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Journal articles on the topic 'Sedimentary basins'

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Published: 4 June 2021
Last updated: 29 July 2024

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1

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

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2

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

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3

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

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4

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

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5

Armstrong, P. A. "Thermochronometers in Sedimentary Basins." Reviews in Mineralogy and Geochemistry 58, no. 1 (January 1, 2005): 499–525. http://dx.doi.org/10.2138/rmg.2005.58.19.

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6

Tankard, A. "Tectonics of sedimentary basins." Sedimentary Geology 106, no. 3-4 (November 1996): 301–3. http://dx.doi.org/10.1016/s0037-0738(96)00004-8.

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7

Crook, Keith A. W. "South Pacific Sedimentary Basins." Marine Geology 123, no. 1-2 (March 1995): 117–18. http://dx.doi.org/10.1016/0025-3227(95)80008-y.

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8

Kreitler, Charles W. "Hydrogeology of sedimentary basins." Journal of Hydrology 106, no. 1-2 (March 1989): 29–53. http://dx.doi.org/10.1016/0022-1694(89)90165-0.

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9

INGERSOLL, RAYMOND V. "Tectonics of sedimentary basins." Geological Society of America Bulletin 100, no. 11 (November 1988): 1704–19. http://dx.doi.org/10.1130/0016-7606(1988)100<1704:tosb>2.3.co;2.

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10

Flüh, Ernst R. "Geophysics for Sedimentary Basins." Tectonophysics 287, no. 1-4 (March 1998): 320–21. http://dx.doi.org/10.1016/s0040-1951(98)80077-2.

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11

Kamp, Peter J. J. "South pacific sedimentary basins." Sedimentary Geology 94, no. 3-4 (January 1995): 304–6. http://dx.doi.org/10.1016/0037-0738(95)90024-1.

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12

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

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13

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

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14

Sunarjanto, Djoko, Sri Wijaya, Suprajitno Munadi, Bambang Wiyanto, and Doma F. Prasetio. "INDONESIAN TERTIARY SEDIMENTARY BASIN." Scientific Contributions Oil and Gas 31, no. 2 (March 21, 2022): 19–27. http://dx.doi.org/10.29017/scog.31.2.1002.

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Since 1980 the number of Indonesian Sedimentary Basin which is officially announced by the government are 60 basins, but informally the variation in the range of less than 60 up to around 66 basins. Based on stratigraphic and tectonics conditions of some areas there are overlapping layers between Tertiary Sedimentary and Pre Tertiary Basin. In general the definition of a sedimentary basin is a region, part of the earth's crust where sedimentary strata have been deposited in a relatively much greater thickness than its surrounding area. The nomenclature for basin is referred more to basinal areas. Based on sedimentary basin classification there are: type of plate where basin exists, basin position in the plate margin, type of plate interaction, time development of basin and basins fill with respect to tectonic and shape of the basin. The updating classification using new technology and knowledge of the basin, can also update previous knowledge because of the limitation of the data and the lack of new concept when the report was published. 63 Tertiary Sedimentary Basins (16 producing basin of oil and gas, 8 drilled basin with discovery, 15 drilled basin with has no discovery yet and 24 basin which has not been drilled yet) could be used as a basic data for development of science and technology, to support government policy and investor, to improve and accelerate oil and gas exploration and production in Indonesia.
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15

Boruah, Annapurna. "Unconventional Shale Gas Prospects in Indian Sedimentary Basins." International Journal of Scientific Research 3, no. 6 (June 1, 2012): 35–38. http://dx.doi.org/10.15373/22778179/june2014/181.

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16

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 (October 1, 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 conglomerates, pelagic sediments, and ubiquitous iron-formations; subaerial deposits have not been identified. In contrast, sedimentary cycles 2 and 4 show a prevalence of fluvial to shallow-water marine and (or) lacustrine deposits. Tectono-magmatic influence on sedimentation during cycles 2 and 4 is documented by (i) the presence of numerous unconformities underlain by plutonic and volcanic rocks; (ii) locally voluminous shoshonitic and calc-alkaline volcanic rocks; (iii) abundance of plutonic detritus; (iv) rapid vertical and lateral facies changes; and (v) repetition of successions of large-scale (50–250 m thick) alluvial and shallow-water deposits. Sedimentary cycle 1 represents incipient arc basins dominated by volcaniclastic debris, whereas cycle 2 reflects unroofing of arc volcanoes down to the plutonic roots. The sedimentary basins of cycle 3 have been tentatively interpreted as basins connecting arc terranes, within which small extensional cycle 4 basins of the successor or pull-apart type developed. The sedimentary facies associations, the tectono-magmatic influence on sedimentation, the chronological basin evolution, and overall southward younging of the basins invite comparison with modern island arcs formed by plate-tectonic processes.
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17

