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Journal articles on the topic 'Sedimentary Geology'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 September 2024

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1

Ginsburg, Robert N. "Global Sedimentary Geology Program." PALAIOS 1, no. 5 (1986): 521. http://dx.doi.org/10.2307/3514636.

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2

Mizutani, Shinjiro. "On the sedimentary geology." Journal of the Sedimentological Society of Japan 77, no. 1 (2018): 3–15. http://dx.doi.org/10.4096/jssj.77.3.

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3

Jones, Brian, Jasper Knight, and Gert Jan Weltje. "Editorial for Sedimentary Geology." Sedimentary Geology 241, no. 1-4 (2011): 1–2. http://dx.doi.org/10.1016/j.sedgeo.2011.10.010.

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4

Ochoa, Carlos G., William Todd Jarvis, and Jesse Hall. "A Hydrogeologic Framework for Understanding Surface Water and Groundwater Interactions in a Watershed System in the Willamette Basin in Western Oregon, USA." Geosciences 12, no. 3 (2022): 109. http://dx.doi.org/10.3390/geosciences12030109.

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A broad understanding of local geology and hydrologic processes is important for effective water resources management. The objectives of this project were to characterize the hydrogeologic framework of the Oak Creek Watershed (OCW) geographical area and examine the connections between surface water and groundwater at selected locations along the main stem of Oak Creek. The OCW area comprises the Siletz River Volcanic (SRV) Formation in the upper portion of the watershed and sedimentary rock formations in the valley. Past hydrologic and geologic studies and our field measurement data were synth

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5

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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6

Elmouttie, M. K., G. Krähenbühl, G. V. Poropat, and I. Kelso. "Stochastic Representation of Sedimentary Geology." Rock Mechanics and Rock Engineering 47, no. 2 (2013): 507–18. http://dx.doi.org/10.1007/s00603-013-0411-x.

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7

ANDREWS, J. E., and A. E. FALLICK. "Stable isotopes in sedimentary geology." Journal of the Geological Society 143, no. 4 (1986): 721–22. http://dx.doi.org/10.1144/gsjgs.143.4.0721.

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8

Kreulen, Rob. "Stable isotopes in sedimentary geology." Sedimentary Geology 54, no. 4 (1988): 350–51. http://dx.doi.org/10.1016/0037-0738(88)90043-7.

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9

Crook, K. A. W., A. D. Miall, and B. W. Sellwood. "Sedimentary Geology: into the nineties." Sedimentary Geology 62, no. 1 (1989): 1–2. http://dx.doi.org/10.1016/0037-0738(89)90096-1.

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10

Martindale, Rowan C., Kathleen Benison, Christopher Jackson, and Brian Romans. "#SEPM - Sedimentary Geology in the Twitterverse." Sedimentary Record 17, no. 4 (2019): 10–12. http://dx.doi.org/10.2110/sedred.2019.4.10.

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11

Rice, Randy J. "Recent developments in Precambrian sedimentary geology." Canadian Journal of Earth Sciences 29, no. 12 (1992): 2521–22. http://dx.doi.org/10.1139/e92-198.

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12

MCKELVEY, V. E. "Phosphorus Deposits: Geology of Sedimentary Phosphates." Science 233, no. 4765 (1986): 796. http://dx.doi.org/10.1126/science.233.4765.796.

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13

Schlager, W. "The Future of Applied Sedimentary Geology." Journal of Sedimentary Research 70, no. 1 (2000): 2–9. http://dx.doi.org/10.1306/2dc408f8-0e47-11d7-8643000102c1865d.

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14

Liu, Cheng Zhi, and Hui Cui Sun. "Geological and Seismic Stratigraphy of Wangfu Sag." Advanced Materials Research 912-914 (April 2014): 1637–39. http://dx.doi.org/10.4028/www.scientific.net/amr.912-914.1637.

