Relevant bibliographies by topics / Sedimentary basins

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Sedimentary basins'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 July 2024

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Journal articles on the topic "Sedimentary basins"

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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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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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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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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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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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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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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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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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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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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Dissertations / Theses on the topic "Sedimentary basins"

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Wilson, N. P. "Thermal studies in sedimentary basins." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383208.

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Turner, Jonathan David. "The subsidence of sedimentary basins." Thesis, University of Edinburgh, 1997. http://hdl.handle.net/1842/13150.

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Theoretical models for the evolution of extensional sedimentary basins make a number of simple, testable predictions for subsidence behaviour. These are that active extension (the syn-rift) will generally be accompanied by rapid subsidence on the downthrown side of normal faults. Once faulting has ceased (the post-rift) the entire basin is predicted to subside at an exponentially decreasing rate, driven by the cooling and thickening of the lithosphere. The aim of this thesis is to determine the significance of second-order departures from this predicted subsidence. Three periods of North Sea subsidence appear to violate these simple predictions: anomalously slow Late Jurassic/Early Cretaceous subsidence, which marks the syn-rift/post-rift transition, and two periods of accelerated post-rift subsidence during the Early Paleogene and Plio-Quaternary. Subsidence data from over 300 boreholes from several basins with different rifting histories on the Northwest European continental plate have been analysed to determine the spatial and temporal distribution of these and other second-order subsidence anomalies. Uncertainties and errors in the observed subsidence calculations cannot explain the anomalous behaviour recognised. The periods of apparently anomalous subsidence are, instead, shown to be the result of geological or tectonic processes that modified either the subsidence history or record of subsidence of the basins studied. Apparent slow Late Jurassic/Early Cretaceous subsidence in the North Sea was the result of well siting and sediment starvation. Analysis of wells from the downthrown side of normal faults in several basins reveals an excellent correlation between rapid subsidence (often >1000m in 10My) and active extension (as documented from other sources of geological information). This was obscured by intense sediment starvation (sedimentation rates <20m/My) in the Central North Sea during Late Jurassic times which generated the apparent subsidence anomaly. Sedimentation rate maps reveal an expansion of the area of sediment starvation during late Jurassic times and into the Early Cretaceous. Cretaceous to Recent sedimentation patterns were then dominated by the interplay between the location and erosion history of extra-basinal sediment source areas and the remnant underfilled Jurassic rift topography.
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Lee, Jimin. "Earthquake site effect modeling in sedimentary basins using a 3-D indirect boundary element-fast multipole method." Diss., Online access via UMI:, 2007.

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Borge, Hans. "Fault controlled pressure modelling in sedimentary basins /." Doctoral thesis, Norwegian University of Science and Technology, Department of Mathematical Sciences, 2000. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-1763.

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The starting point for this Dr. Ing. thesis was the requirement for models describing basin scale overpressure for use in basin modelling studies. It is necessary to identify, understand and describe both the generating mechanisms and the fluid flow in sedimentary basins in order to meet this requirement.

All of the models developed are based upon a study area consisting of fault bounded pressure compartments. A reservoir simulator has applied a lateral cross fault transmissibility model and by defining the overpressure history in some of the pressure compartments it has been possible to model the overpressure through geological time. A simpler model estimating the present day overpressure distribution based upon the same fault transmissibility model is developed. This model is able to provide a snapshot of the main present day pressure trends. This model has further been developed to a full pseudo 3D-pressure simulator including generation and dissipation of pressure through time. Due to the quantification of generation and dissipation of overpressure it is possible to model hydraulic fracturing and leakage through the overlying seals. In addition to the models describing the overpressure, an algorithm that converts the pressure compartments into a quadrangle grid system is developed.

The main part of the work in this thesis deals with quantifying basin scale generation and dissipation of overpressure. Different models are developed based upon the available literature and knowledge achieved during this work. All the models used are thoroughly described. The pressure simulator PRESSIM is developed in order to test, improve and reject different models. Several simulations of the overpressure history in the North Viking Graben and the Haltenbanken area offshore Norway are presented. The modelled overpressures are calibrated to the observed pressures revealed by exploration wells. In general, the results are very satisfactory due to relatively small deviations between the modelled and observed overpressures. The simulations provide an increased knowledge of the mechanisms generating and dissipating the overpressure and form a good basis for discussing the nature of the overpressure. In addition, the results suggest which mechanisms are the most important in the different parts of the basin. The pressure simulator PRESSIM can be used to test and verify alternative pressure generation models and flow descriptions in a basin. It is possible to model the position and timing of the hydraulic fracturing because the pressure simulations are based upon a water budget for each pressure compartment.

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Ferrero, Charlie David. "Stochastic modelling of thermal histories in sedimentary basins." Thesis, Imperial College London, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.408156.

