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  • ==Accommodation== ...1}}Example of global sea level cycles combining with subsidence to produce accommodation. Copyright: Posamentier and Vail;<ref name=ch21r33 /> courtesy SEPM.]]
    8 KB (1,093 words) - 21:21, 3 February 2022
  • Depositional sequences can stack into successions of sequences if accommodation space permits preservation of successive sequences. Seismically, stacked se ...pace was created in the same area during seven cycles of progradation. The accommodation space is formed by down-to-the-north movement on the fault. This fault is p
    5 KB (698 words) - 14:57, 23 February 2022
  • ...Stacking patterns displayed in [[cross section]]s and individual logs show accommodation space changes which help us identify sequence and systems tracts. # Determine accommodation space changes from parasequence stacking patterns seen in well log cross se
    6 KB (845 words) - 16:53, 4 February 2022
  • * '''Prograde''' if the rate of sediment supply exceeds the rate of [[accommodation]] space formation. * '''Aggrade''' if the rate of sediment supply equals the rate of accommodation space formation.
    6 KB (811 words) - 16:50, 22 February 2022
  • ...lative changes of sea level create space for sediment accumulation (called accommodation space). ...a/a168/a168/0001/0300/0305.htm Parasequence stacking patterns, third-order accommodation events, and sequence stratigraphy of Middle to Upper Cambrian platform carb
    7 KB (989 words) - 20:45, 6 April 2022
  • ...e filling of the basin margin, shifting the accommodation space basinward. Accommodation space refers to the volume of space available for sediment accumulation—t
    5 KB (753 words) - 19:58, 18 February 2022
  • ==Accommodation space== ...loading of the mobile salt resulted in some syndepositional subsidence and accommodation of the ''Glob alt'' sand-prone [[isochron]] thick. The apparent thickening
    13 KB (1,771 words) - 17:24, 5 December 2023
  • ...of sediments depends on the interaction of cycle phase and the creation of accommodation space. The sediments comprising a depositional sequence are deposited durin ...rns|progradational]] stacking pattern due to sediment supply exceeding the accommodation space. Progradation results in basinward downlapping onto the maximum flood
    8 KB (1,103 words) - 21:21, 23 February 2022
  • ...flect [[Wikipedia:Marine transgression|transgression]] from an increase in accommodation space that exceeds the sediment supply (Figure 4-22). Progradation of paras ...<ref name=ch04r68 /> These can be interpreted as sediment supply exceeding accommodation space, forcing progradation but with subsidence exceeding the relative chan
    15 KB (2,029 words) - 21:21, 23 February 2022
  • Because rates of sediment accumulation and areas of accommodation space vary, thickness and areal extent are of little use in establishing th
    7 KB (982 words) - 21:20, 23 February 2022
  • Accommodation rates are high during transgressive–early highstand episodes of sea level
    8 KB (1,184 words) - 20:44, 4 February 2022
  • ...ation]] pulses in the active margin of Gondwana were the major controls of accommodation space variation rates. The orogenic apex matches periods of accelerated dev ...ine-Chilean Andes: Tectonics, v. 5, n0. 6, p. 855–880</ref> which provided accommodation space for the of the first unit: the Rio Ivaí supersequence.
    22 KB (3,382 words) - 19:52, 4 January 2024
  • ...l. This is interpreted as sediment accumulation rate exceeding the rate of accommodation space formation by sea level rise plus basin subsidence. The consequence is
    11 KB (1,548 words) - 16:58, 24 February 2022
  • ...gesting relative rise of sea level (with consistent widespread increase in accommodation space). Observations of [http://wiki.seg.org/wiki/Dictionary:Seismic_facies
    15 KB (2,070 words) - 20:34, 7 July 2016
  • ...eum industry. They account for relative and eustatic sea level changes and accommodation space left for new sediments. Likewise, growth faults are connected directl
    14 KB (2,168 words) - 21:31, 13 March 2019
  • ...theories of structural geology generally relate the formation of folds to accommodation on irregular fault surfaces.<ref name=Hamblin_1965>Hamblin, W. K., 1965, [h
    20 KB (2,865 words) - 19:24, 19 January 2022
  • ...n ocean or the failure of the rift zone. In tectonic strike-slip settings, accommodation spaces occur as transpresional, transtensional or transrotational basins ac
    24 KB (3,689 words) - 17:46, 18 April 2019
  • ...s occurring long before the formation of the Zagros folds, and the late re-accommodation of part of the gas in anticlines that resulted from the Late Miocene to Pli
    27 KB (3,901 words) - 13:51, 26 January 2017
  • .... These highlands also contributed to deformational loading, providing the accommodation space for accumulating sediments within the subsiding basin. ...rvasive. Here, during Alleghenian thrusting, much of the early and basinal accommodation was provided by the [[deformation]] of the Salina and then to a lesser exte
    89 KB (13,415 words) - 19:16, 16 January 2024
  • ...and 2, representing the main landing zones). Once the sediment filled the accommodation space, the hydrodynamic processes (e.g., tides, waves, currents, gravity fl
    77 KB (11,201 words) - 20:07, 15 January 2024

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