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• W91654092 abstract "The Early to Middle Cambrian Carrara Formation includes two partial third-order sequences and three complete third-order sequences. The first partial sequence, composed of the basal two Carrara Formation members, is completed by the addition of the underlying Early Cambrian Zabriskie Quartzite. The middle six Carrara Formation members compose three complete sequences. The second partial sequence incorporates the uppermost Carrara Formation member and is completed by the addition of the basal part of the overlying Middle to Late Cambrian Bonanza King Formation.These third-order sequences consist of a basal siliciclastic portion and an upper carbonate portion, corresponding to Grand Cycles. Minimal evidence of erosion or exposure along Carrara Formation sequence boundaries indicates that they are Type 2 unconformities. Carrara Formation Grand Cycles allow sequence-stratigraphic modeling of a depositional system with two sediment sources that respond differently to changes in accommodation. Nearshore marine and non-marine, fine-grained siliciclastics prograded basinward from the craton and were deposited in shelf-margin systems tracts or by-passed the shelf if little to no accommodation space was available on the shelf. In either case, subsequent siliciclastic deposition was retrogradational forming transgressive systems tracts. Siliciclastics were distributed widely in shelf-margin and early transgressive systems tracts, but were not able to maintain wide distribution during later transgressive and highstand systems tracts. Subtidal and peritidal carbonates prograded cratonward from an offshore carbonate bank and were deposited in transgressive and highstand systems tracts. The carbonate bank experienced decreased sediment production rates during accumulation of the shelf-margin systems tract and ever-increasing rates during accumulation of the transgressive and highstand systems tracts. This interpretation of shelf-margin systems tract siliciclastics and highstand systems tract carbonates differs from some interpretations of Grand Cycles in the southern Canadian Rockies. Shelf-margin systems tracts in most (common) Grand Cycles are either very thin and difficult to distinguish from transgressive systems tracts or are missing entirely. In anomalous Grand Cycles, the shelf-margin systems tract is well developed with intertidal to supratidal lithofacies. Both the common and the anomalous types of Grand Cycles are present in the Carrara Formation." @default.
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• W91654092 date "1995-01-01" @default.
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• W91654092 title "Sequence-Stratigraphy of Early-Middle Cambrian Grand Cycles in the Carrara Formation, Southwest Basin and Range, California and Nevada" @default.
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• W91654092 doi "https://doi.org/10.1007/978-94-015-8583-5_10" @default.
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