By Andrew D. Miall, Noel Tyler
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Extra info for The Three-Dimensional Facies Architecture of Terrigenous Clastic Sediments and Its Implications for Hydrocarbon Discovery and Recovery (SEPM Concepts in Sedimentology & Paleontology 3)
Sample text
The aniqaeness of this set wslhin the 'A' comptes, however, suggests that boeckan dones f ormed but one component of the overall seeing. Its presence dons suggest, however, that the overall regime was snob that transverse dunes without phaths could form, and thaI the sets of wind-ripple laminav arenal plintb deposits. The personen of sets, especially the better organized trosgh sets of A8 to 10, dons demand a becfform origin. Zibars or similar low-relief bedforms that tack sliplaces and consist of wind-tippte stenosners (Nielson and Kocueek, 1986) seem most likely here, especially considering the coarser grain size.
Complex m which sufficient good data exist. Esco collectively, sets below 08 define a narrow range of curvature (maximum for a single set is 48' for 04, 54' collectively). Mean faresel dip direction is toward t60'. Exposures exist on the south wall where exhumed ripples are present on f oreset faces; these arr migrating alongslope lo the W. Isrerprerarion Angle of climb for sets in the 'D' complus cao be oslimulud where sels overlie other 'D' sols, and are continuous in the migrasion direction.
A reprouve pallern of cross-strata may be present in mont of the 'A' templen, but is most distinct in the wind-tippte laminas of AS, Ab, A8 and AtO, and in alternating ripple and geninflow strata of A7-b. ta AtO, red, finer graineil laminas alternate with white, coarser praised laminas in paekagss measuring 20-38 cm in the general migration direetton, gsvmg the unit a 'candy-striped' appearance (Fig. 7A, B). In A7-b, layers al grainflow are separated by layers of wind-ripple laminas forming repetitive packages 88cm thick.