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By combining seismic with geology, we processing a detailed stratigraphic classification in the Wangfu depressed areas. In this way, targeting the geologic horizons and seismic horizons in the wells according to the synthetic seismic logs. We may gain an Corresponding Relation between seismic with geology. Then compare the stratigraphic division . From the point of evolutionary history of regional structure, geological information generated by tectonic movement was recorded, for example, plane of unconformity, sedimentary cycle, lithology, lithofacies, and their responds in the seismic profile

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15

Nainggolan, Tumpal Bernhard, Dida Kusnida, Eddy Mirnanda, Imam Setiadi, Erwin Haryanto Nugroho, and Subagio. "Delineating subbasins of sedimentary rock structure beneath eastern Central Sumatra Basin based on gravity model, seismic profiles, and well-log data: A case study." Leading Edge 43, no. 3 (2024): 176–84. http://dx.doi.org/10.1190/tle43030176.1.

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The Central Sumatra Basin is a vast sedimentary basin that has been proven to produce hydrocarbon. The basin comprises several subbasins that are not sufficiently imaged by conventional seismic reflection profiles and limited well-log data, particularly in the nearshore area to the east. This research aims to delineate sedimentary subbasins, interpret the subsurface geologic model, and identify geologic structures beneath the eastern part of the Central Sumatra Basin using integrated geophysical gravity, seismic profiles, and well-log data. Three-dimensional gravity inversion modeling results

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16

Russell, Richard J. "RECENT GEOLOGY OF COASTAL LOUISIANA." Coastal Engineering Proceedings 1, no. 2 (2000): 9. http://dx.doi.org/10.9753/icce.v2.9.

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Recent, in a technical geological sense, refers to the latest episode of geological time. Definitions vary. Northern European geologists are likely to refer to about the last 10,000 years for the reason that only the sedimentary deposits of such an interval are available for study. Geologists in the United States commonly regard the Recent as a post-glacial period of somewhat longer duration. Studies of materials containing the carbon isotope, C14, are resulting in time determinations in years. Louisiana geologists define Recent as that period of time during -which sea level made its last gene

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17

SNYDER, W. S. "Sedimentary Geology And Paleontology Research--A Perspective." PALAIOS 19, no. 3 (2004): 191–92. http://dx.doi.org/10.1669/0883-1351(2004)019<0191:sgaprp>2.0.co;2.

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18

Matthews, Rob. "The Role of Paradigms in Sedimentary Geology." PALAIOS 1, no. 5 (1986): 433. http://dx.doi.org/10.2307/3514627.

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19

Flessa, Karl W. "NSF Funding for Paleontology and Sedimentary Geology." PALAIOS 5, no. 5 (1990): 393. http://dx.doi.org/10.2307/3514833.

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20

SLOSS, L. L. "Sedimentary Geology: New Perspectives in Basin Analysis." Science 241, no. 4874 (1988): 1839–40. http://dx.doi.org/10.1126/science.241.4874.1839-a.

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21

Stokstad, E. "SEDIMENTARY GEOLOGY: Homegrown Quartz Muddies the Water." Science 289, no. 5484 (2000): 1449–51. http://dx.doi.org/10.1126/science.289.5484.1449.

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22

Mallet, Jean-Laurent. "Space–Time Mathematical Framework for Sedimentary Geology." Mathematical Geology 36, no. 1 (2004): 1–32. http://dx.doi.org/10.1023/b:matg.0000016228.75495.7c.

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23

Sherwood, Christopher R., and Joe S. Creager. "Sedimentary geology of the Columbia River Estuary." Progress in Oceanography 25, no. 1-4 (1990): 15–79. http://dx.doi.org/10.1016/0079-6611(90)90003-k.

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24

Pomar, L., and P. Hallock. "Carbonate factories: A conundrum in sedimentary geology." Earth-Science Reviews 87, no. 3-4 (2008): 134–69. http://dx.doi.org/10.1016/j.earscirev.2007.12.002.

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25

Magistrale, Harold, Keith McLaughlin, and Steven Day. "A geology-based 3D velocity model of the Los Angeles basin sediments." Bulletin of the Seismological Society of America 86, no. 4 (1996): 1161–66. http://dx.doi.org/10.1785/bssa0860041161.

