the filling and leveling gradually reduces the terrain elevation difference; After the late Jurassic deformation, the flat paleogeomorphology was changed and the deposition of Early Cretaceous strata was controlled. Under the control of marker beds, sedimentary cycles are divided according to the cycle characteristics of logging curves. Under the control of cycle interface (standard layer), accordi

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48

Zhang, Mingwang, and Kebin Shi. "Comprehensive analysis of water-sediment variation characteristics at the confluence of the upper reaches of the Weigan River and Heizi River with multiple methods and multiple influencing factors." Water Supply 22, no. 2 (2021): 1275–92. http://dx.doi.org/10.2166/ws.2021.354.

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Abstract In-depth analysis of the characteristics of water and sedimentary changes at the confluence of the upper reaches of Weigan River and Heizi River is the prerequisite and basis for studying the future water and sedimentary situation in the Kizil Reservoir. This article analyzes the trend, mutation point and periodicity of the water and sedimentary sequence with multi-methods. The double cumulative curve method and the attenuation analysis method were used to analyze the impact of precipitation and human activities on runoff and sedimentary transport, and other influencing factors were q

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49

Zhou, Chao, and Kunkun Li. "Review of Mixed Sedimentation Studies." International Journal of Energy 5, no. 3 (2024): 41–49. https://doi.org/10.54097/jwv2tt08.

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Since the 1950s, mixed sedimentation has come into people's attention, and has gradually become the research direction of sedimentology. On the basis of previous studies, the research progress of mixed deposition at home and abroad is summarized, and some problems and prospects of mixed deposition are put forward. Mixed sediment is widely developed in Marine and lake sedimentary environments. As a special sediment with complex sedimentary patterns, it is controlled by many factors such as terrigenous supply, climate change, sea level change, hydrodynamic conditions, tectonic action and so on.

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50

Wang, Yong Ping, Feng Jiao Wang, Hui Min Tang, and Wen Chao Jiang. "Sedimentary Facies Influence Oil Production with Grey Correlation Degree Method." Advanced Materials Research 868 (December 2013): 593–96. http://dx.doi.org/10.4028/www.scientific.net/amr.868.593.

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The sedimentary facies is the combination of the sediment which has some rules of lithological and construction characters and paleontological evidence. It characterizes the source direction and the strength degree of water dynamics. As the developmental situation of the reservoir of different sedimentary facies is different, the permeability, porosity and oil saturation is distinctive. The production is related to the sedimentary facies, this lead to the different production capacity of different sedimentary facies. The oil-producing capacity varies with the sedimentary facies of the reservoi

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