Oxburgh, E. R., R. K. O'Nions, and R. I. Hill. "Helium isotopes in sedimentary basins." Nature 324, no. 6098 (December 1986): 632–35. http://dx.doi.org/10.1038/324632a0.

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18

Stewart, S. A., G. J. Hay, P. L. Rosin, and T. J. Wynn. "Multiscale structure in sedimentary basins." Basin Research 16, no. 2 (June 2004): 183–97. http://dx.doi.org/10.1111/j.1365-2117.2004.00228.x.

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19

Carroll, A. R., S. A. Graham, and M. E. Smith. "Walled sedimentary basins of China." Basin Research 22, no. 1 (February 2010): 17–32. http://dx.doi.org/10.1111/j.1365-2117.2009.00458.x.

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20

Scheck-Wenderoth, Magdalena, Francois Roure, and Ulf Bayer. "Progress in understanding sedimentary basins." Tectonophysics 470, no. 1-2 (May 2009): 1–2. http://dx.doi.org/10.1016/j.tecto.2008.10.007.

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21

Cotillon, Pierre. "Geodynamic evolution of sedimentary basins." Geobios 31, no. 4 (1998): 466. http://dx.doi.org/10.1016/s0016-6995(98)80118-6.

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22

Jessop, Alan M. "Thermal modeling in sedimentary basins." Marine Geology 83, no. 1-4 (September 1988): 321–22. http://dx.doi.org/10.1016/0025-3227(88)90067-9.

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23

Deming, David, Constantin Cranganu, and Youngmin Lee. "Self-sealing in sedimentary basins." Journal of Geophysical Research: Solid Earth 107, B12 (December 2002): ETG 2–1—ETG 2–9. http://dx.doi.org/10.1029/2001jb000504.

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24

BETHKE, C. M., S. P. ALTANER, W. J. HARRISON, and C. UPSON. "Supercomputer Analysis of Sedimentary Basins." Science 239, no. 4837 (January 15, 1988): 261–67. http://dx.doi.org/10.1126/science.239.4837.261.

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25

Vilotte, J. P., J. Melosh, W. Sassi, and G. Ranalli. "Lithosphere rheology and sedimentary basins." Tectonophysics 226, no. 1-4 (November 1993): 89–95. http://dx.doi.org/10.1016/0040-1951(93)90112-w.

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26

Purdy, G. M. "The Evolution of Sedimentary Basins." Sedimentary Geology 43, no. 1-4 (April 1985): 307–8. http://dx.doi.org/10.1016/0037-0738(85)90063-6.

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27

Cobbold, P. R., P. Davy, D. Gapais, E. A. Rossello, E. Sadybakasov, J. C. Thomas, J. J. Tondji Biyo, and M. de Urreiztieta. "Sedimentary basins and crustal thickening." Sedimentary Geology 86, no. 1-2 (July 1993): 77–89. http://dx.doi.org/10.1016/0037-0738(93)90134-q.

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28

Bjørlykke, Knut. "Fluid flow in sedimentary basins." Sedimentary Geology 86, no. 1-2 (July 1993): 137–58. http://dx.doi.org/10.1016/0037-0738(93)90137-t.

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29

Kholodov, V. N. "Sedimentary basins: Regularities in their formation and classification principles. Communication 2. Sedimentary rock basins." Lithology and Mineral Resources 45, no. 3 (May 2010): 238–74. http://dx.doi.org/10.1134/s0024490210030028.

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30

Radkovets, Nataliya, Kostyantyn Hrygorchuk, Yuriy Koltun, Volodymyr Hnidets, Ihor Popp, Marta Moroz, Yuliya Hayevska, et al. "Dynamics of lithogenesis of Phanerozoic sedimentary sequence of the Carpathian-Black Sea region in the aspect of their oil- and gas-bearing potential." Geology and Geochemistry of Combustible Minerals 1-2, no. 183-184 (2021): 60–75. http://dx.doi.org/10.15407/ggcm2021.01-02.060.

