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• W2079908213 abstract "The evolution and controls on lithofacies distribution in ancient fluvio-paralic successions have been the focus of many studies. However, the evolution of ancient continental-scale fluvio-paralic depositional systems is not well documented due to a lack of suitable outcropping or subcropping examples. Features inherent to continental-scale fluvial systems, such as low overall gradients and large distances separating source from sink are likely to have a strong influence on vertical and lateral lithofacies evolution. During the Early Cretaceous a vast fluvio-paralic system drained the interior of the north Gondwana continent, terminating at approximately the present day coastline of North African/Saharan platform, and extending for > 1500 km across the margin. In the Murzuq Basin, ~ 600 km from the shelf edge, extensive outcrops of Lower Cretaceous (named the Messak Fm) comprise ~ 300 m of fluvio-paralic sediments. Correlation with more distal equivalent outcrops on the northern margin of the Ghadames Basin presents an excellent opportunity to assess facies development of a large-scale continental system, and clearly illustrates the effects of limited accommodation availability. For the first time, we identify evidence of marine influence in the Murzuq Basin during the early Cretaceous and interpret this as the record of transgressions associated with the regionally well-documented early Aptian sea level rise. The distribution of fluvial and paralic facies is interpreted to be controlled by a combination of limited accommodation availability, repeated relative sea level rises, and autocyclic fluvial processes. Relative sea level rises were able to rapidly inundate large parts of the Gondwanan margin due to the low gradient of the platform, but transgressive facies distribution and preservation were restricted due to the balance between sediment supply and limited long-term accommodation availability. Thus, while relative sea level exerts a strong influence in such a setting, marine-influenced deposits are likely to be relatively rare. The Messak Fm provides a clear example of how sediments preserved by a large-scale low-gradient fluvial system do not necessarily reflect the relative balance of depositional controls." @default.
• W2079908213 created "2016-06-24" @default.
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• W2079908213 date "2014-04-01" @default.
• W2079908213 modified "2023-10-18" @default.
• W2079908213 title "Controls on facies evolution in low accommodation, continental-scale fluvio-paralic systems (Messak Fm, SW Libya)" @default.
• W2079908213 cites W1516351198 @default.
• W2079908213 cites W1857814390 @default.
• W2079908213 cites W1970381583 @default.
• W2079908213 cites W1970440610 @default.
• W2079908213 cites W1971320400 @default.
• W2079908213 cites W1972364808 @default.
• W2079908213 cites W1974782268 @default.
• W2079908213 cites W1980642926 @default.
• W2079908213 cites W1983134347 @default.
• W2079908213 cites W1983489601 @default.
• W2079908213 cites W1986285805 @default.
• W2079908213 cites W1987000607 @default.
• W2079908213 cites W1989195581 @default.
• W2079908213 cites W1998209963 @default.
• W2079908213 cites W2000417941 @default.
• W2079908213 cites W2005282721 @default.
• W2079908213 cites W2008793628 @default.
• W2079908213 cites W2017774024 @default.
• W2079908213 cites W2019616775 @default.
• W2079908213 cites W2019663851 @default.
• W2079908213 cites W2020880676 @default.
• W2079908213 cites W2022830090 @default.
• W2079908213 cites W2024188615 @default.
• W2079908213 cites W2026094446 @default.
• W2079908213 cites W2029390808 @default.
• W2079908213 cites W2036964633 @default.
• W2079908213 cites W2038734492 @default.
• W2079908213 cites W2041577650 @default.
• W2079908213 cites W2047097742 @default.
• W2079908213 cites W2048215676 @default.
• W2079908213 cites W2049483750 @default.
• W2079908213 cites W2051854135 @default.
• W2079908213 cites W2053619286 @default.
• W2079908213 cites W2057403102 @default.
• W2079908213 cites W2060979021 @default.
• W2079908213 cites W2065108022 @default.
• W2079908213 cites W2067628429 @default.
• W2079908213 cites W2068724623 @default.
• W2079908213 cites W2069232301 @default.
• W2079908213 cites W2080201030 @default.
• W2079908213 cites W2080591287 @default.
• W2079908213 cites W2082232448 @default.
• W2079908213 cites W2089248374 @default.
• W2079908213 cites W2089892750 @default.
• W2079908213 cites W2093119790 @default.
• W2079908213 cites W2094581504 @default.
• W2079908213 cites W2095900855 @default.
• W2079908213 cites W2098762071 @default.
• W2079908213 cites W2099581206 @default.
• W2079908213 cites W2101644114 @default.
• W2079908213 cites W2105612923 @default.
• W2079908213 cites W2107190049 @default.
• W2079908213 cites W2108998966 @default.
• W2079908213 cites W2109107132 @default.
• W2079908213 cites W2118432836 @default.
• W2079908213 cites W2118973073 @default.
• W2079908213 cites W2122503603 @default.
• W2079908213 cites W2124565668 @default.
• W2079908213 cites W2125493971 @default.
• W2079908213 cites W2130432031 @default.
• W2079908213 cites W2131616329 @default.
• W2079908213 cites W2134806919 @default.
• W2079908213 cites W2151346749 @default.
• W2079908213 cites W2156869239 @default.
• W2079908213 cites W2158018179 @default.
• W2079908213 cites W2167948308 @default.
• W2079908213 cites W2177010457 @default.
• W2079908213 cites W2305998502 @default.
• W2079908213 cites W2322898176 @default.
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• W2079908213 doi "https://doi.org/10.1016/j.sedgeo.2014.01.007" @default.
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