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Abstract Seismic hazard studies of the Los Angeles basin area require a realistic seismic-velocity model. We use geologic information about depth to crystalline basement, depths to sedimentary horizons, uplift of sediments, and surface geology in a velocity-depth-age function to construct a three-dimensional velocity model. In earthquake location tests, the model predicts travel times satisfactorily, and in earthquake ground-motion simulations, the model correctly determines the timing and amplitude of late-arriving waves.

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26

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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27

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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28

Yang, Xiuwei, and Peimin Zhu. "Reservoir Prediction Under Control of Sedimentary Facies." Journal of Computational Acoustics 25, no. 03 (2017): 1750022. http://dx.doi.org/10.1142/s0218396x17500229.

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Acoustic impedance (AI) from seismic inversion can indicate rock properties and can be used, when combined with rock physics, to predict reservoir parameters, such as porosity. Solutions to seismic inversion problem are almost nonunique due to the limited bandwidth of seismic data. Additional constraints from well log data and geology are needed to arrive at a reasonable solution. In this paper, sedimentary facies is used to reduce the uncertainty in inversion and rock physics modeling; the results not only agree with seismic data, but also conform to geology. A reservoir prediction method, wh

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29

Postma, George. "The geology of fluvial deposits, sedimentary facies, basin analysis and petroleum geology." Sedimentary Geology 110, no. 1-2 (1997): 149–50. http://dx.doi.org/10.1016/s0037-0738(96)00081-4.

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30

Totman Parrish, Judith, and Gerilyn S. Soreghan. "Sedimentary Geology and the Future of Paleoclimate Studies." Sedimentary Record 11, no. 2 (2013): 4–10. http://dx.doi.org/10.2110/sedred.2013.2.4.

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31

Davis, Larry Eugene, and Robert Leo Eves. "A Sedimentary Rock Classification Scheme for Introductory Geology." Journal of Geological Education 34, no. 3 (1986): 186–87. http://dx.doi.org/10.5408/0022-1368-34.3.186.

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32

Soreghan, Lynn (Gerilyn) S., and Michael J. Soreghan. "A Reservoir Characterization Case Study for Sedimentary Geology." Journal of Geoscience Education 51, no. 2 (2003): 177–84. http://dx.doi.org/10.5408/1089-9995-51.2.177.

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33

Grotzinger, John, David Beaty, Gilles Dromart, et al. "Mars Sedimentary Geology: Key Concepts and Outstanding Questions." Astrobiology 11, no. 1 (2011): 77–87. http://dx.doi.org/10.1089/ast.2010.0571.

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34

Di Pietro, Ilaria, Gian Gabriele Ori, Monica Pondrelli, and Francesco Salese. "Geology of Aeolis Dorsa alluvial sedimentary basin, Mars." Journal of Maps 14, no. 2 (2018): 212–18. http://dx.doi.org/10.1080/17445647.2018.1454350.

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35

Sun, Jiajia, Aline Tavares Melo, Jae Deok Kim, and Xiaolong Wei. "Unveiling the 3D undercover structure of a Precambrian intrusive complex by integrating airborne magnetic and gravity gradient data into 3D quasi-geology model building." Interpretation 8, no. 4 (2020): SS15—SS29. http://dx.doi.org/10.1190/int-2019-0273.1.

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Mineral exploration under a thick sedimentary cover naturally relies on geophysical methods. We have used high-resolution airborne magnetic and gravity gradient data over northeast Iowa to characterize the geology of the concealed Precambrian rocks and evaluate the prospectivity of mineral deposits. Previous researchers have interpreted the magnetic and gravity gradient data in the form of a 2D geologic map of the Precambrian basement rocks, which provides important geophysical constraints on the geologic history and mineral potentials over the Decorah area located in the northeast of Iowa. Ho

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36

Kuznetsov, V. G., and A. N. Dmitrievsky. "L.V. Pustovalov and the Development of His Ideas on Oil and Gas Lithology." Литология и полезные ископаемые, no. 2 (March 1, 2023): 201–7. http://dx.doi.org/10.31857/s0024497x22700069.