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The objective of this work was to study the environments and processes of ancient sedimentation in the epi- and mesopelagic basins of the Carpathian-Black Sea region and to clarify the conditions of oil and gas basins formation within the study region as well as the main aspects of hydrocarbon generation. The burial history of the basins, some aspects of their fluid regime, issues of lithogenetic record, features of transformation of sedimentary basins into the rock-formation basins and the development of the latter during the Phanerozoic are considered. The spatial and temporal peculiarities of the evolution of epi-mesopelogic systems and their influence on the formation of oil- and gas-bearing strata within the Carpathian-Black Sea region have been studied. It has been established that in the sedimentary basins of the Carpathian-Black Sea continental margin of the Tethys Ocean during the long geological history the different intensity structural and morphological changes took place: changes of the subsidence rate of the basin bottom, inversion uplifts, sedimentation pauses, deformation of the sedimentary fill. This was reflected both in the peculiarities of the development of sedimentary environments and in the processes of substance differentiation with the formation of certain post-sedimentary mineral-structural parageneses. It was proved that discrete processes of differentiated compaction and defluidization of sediments cause a number of deformation phenomena, which can be reflected in the features of the morphology of the sedimentary basin bottom, influencing the nature of sediment transportation and accumulation. On the basis of the conducted investigations a number of practical results were obtained which will allow forming new approaches to criteria of hydrocarbons prospecting, in particular the lithophysical aspect which is concentrated on the reservoir properties of rocks; sedimentary reconstructions and the diversity of cyclicity of the studied sediments as a factor of the establishment of prospective areas, reconstruction of the burial history, which provides an information on the state of transformation of organic matter and hydrocarbons, and therefore the range of prospective depths for oil and gas occurrence.
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31

Guliyev, I. S., N. R. Abdullayev, and Sh M. Huseynova. "Distribution and volume of rocks in sedimentary basins – unusual case of the South Caspian basin." SOCAR Proceedings, no. 3 (June 30, 2020): 7–13. http://dx.doi.org/10.5510/ogp20200300439.

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The article gives a brief overview of the sedimentary cover of the Earth and summarizes volumes and mass of sediments contained in the Earth sedimentary layer (stratisphere). Using available data authors show unique nature of the South Caspian Basin and other rapidly subsiding basins with large amount of sediments and attenuated crust. Sedimentary, crustal and lithospheric thickness correlations are discussed.
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32

Speece, Marvin A., Timothy D. Bowen, James L. Folcik, and Henry N. Pollack. "Analysis of temperatures in sedimentary basins: the Michigan Basin." GEOPHYSICS 50, no. 8 (August 1985): 1318–34. http://dx.doi.org/10.1190/1.1442003.

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We develop an analytical and numerical methodology for the analysis of large bottom‐hole temperature (BHT) data sets from sedimentary basins, and test the methodology using temperature, stratigraphic, and lithologic data from 411 boreholes in the Michigan Basin. Least‐squares estimates of temperature gradients in the formations and lithologies present are calculated as solutions to a large system of linear equations. At each borehole the temperature difference between the bottom and top of the hole is represented as a sum of temperature increments through the various formations or lithologies penetrated by the borehole. Quadratic programming techniques enable bounds to be placed on the gradient solutions in order to suppress or exclude improbable gradient estimates. Numerical experiments with synthetic data reveal that the estimates of temperature gradients for a given formation or lithology are sensitive to the degree of representation of that unit; well represented units have more stable gradient estimates in the presence of noise than do poorly represented units. The estimates of temperature gradients obtained for lithologies are more stable than those for formations and are believed to be good estimates of actual lithologic temperature gradients in the Michigan Basin. Formation temperature gradients obtained as a weighted sum of the estimates of the component lithologic temperature gradients appear to be good estimates of the average temperature gradients for the formations of the basin. At each borehole a temperature residual exists corresponding to the difference between the observed BHT and the BHT predicted by the estimated interval temperature gradients. Residuals are far more stable than estimated temperature gradients. The values of residuals change little regardless of whether lithology, formation, bounded, or unbounded gradient estimates are used to calculate them. Maps of residuals indicate well‐defined and spatially coherent patterns of positive and negative temperature residuals. Filtered subsets of large‐magnitude residuals alone show a pattern of negative residuals coinciding with the mid‐Michigan gravity high, a geophysical feature thought to delineate a Precambrian (Keweenawan) rift zone in the crust beneath the basin. Thermal models of the Michigan Basin and the crust and upper mantle beneath the basin indicate that the suspected rift beneath the basin can cause a variation in basement heat flow sufficient to produce temperature residuals of the magnitude observed in the sediments, with negative temperature residuals over the area of the rift.
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33

