2011
DOI: 10.1016/j.sedgeo.2011.05.002
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Large-scale progradation, demise and rebirth of a high-relief carbonate platform (Triassic, Lombardy Southern Alps, Italy)

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Cited by 10 publications
(19 citation statements)
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“…The depositional architecture of the Lombardy platforms (Assereto & Casati, 1965;Assereto & Kendall, 1971;Jadoul et al, 1992;Berra, 2007) reflects different evolutionary stages (Berra et al, 2011): an inception stage followed by an aggradational stage with increasing water depth in the basins and a later progradational stage. The flat-topped Esino Limestone platform reaches a maximum thickness of about 800 m and rapidly pinches out basinward with steep slopes (dipping about 35°) consisting of clinostratified breccias, with a platform to basin relief that reaches about 600-700 m (Berra et al, 2011). This evolution reflects changes in accommodation space, which control the type and storage sites of the sediments produced by the carbonate factory as well as the geometry of the carbonate platform.…”
Section: Geological Settingmentioning
confidence: 99%
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“…The depositional architecture of the Lombardy platforms (Assereto & Casati, 1965;Assereto & Kendall, 1971;Jadoul et al, 1992;Berra, 2007) reflects different evolutionary stages (Berra et al, 2011): an inception stage followed by an aggradational stage with increasing water depth in the basins and a later progradational stage. The flat-topped Esino Limestone platform reaches a maximum thickness of about 800 m and rapidly pinches out basinward with steep slopes (dipping about 35°) consisting of clinostratified breccias, with a platform to basin relief that reaches about 600-700 m (Berra et al, 2011). This evolution reflects changes in accommodation space, which control the type and storage sites of the sediments produced by the carbonate factory as well as the geometry of the carbonate platform.…”
Section: Geological Settingmentioning
confidence: 99%
“…Sedimentary dikes often penetrate for several meters downwards in the underlying platform, filling paleokarst pockets and fractures with terra-rossa sediments Binda, 2010;Berra et al, 2011;Vola & Jadoul, 2014). Some major, laterally continuous red paleosols represent marker horizons in the lower and middle part of the Calcare Rosso (Vola & Jadoul, 2014).…”
Section: Type 3) Peritidal-supratidal Carbonates Affected By Multiplementioning
confidence: 99%
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