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Edwards, G. R. H. "Inverse modelling of extensional sedimentary basins and margins." Thesis, University of Cambridge, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.598779.

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In this dissertation, a fully depth-dependent 2D kinematic model of the litho­sphere is developed. This forward model forms the basis of an inversion scheme capable of recovering the temporal and spatial strain rate history of a basin from present-day observed stratigraphic and subsidence data. The inversion scheme does not assume any a priori form for the strain rate distribution and unlike previous inversion schemes does not assume that the strain rate is invariant with depth (White and Bellingham, 2002). The depth-dependent inversion is applied to two sedimentary basins. Data from the Northern North Sea is used to benchmark the new code against the previous 2D inversion scheme and the Gulf of Suez is studied in detail using newly collated stratigraphic profiles from across the region. The Gulf of Suez is found to have stretched by 12-18 km in two rift phases at 23-18 Ma and 14-11 Ma. Depth­-dependent stretching appears to be more important in the Southern Gulf than in the north. In the south, stretching factors beneath uplifted regions are higher in the mantle than in the crust. Data from three passive margins is also inverted. The inversion scheme provides little evidence for depth-dependent stretching in the Eastern Black Sea. However, the stratigraphic data from the Pearl River Mouth basin and Angolan Margin can be more faithfully reproduced when depth-dependent effects are included. In all cases, recovered strain rates and timings of rift events are consistent with published values. Using the inversion scheme developed within this dissertation allowed results to be obtained with no a priori assumptions about the form or timing of the rifting periods.
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Podkhlebnik, Yvette. "Subsidence et régime thermique des bassins intracratoniques et des marges continentales passives = Subsidence and thermal regime of intracratonic basins and continental passive margins /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1992. http://theses.uqac.ca.

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Holt, Peter Jonathan. "Subsidence mechanisms of sedimentary basins developed over accretionary crust." Thesis, Durham University, 2012. http://etheses.dur.ac.uk/3584/.

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This thesis uses forward modelling to investigate the formation of intercratonic basins upon accretionary crust. It began from the hypothesis that accretionary crust forms with a near normal thickness crust, but a thin lithosphere inherited from the terranes that compose it. After the accretion process has ceased the lithosphere stabilises and begins to cool, causing it to grow thicker and this in turn drives subsidence of the accretionary crust. A 1-D finite difference computer code was developed to model conductive heat flow through a column of cooling lithosphere and asthenosphere. To test the hypothesis, the subsidence produced by the modelling of this process was compared to the observed subsidence from backstripping numerous basins situated on accretionary crust The model produced a good fit to the subsidence in a detailed case study of two of the Palaeozoic basins in North Africa. The study was then extended to test the applicability of to accretionary crust globally. It found that while using measured values of the crust and lithospheric thickness for each region the model produced subsidence curves that matched the observed subsidence in each basin. It makes a more coherent argument for the formation of these basins that is able to explain a wider variety of features than other proposed subsidence mechanisms such as slow stretching or dynamic topography. These results suggest that such subsidence is an inherent property of accretionary crust which could influence the evolution of the continental crust over long time periods. The model was used to investigate the subsidence of the West Siberian Basin and found the subsidence patterns to be consistent with the decay of a plume head which thinned the lithosphere. This subsidence patterns indicate the plume material thinned the lithosphere over an area of 2.5 million km2 resulting in uplift before it cooled and subsided.
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Yang, Xin-She. "Mathematical modelling of compaction and diagenesis in sedimentary basins." Thesis, University of Oxford, 1997. http://ora.ox.ac.uk/objects/uuid:0bdc6c43-4534-4f08-97e2-8a33d6b13e61.

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Sedimentary basins form when water-borne sediments in shallow seas are deposited over periods of millions of years. Sediments compact under their own weight, causing the expulsion of pore water. If this expulsion is sufficiently slow, overpressuring can result, a phenomenon which is of concern in oil drilling operations. The competition between pore water expulsion and burial is complicated by a variety of factors, which include diagenesis (clay dewatering), and different modes (elastic or viscous) of rheological deformation via compaction and pressure solution, which may also include hysteresis in the constitutive behaviours. This thesis is concerned with models which can describe the evolution of porosity and pore pressure in sedimentary basins. We begin by analysing the simplest case of poroelastic compaction which in a 1-D case results in a nonlinear diffusion equation, controlled principally by a dimensionless parameter lambda, which is the ratio of the hydraulic conductivity to the sedimentation rate. We provide analytic and numerical results for both large and small lambda in Chapter 3 and Chapter 4. We then put a more realistic rheological relation with hysteresis into the model and investigate its effects during loading and unloading in Chapter 5. A discontinuous porosity profile may occur if the unloaded system is reloaded. We pursue the model further by considering diagenesis as a dehydration model in Chapter 6, then we extend it to a more realistic dissolution-precipitation reaction-transport model in Chapter 7 by including most of the known physics and chemistry derived from experimental studies. We eventually derive a viscous compaction model for pressure solution in sedimentary basins in Chapter 8, and show how the model suggests radically different behaviours in the distinct limits of slow and fast compaction. When lambda << 1, compaction is limited to a basal boundary layer. When lambda >> 1, compaction occurs throughout the basin, and the basic equilibrium solution near the surface is a near parabolic profile of porosity. But it is only valid to a finite depth where the permeability has decreased sufficiently, and a transition occurs, marking a switch from a normally pressured environment to one with high pore pressures.
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White, Adrian James. "Minimum stress and pore fluid pressure in sedimentary basins." Thesis, Durham University, 2001. http://etheses.dur.ac.uk/3879/.