Zhong, Guang Jian, Da Meng Liu, and Guang Hong Tu. "Petroleum Exploration Potential of Xisha Trough Basin in SCS." Advanced Materials Research 734-737 (August 2013): 1230–34. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.1230.

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Nowadays oil-gas exploration make a great contribution to the world oil-gas reserve increase. A series of deepwater passive continental margin basins are found in Northern Continental Slope of South China Sea. These basins consisted of thick Mesozoic and Cenozoic sedimentary strata with the characteristics of the major world deepwater oil-gas basins. As one of Cenozoic sedimentary basins in deepwater area of Northern Slope of South China Sea, Xisha Trough Basin developed 1500-8000m thick sedimentary strata, which are north-south zoning characteristics of thicker in the center and thinner both in the north and south sides of basin. In its evolutionary history there are two stages: One is Paleocene-Oligocene Rift with Continental River-Lake Facies sedimentary and the other is Miocene-Quaternary Depression with shallow sea-hemiplegic sedimentary. It has good petroleum geological conditions that source rocks consist of lacustrine mudstones, paralic mudstone, and marine mudstone, Tertiary high porosity and permeability deepwater fan reservoirs are the main reservoir, and structural traps and lithologic traps developed. In a word, it has good oil-gas exploration potential.
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34

Sidorov, Roman V., Mikhail K. Kaban, Anatoly A. Soloviev, Alexei G. Petrunin, Alexei D. Gvishiani, Alexei A. Oshchenko, Anton B. Popov, and Roman I. Krasnoperov. "Sedimentary basins of the eastern Asia Arctic zone: new details on their structure revealed by decompensative gravity anomalies." Solid Earth 12, no. 12 (December 20, 2021): 2773–88. http://dx.doi.org/10.5194/se-12-2773-2021.

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Abstract. In the present study, the structure of sedimentary basins in the eastern Asia Arctic zone is analysed by employing the approach based on decompensative gravity anomalies. Two obtained models, differing in their initial conditions, provide thickness and density of sediments in the study area. They demonstrate essentially new details on the structure, shape, and density of the sedimentary basins. Significant changes in the sedimentary thickness and the depo-centre location have been found for the Anadyr Basin in its continental part. Also, new details on the sedimentary thickness distribution have been revealed for the central part of the Penzhin and Pustorets basins; for the latter, the new location of the depo-centre has been identified. The new model agrees well with the seismic data on the sedimentary thickness for the offshore part of the Chauna Basin confirming that the method is robust. The most significant lateral redistribution of the thickness has been found for the Lower Cretaceous coal-bearing strata in the northern part of the Zyryanka Basin, where the connection of two coal-bearing zones, which was not previously mapped, has been identified. Also, the new details on the sedimentary thickness distribution have been discovered for the Primorsk Basin. Therefore, the new results substantially improve our knowledge about the region, since previous geological and geophysical studies were unsystematic, sparse, and limited in depth. Thus, the implementation of the decompensative gravity anomalies approach provides a better understanding of the evolution of the sedimentary basins and the obtained results can be used for planning future detailed studies in the area.
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35

Løtveit, Ingrid F., Willy Fjeldskaar, and Magnhild Sydnes. "Tilting and Flexural Stresses in Basins Due to Glaciations—An Example from the Barents Sea." Geosciences 9, no. 11 (November 11, 2019): 474. http://dx.doi.org/10.3390/geosciences9110474.

