Published 1995 as part of Memoir 64
Copyright © 1995 The American Association of Petroleum Geologists.  All Rights Reserved.
 

The upper Campanian Grassy Member of the Blackhawk Formation, Mesa Verde Group, Utah, consists of two high-frequency, unconformity-bounded sequences within the upper part of the Blackhawk Formation highstand sequence set. Incised valley-fill deposits overlie the sequence boundaries and are laterally separated by subaerially exposed interfluve areas with minor pod-like channel tributaries. There is indirect evidence of an emerging structural high which controlled the position of incised valleys and associated interfluves. Evidence for shelf erosion and subaerial exposure together with a significant basinward shift in facies tracts is indicative of Type 1 sequence boundaries. Within the Grassy Member, the degree of shelf erosion in outcrop appears far less significant than that associated with type 1 sequence boundaries described from the stratigraphically higher Desert Member and Castlegate Formation. There appears to be a hierarchy of unconformities bounding sequences within the Blackhawk Formation recording progressively larger basinward shifts of facies tracts and greater amounts of shelf incision with time. Similarly, several orders of stratal surfaces define the internal architecture of each sequence and constituent parasequences.

Valley-fill deposits consist of multistory fluvial-estuarine complexes representing lowstand and early transgressive systems tracts. Transgressive facies preserved between the subaerially exposed interfluve and maximum flooding surface usually consist of a downdip heavily bioturbated lag deposit correlatable updip with the top of a coal or swamp facies. The internal architecture of Grassy shoreface parasequences consists of stacked bedset shingles. The lateral shift in facies tracts across bedset