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The article discusses the main directions of lithological research in the field of oil and gas geology, continuing and developing the ideas and research of L.V. Pustovalov. A number of such areas are closely coordinated with other branches of geology – tectonics, stratigraphy, etc. A wide range of such studies includes the analysis of the structure and development of sedimentary basins, the elucidation of the structure of the internal structure of sedimentary complexes, the forecast and search for non-structural traps of oil and gas, the study of natural reservoirs of oil and gas at different

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37

Meng, Ning Ning, Guang Xue Zhang, Gao Qun Wei, and Xin Lv. "Study on Three-Dimensional Geological Modeling of Reservoir in Hei46 Block." Advanced Materials Research 1073-1076 (December 2014): 2349–52. http://dx.doi.org/10.4028/www.scientific.net/amr.1073-1076.2349.

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Three dimensional (3D) geologic modeling is used to study the reservoir quantitatively from a three-dimensional angle, and its core is the prediction to reservoir of multi-disciplinary integration, quantitative and visualization. Compared with traditional reservoir research, it has a significant advantage. This paper makes geological modeling research and builds structural models sedimentary micro-facies models and phased property model for Hei46 block of Daqingzi oilfield by utilizing 3D geologic modeling technique and petrel software on the basis of integrated using of geology, logging, oil

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38

He, Qing Kun, and Chang Ying Shi. "Application of Electron Probe Microanalyzer (EPMA) to Depositional Environment Identification of Sedimentary Rock." Advanced Materials Research 881-883 (January 2014): 1795–98. http://dx.doi.org/10.4028/www.scientific.net/amr.881-883.1795.

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s: Electron microprobe technology is widely used to component analysis of metals, minerals and geology. Elements of sedimentary rock including B, Ga, Ba, Sr, Co, V, Cr, Mn, Fe, Ni were analyzed by EPMA respectively. It was discussed that marine faces and continental facies, oxidation environment and reducing environment, the depth of water and salinity influence on sedimentary rock, respectively. Then the influence of marine faces, continental faces, oxidation environment, reducing environment and the depth of water and salinity on sedimentary rock was discussed respectively. The results show

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39

Yu, Jiang Tao, Jin Liang Zhang, and Shuang Yan Chen. "Application of Three-Dimensional Fine Geological Modeling in Complex Fault-Block Reservoir with Low Permeability." Applied Mechanics and Materials 511-512 (February 2014): 779–82. http://dx.doi.org/10.4028/www.scientific.net/amm.511-512.779.

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Three dimensional geologic modeling is a powerful tool for reservoir development stages of geological study, it can solves many traditional problems existing in geological research through the establishment of precise three dimensional geologic modeling and represents an important direction for the further development of oilfield geological research. Low permeability and thin interbed reservoir of complex fault block have the characteristics of severe heterogeneity, complex relations of oil-water distribution, poor development effect, it is necessary to built high precision three dimensional g

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40

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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41

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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42

Gayer, Rod. "Tectonics of sedimentary basins." Journal of Structural Geology 17, no. 12 (1995): 1805. http://dx.doi.org/10.1016/0191-8141(95)90021-7.

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43

Mushayandebvu, M. F., and J. Davies. "Magnetic gradients in sedimentary basins: Examples from the Western Canada Sedimentary Basin." Leading Edge 25, no. 1 (2006): 69–73. http://dx.doi.org/10.1190/1.2164758.

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44

Vernikovsky, V. A., and V. S. Shatsky. "Current Issues of Tectonics, Paleogeography, Geodynamic Evolution, and Mineral Resources of the Continental Margins of the Russian Arctic." Russian Geology and Geophysics 63, no. 4 (2022): 321–23. http://dx.doi.org/10.2113/rgg20214445.