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Many of the Earth’s sedimentary basins are affected by glaciations. Repeated glaciations over millions of years may have had a significant effect on the physical conditions in sedimentary basins and on basin structuring. This paper presents some of the major effects that ice sheets might have on sedimentary basins, and includes examples of quantifications of their significance. Among the most important effects are movements of the solid Earth caused by glacial loading and unloading, and the related flexural stresses. The driving factor of these movements is isostasy. Most of the production licenses on the Norwegian Continental Shelf are located inside the margin of the former Last Glacial Maximum (LGM) ice sheet. Isostatic modeling shows that sedimentary basins near the former ice margin can be tilted as much as 3 m/km which might significantly alter pathways of hydrocarbon migration. In an example from the SW Barents Sea we show that flexural stresses related to the isostatic uplift after LGM deglaciation can produce stress changes large enough to result in increased fracture-related permeability in the sedimentary basin, and lead to potential spillage of hydrocarbons out of potential reservoirs. The results demonstrate that future basin modeling should consider including the loading effect of glaciations when dealing with petroleum potential in former glaciated areas.
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36

Rodnikov, A. G. "GEODYNAMICS." GEODYNAMICS 2(11)2011, no. 2(11) (September 20, 2011): 266–68. http://dx.doi.org/10.23939/jgd2011.02.266.

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Research was conducted on the deep structure of sedimentary basins located in the continent – ocean contact zones characterized by increased seismicity, volcano eruptions and other disastrous phenomena. Sedimentary basin formation is associated with processes going on in the upper mantle and specifically in the asthenosphere. From the asthenosphere to the crust, diapirs branch off that are channels by which deep fluids bearing earth-degassing products penetrate into sedimentary basins, being an additional source of hydrocarbons.
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37

Ivanov, V. L. "Evolution of Antarctic prospective sedimentary basins." Antarctic Science 1, no. 1 (March 1989): 51–56. http://dx.doi.org/10.1017/s095410208900009x.

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No less than 15–20 sedimentary basins are now known on the Antarctic continental landmass and surrounding continental shelves. Reconstruction of their tectonic and stratigraphic evolution is a specialized task. Owing to the polar position of the continent, the Pacific and Atlantic global geostructures are closely spaced there and the interplay between them is strong enough to result in hybridization of the characteristic tectonic features of the various basins. The present morphostructure of the southern polar region of the Earth is characterized by a prominent circumpolar zoning. Therefore, the sedimentary basins form a gigantic ring along the continental margin, including both the shelf proper and the edge of the continent. Within the ring, the basins are associated with different types of margins successively replacing each other, from the Mesozoic magmatic are in the Pacific segment to the classic passive margin off East Antarctica. The formation of the sedimentary basins in the Antarctic segment of the Pacific mobile belt was a part of a single process of geosynclinal development, whereas on the craton flank the process was superposed on the continental structures by rifting during Gondwana fragmentation. During post-break-up tectonism, continental glaciation played an important part in the formation of the sedimentary basins.
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38

Costamagna, Luca Giacomo. "The carbonates of the post-Variscan basins of Sardinia: the evolution from Carboniferous–Permian humid-persistent to Permian arid-ephemeral lakes in a morphotectonic framework." Geological Magazine 156, no. 11 (May 31, 2019): 1892–914. http://dx.doi.org/10.1017/s0016756819000232.

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AbstractLate to post-Variscan sedimentary basins of Sardinia were influenced during Pennsylvanian to Permian times by two main tectono-sedimentary cycles: a Pennsylvanian to Cisuralian cycle represented mainly by dark limnic deposits, overlain by a Guadalupian to a possibly Lopingian cycle, mostly characterized by red-bed deposits. Lacustrine waterbodies developed in some sedimentary basins that were filled with siliciclastic to frequently early silicified carbonate deposits, depending on the climate and environmental conditions, landscape morphology and tectonic regime. The limnic successions of the lower tectono-sedimentary cycle were deposited in permanent, tens of metres deep lakes in deep, narrow tectonic strike-slip basins under a temperate to warm-humid climate. They started as lakes with terrigenous sedimentary input and developed minor carbonate deposits mainly at the end of their story. Conversely, the red-bed successions of the upper cycle were deposited in ephemeral, shallow playa lakes related to wider basins in an extensive alluvial plain under a hot and arid climate. Here, the siliciclastic sediments are intercalated with thin carbonate beds that are typical of a high evaporation rate. The evolution of the lake type could be related not only to a major climatic shift, but also to the changing morphotectonic conditions of the Variscan chain influencing the local microclimate. Comparisons with coeval successions in the Provence Basin, the Massif Central Aumance basin (France) and the Saar–Nahe Basin (Germany) show both similarities and differences between the basins.
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39

Hoang, Tien Dinh, and Luan Thi Bui. "The mechanism of formation, development and deformation of sedimentary basins in Viet Nam continental shelf." Science and Technology Development Journal - Natural Sciences 1, T5 (November 29, 2018): 278–89. http://dx.doi.org/10.32508/stdjns.v1it5.561.

