By Andrew D. Miall, Noel Tyler
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Additional 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)
Example text
Foreseldap dtrectianu show a wide spread (senthwest to east-southeast, some ta the west) with a mean of 189' (Ftg. 20). 13 . -. --- - (Ftg. 20). These show shapes that range from tight erricentie dunes lo bread feaenrex. F5 ix aniqne in showing n erescentic shape marked by grainflow sleuth thai yield lalerally to small-scale coasts )Ftgs. 2A, 20, 21). Restoration of these subsets on a stereonrt (Rabiar and Hunier, 1903) show thai the superimposed dunes migrated exactly alongxlope lathe northeast (Fig.
A7-a was deposited on ths then lowest part of the western side of the urea; A7-b shows an saslwasl shift again to fill the eastern part of the depression. AO (not shown on Fig. 8) is a blanket deposit that completed lulling of the origtnat J-2 depreeaon, at least as the study esscrep. At-b tannes be correlated directly with any other amt, but in terms of elseatirn it represents an erosional rsmnast of AO. Fereset dip dsreetians collectively for the 'A' complsn span the compass (Fig. 8). With the sncepltan of A7-b, however, strata are ripple laminas and their Orientation thaws rosgbly the drposisional slope, bss not necessarily ripple migration or paleowind direction (Hunter, 1977).
A similar red bref oecnrs on the comer of Ihr sonde and sonlbwest walls (Fig 2B, C). flltrpreeatioo One of the most difftcstlt interpretations Io make foe an cellan seqncnce, defined by foresets S/ALE SLIP FACE especially on the outcrop scale, is whether a 'eonlianonu' surface represents a snper cnr! order bonnding sserface eesnitirsg from dnne/draa migration and representing the inlerdnatr floor. Discstssion of the criteria foe distinguishing the Iwo types of surfaces, none of which are preseettly considered entirely 'fool-proof', is presented al the end of dee papee, but clearly the alternate interpretations are fondamental.
