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This document describes swaley cross-stratification observed in medium to coarse sandstone of the Proterozoic Kansapathar Formation in central India. Swaley cross-strata consist of nested elliptical swales that are commonly symmetrically filled. They occur alongside trough cross-strata. The spatial distribution and orientations of the different cross-strata types relate to shoreline proximity and wave/current interactions during deposition. The coarse grain size and steeply dipping laminae of the swaley cro

Author

Andreyriv Diaz

Language

EN