2014
DOI: 10.1007/s12517-014-1720-4
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Lithofacies of transgressive–regressive sequence on a carbonate ramp in Vindhyan basin (Proterozoic): a case of tidal-flat origin from central India

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Cited by 10 publications
(1 citation statement)
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“…The Limestone Lithofacies Association containing abundant Nummulites represents deposition during sea level rise (transgression), [40] [35] [41]. The limestone, varying from wackestone to packstone, is impure, containing sand and silt, which implies that during deposition the clastic supply from land was drastically reduced or became negligible preventing salinity dilution and inducing limestone sedimentation [41] [38] [42]. Wackestones were deposited in the lower shoreface to inner neritic conditions whereas, packstones in upper shoreface sedimentation.…”
Section: Paleobiogeographical and Paleoevironmental Implicationsmentioning
confidence: 99%
“…The Limestone Lithofacies Association containing abundant Nummulites represents deposition during sea level rise (transgression), [40] [35] [41]. The limestone, varying from wackestone to packstone, is impure, containing sand and silt, which implies that during deposition the clastic supply from land was drastically reduced or became negligible preventing salinity dilution and inducing limestone sedimentation [41] [38] [42]. Wackestones were deposited in the lower shoreface to inner neritic conditions whereas, packstones in upper shoreface sedimentation.…”
Section: Paleobiogeographical and Paleoevironmental Implicationsmentioning
confidence: 99%