File:M31F14v2.jpg

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Core photographs showing stratification in an abandoned distributary fill deposit. Diameter of cores is 13 cm (5 in.). A. Clay clasts in a sand matrix found near the base of the channel. B. Highly contorted and disrupted bedding in sandy matrix in channel-fill deposits. C. Irregular bedding and burrowed structures in silty clay layers of a channel-fill deposit. D. Contorted bedding and flow rolls in sands and sandy silt deposits of the channel fill. E. High organic clays forming the uppermost part of the channel-fill deposits. Coleman, J. M., and D. B. Prior, 1981, Deltaic environments of deposition in P. A. Scholle and D. Spearing, eds., Sandstone depositional environments: AAPG Memoir 31, p. 139-178.

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current15:16, 18 August 2014Thumbnail for version as of 15:16, 18 August 20141,134 × 503 (75 KB)Molyneux (talk | contribs)Core photographs showing stratification in an abandoned distributary fill deposit. Diameter of cores is 13 cm (5 in.). A. Clay clasts in a sand matrix found near the base of the channel. B. Highly contorted and disrupted bedding in sandy matrix in chan...

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