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Leak-off pressures (LOPs) recorded during leak-off tests (LOTs) conducted down boreholes are often used to estimate the magnitude of the minimum stress (usually assumed to be horizontal – S(_h)) in the subsurface. However, the reliability of these tests has previously been questioned in the literature and the accuracy of the data obtained from them has been in doubt. Using original LOT data from Mid-Norway, this study has shown that through stringent quality control, good LOT data can be used to accurately constrain the magnitude of S(_h). Knowledge of the relationship between in-situ stress and pore pressures (Pp) in basins provides insights into their structure as well as having implications for well design and drilling safety. Using stress-depth plots to display S(_h) measurements from Mid-Norway and six further basins from around the world reveals a variability in the magnitude of Sh at all depths. Analyses show that rock mechanical properties or differences in the way LOTs are performed cannot explain this variability. Separate analysis of extended leak-off test (XLOT) data from Mid-Norway shows that variability in the magnitude of the LOP (most often used to calculate S(_h)) is inherent in the testing procedure. This inherence suggests either the variations in Sh are real (they represent basin heterogeneities) or that they result from a combination or rock mechanical and/or pumping pressure test parameters. Further use of multiple cycle XLOTs shows that using LOPs and instantaneous shut-in pressures (ISIPs) to calculate S(_h) produces similar results. Considering re-opening cycles of tests and those tests from greater depths shows the difference between the magnitude of Sh calculated using the LOP and ISIP is reduced. These same high quality data have been used to calculate the magnitude of the three principal stress from Mid-Norway and show the contemporary stress situation to be S(_h)
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Books on the topic "Sedimentary basins"

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Einsele, Gerhard. Sedimentary Basins. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5.

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Einsele, Gerhard. Sedimentary Basins. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4.

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L, Ridgley Jennie, ed. Evolution of sedimentary basins--Illinois Basin. Washington: U.S. G.P.O., 1995.

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Christopher, Beaumont, Tankard A. J, Atlantic Geoscience Society, and Canadian Society of Petroleum Geologists., eds. Sedimentary basins and basin-forming mechanisms. Halifax, N.S: Atlantic Geoscience Society, 1987.

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Busby, Cathy, and Antonio Azor, eds. Tectonics of Sedimentary Basins. Chichester, UK: John Wiley & Sons, Ltd, 2011. http://dx.doi.org/10.1002/9781444347166.

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Slingerland, Rudy. Simulating clastic sedimentary basins. Englewood Cliffs, N.J: PTR Prentice Hall, 1994.

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Henry, Georges. Geophysics for sedimentary basins. Paris: Editions Technip, 1997.

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Catherine, Busby, and Ingersoll Raymond V, eds. Tectonics of sedimentary basins. Cambridge, Mass., USA: Blackwell Science, 1995.

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F, Ballance P., ed. South Pacific sedimentary basins. Amsterdam: Elsevier, 1993.

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1939-, Selley Richard C., ed. African basins. Amsterdam: Elsevier Science, 1997.

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Book chapters on the topic "Sedimentary basins"

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Scheck-Wenderoth, Magdalena. "Sedimentary Basins." In Encyclopedia of Solid Earth Geophysics, 1–13. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10475-7_216-1.

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Jelgersma, Saskia. "Sedimentary Basins." In Encyclopedia of Earth Sciences Series, 1517–23. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_280.

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Jelgersma, Saskia. "Sedimentary Basins." In Encyclopedia of Earth Sciences Series, 1–7. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-48657-4_280-2.

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Scheck-Wenderoth, Magdalena. "Sedimentary Basins." In Encyclopedia of Solid Earth Geophysics, 1059–70. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_216.

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Healy, Terry R., Katherine Stone, Orville Magoon, Billy Edge, Lesley Ewing, Andrew D. Short, Dougals L. Inman, et al. "Sedimentary Basins." In Encyclopedia of Coastal Science, 853–59. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_280.

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Scheck-Wenderoth, Magdalena. "Sedimentary Basins." In Encyclopedia of Solid Earth Geophysics, 1353–65. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_216.