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Abstract The special issue is focused on the problems of tectonics, paleogeography, geodynamic evolution, and mineral resources of the continental margins of the Russian Arctic. This topic is relevant, since the knowledge of the geologic structure of the Arctic Ocean and its formation and evolution can solve many global problems of geology and important regional problems, including the formation of oil- and gas-bearing sedimentary basins as well as prospecting for, and development of, diamonds and deposits of nonferrous, noble, rare-earth, and other minerals. In previous issues of Russian Geol

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45

Cavalcante, Francesco. "Editorial for Special Issue “Clays, Clay Minerals, and Geology”." Minerals 11, no. 10 (2021): 1057. http://dx.doi.org/10.3390/min11101057.

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46

Łuczyński, Piotr, Stanisław Skompski, and Wojciech Kozłowski. "Recent studies on the Silurian of the western part of Ukraine." Acta Geologica Polonica 66, no. 3 (2016): 304–20. http://dx.doi.org/10.1515/agp-2016-0014.

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Abstract The paper summarises the effects of recent studies carried out by a team from the Department of Historical and Regional Geology of the Faculty of Geology, University of Warsaw on the upper Silurian of Podolia (western part of Ukraine). The sedimentary history of the Silurian succession of Podolia is characterised by its cyclic pattern, with shallowing-upward cyclothems. In the traditional interpretation, the occurrence of stromatoporoid beds within each cyclothem marks the deepest (or most open-marine) sedimentary environment within the cycle. According to the results of recent studie

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47

Gehrels, George E., Jason B. Saleeby, and Henry C. Berg. "Geology of Annette, Gravina, and Duke islands, southeastern Alaska." Canadian Journal of Earth Sciences 24, no. 5 (1987): 866–81. http://dx.doi.org/10.1139/e87-086.

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Geologic mapping, U–Pb (zircon) geochronometry, and conodont studies indicate that the major pre-Jurassic assemblages on Annette, Gravina, Duke, and adjacent smaller islands include pre-Middle Ordovician metavolcanic and metasedimentary rocks (Wales metamorphic suite); Cambrian metaplutonic rocks; Ordovician – Early Silurian volcanic (Descon Formation), dioritic, and gabbroic rocks; Silurian trondhjemitic plutons; Early Devonian sedimentary (Karheen Formation) and volcanic rocks; Late Triassic sedimentary and volcanic rocks (Hyd Group); and a large body of Late Triassic pyroxene gabbro.Stratig

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48

Zhang, Huan, Jun Li, Tong Wei Luo, and Wen Li Lv. "Geological Characteristics of the Changdong-Manxu Pb-Zn Deposit in Ninger, Yunnan and its Ore-Search Prospects." Advanced Materials Research 634-638 (January 2013): 3390–93. http://dx.doi.org/10.4028/www.scientific.net/amr.634-638.3390.

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Since the 1950s, the Changdong-Manxu Pb-Zn deposit has ever been explored for ore bodies by a number of Geology Parties，On the basis of studying the regional metallogenic geological background, Geologic characteristics of the deposits, ore-controlling geological factors, they thought the deposit belongs to sedimentary transformation type stratabound lead-zinc ore deposit ,which controlled by fault structures. According to the features of ore-controlling fault features and metallogenic conditions，it is possible to find large to super-large ores inside and outside the tectonic zones of the depos

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49

Francesco, Guerrera, Martín Manuel Martín, Martín-Pérez José A., Martín-Rojas Iván, Miclăuş Crina, and Serrano Francisco. "Tectonic control on the sedimentary record of the central Moldavidian Basin (Eastern Carpathians, Romania)." Geologica Carpathica 63, no. 6 (2012): 463–79. http://dx.doi.org/10.2478/v10096-012-0036-0.

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AbstractThe sedimentary record of the Tarcău and Vrancea Nappes, belonging to the flysch accretionary zone of the Eastern Carpathians (Eastern Carpathian Outer Flysch), registered Cretaceous-Miocene events during the evolution of the Moldavidian Basin. Our biostratigraphic data indicate that the deposits studied are younger than previously reported. The comparison of sedimentary record studied with the Late Cretaceous-Early Miocene global eustatic curve indicates that eustatic factor played a secondary role, after the tectonic one. Four main stages of different processes influenced by tectonic

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50

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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