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The sedimentary basins in area of Việt Nam continental shelf are located along the deep fault systems between the folded Indochinese block and Việt Băc-Hoa Nam platform and with the transitional zone. Is means that the zone attenuated continental crust. Due to that extruction of the Indochinese block toward the SoustEast which wrenched in right, in addition, due to the appearance of the thermal anomaly, producing the activity of Bien Dong seafloor spreading axis and drift of Australian–New Guinea plate toward Nord-East, induced some geodinamic factors to form many sedimentary basins in margins of Biển Dong Sea, such as: rift, pressure, extension, vertical slide cliff, horizontal displacement and wrench. These geodinamic factors created favourable conditions to form, develop and deform the sedimentary basins in Việt Nam continental shelf, followed the pull- apart type mechanism. But each sedimentary basin had its type of mechanism which depended on the concrete place of its basin from the Indochinese block and the thermal anomaly in Bien Dong Sea. Beside, itsformed condition for gas hydrate accumulations in some basins.
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40

Martín-Martín, Manuel. "Tectono-Sedimentary Evolution of Cenozoic Basins." Geosciences 11, no. 5 (May 2, 2021): 199. http://dx.doi.org/10.3390/geosciences11050199.

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41

Pinet, B. "Deep seismic profiling and sedimentary basins." Bulletin de la Société Géologique de France V, no. 4 (July 1, 1989): 749–66. http://dx.doi.org/10.2113/gssgfbull.v.4.749.

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42

Yang, X. S. "Nonlinear viscoelastic compaction in sedimentary basins." Nonlinear Processes in Geophysics 7, no. 1/2 (June 30, 2000): 1–8. http://dx.doi.org/10.5194/npg-7-1-2000.

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Abstract. In the mathematical modelling of sediment compaction and porous media flow, the rheological behaviour of sediments is typically modelled in terms of a nonlinear relationship between effective pressure pe and porosity Φ, that is pe = pe (Φ). The compaction law is essentially a poroelastic one. However, viscous compaction due to pressure solution becomes important at larger depths and causes this relationship to become more akin to a viscous rheology. A generalised viscoelastic compaction model of Maxwell type is formulated, and different styles of nonlinear behaviour are asymptotically analysed and compared in this paper.
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43

Tipper, John C. "Modelling the fill of sedimentary basins." Exploration Geophysics 22, no. 2 (June 1991): 397–400. http://dx.doi.org/10.1071/eg991397.

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44

KLEIN, G. DEV. "Geothermometry: Thermal History of Sedimentary Basins." Science 243, no. 4898 (March 24, 1989): 1619. http://dx.doi.org/10.1126/science.243.4898.1619.

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45

Gay, Aurélien, and Sébastien Migeon. "Geological fluid flow in sedimentary basins." Bulletin de la Société géologique de France 188, no. 4 (2017): E3. http://dx.doi.org/10.1051/bsgf/2017200.

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46

Seslavinskiy, K. B., and V. A. Kucherinenko. "HIERARCHY OF PALEOZOIC PLATFORMAL SEDIMENTARY BASINS." International Geology Review 34, no. 8 (August 1992): 783–93. http://dx.doi.org/10.1080/00206819209465636.

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47

Kyser, Kurt, and Eric E. Hiatt. "Fluids in sedimentary basins: an introduction." Journal of Geochemical Exploration 80, no. 2-3 (September 2003): 139–49. http://dx.doi.org/10.1016/s0375-6742(03)00188-2.

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48

Wangen, Magnus. "The blanketing effect in sedimentary basins." Basin Research 7, no. 4 (December 1995): 283–98. http://dx.doi.org/10.1111/j.1365-2117.1995.tb00118.x.

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49

Shock, Everett L. "Organic acid metastability in sedimentary basins." Geology 16, no. 10 (1988): 886. http://dx.doi.org/10.1130/0091-7613(1988)016<0886:oamisb>2.3.co;2.

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50

Fjeldskaar, W., and A. Amantov. "Effects of glaciations on sedimentary basins." Journal of Geodynamics 118 (July 2018): 66–81. http://dx.doi.org/10.1016/j.jog.2017.10.005.

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