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Kundu, Sandeep Narayan. "Sedimentary Basins." In Geoscience for Petroleum Engineers, 33–42. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-7640-7_3.

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Einsele, Gerhard. "Basin Classification and Depositional Environments (Overview)." In Sedimentary Basins, 3–15. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_1.

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Einsele, Gerhard. "Sedimentation Rates and Organic Matter in Various Depositional Environments." In Sedimentary Basins, 455–79. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_10.

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Einsele, Gerhard. "The Interplay Between Sediment Supply, Subsidence, and Basin Fill." In Sedimentary Basins, 480–540. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_11.

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Conference papers on the topic "Sedimentary basins"

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Feng, Zhiqiang, Gao Dengliang, Stephan A. Graham, Wu Gaokui, and Duan Taizhong. "Classification of sedimentary basins." In International Meeting for Applied Geoscience & Energy. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2023. http://dx.doi.org/10.1190/image2023-3917017.1.

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Mboya, V. E. "Sedimentary Basins Prospective for Hydrocarbons." In Third EAGE Eastern Africa Petroleum Geoscience Forum. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201702431.

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Lawrence, David T., Mark Doyle, Sigmund Snelson, and W. T. Horsfield. "Stratigraphic modeling of sedimentary basins." In SEG Technical Program Expanded Abstracts 1987. Society of Exploration Geophysicists, 1987. http://dx.doi.org/10.1190/1.1891985.

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Hatton, Chris. "Geotherms, Lithosphere Thickness and Sedimentary Basins." In 11th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.241.hatton_paper1.

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Frankel, Arthur D. "Earthquake Ground Motions in Sedimentary Basins." In Structures Congress 2001. Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40558(2001)65.

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Planke, Sverre, John M. Millett, John M. Millett, John M. Millett, Dougal A. Jerram, Dougal A. Jerram, Dougal A. Jerram, Reidun Myklebust, Reidun Myklebust, and Reidun Myklebust. "UNDERSTANDING VOLCANIC DEPOSITS IN SEDIMENTARY BASINS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338222.

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Helwig, J. A. "Origin and Classification of Sedimentary Basins." In Offshore Technology Conference. Offshore Technology Conference, 1985. http://dx.doi.org/10.4043/4843-ms.

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Crampin, S. "Shear-wave point singularities in sedimentary basins." In 53rd EAEG Meeting. European Association of Geoscientists & Engineers, 1991. http://dx.doi.org/10.3997/2214-4609.201410907.

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Burlin, Y. K., and E. E. Karnyushina. "Reservoirs of Decompaction Zones in Sedimentary Basins." In 59th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.131.gen1997_d036.

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M. Astakhov, S., and A. N. Reznikov. "Geothermal Regime of the World Sedimentary Basins." In Simpósio Brasileiro de Geofísica. Sociedade Brasileira de Geofísica, 2012. http://dx.doi.org/10.22564/5simbgf2012.044.

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Reports on the topic "Sedimentary basins"

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Mossop, G. D., K. E. Wallace-Dudley, G. G. Smith, and J. C. Harrison. Sedimentary basins of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215559.

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Bell, J. S. Stress in Sedimentary Basins Seminar. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/130791.

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Syvitski, J. P. M. Modelling the sedimentary fill of basins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128089.

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Diecchio, R. J. Taconian Sedimentary Basins of the Appalachians. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132191.

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Peter J. Ortoleva. Self-Organized Megastructures in Sedimentary Basins. Office of Scientific and Technical Information (OSTI), June 2004. http://dx.doi.org/10.2172/825402.

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Thaddeus S. Dyman, Troy Cook, Robert A. Crovelli, Allison A. Henry, Timothy C. Hester, Ronald C. Johnson, Michael D. Lewan, et al. NATURAL GAS RESOURCES IN DEEP SEDIMENTARY BASINS. Office of Scientific and Technical Information (OSTI), February 2002. http://dx.doi.org/10.2172/833232.

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Huot-Vézina, G., V. Brake, N. Pinet, and D. Lavoie. GIS compilation of the Hudson Bay / Foxe sedimentary basins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292800.

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Dewing, K., L. E. Kung, C. J. Lister, E A Atkinson, and H. M. King. Resource assessments of northern Canadian sedimentary basins, 1973-2022. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330301.

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Paola, Chris, and Juan J. Fedele. Experimental and Theoretical Study of Strata Formation in Sedimentary Basins. Fort Belvoir, VA: Defense Technical Information Center, September 2004. http://dx.doi.org/10.21236/ada628057.

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Paola, Chris, and Juan J. Fedele. Experimental and Theoretical Study of Strata Formation in Sedimentary Basins. Fort Belvoir, VA: Defense Technical Information Center, September 2005. http://dx.doi.org/10.21236/ada572533.

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