DEPOSITIONAL PROCESSES AND XRF GEOCHEMISTRY OF THE UTICA SHALE WITHIN THE ORDOVICIAN OUTCROP BELT IN CENTRAL NEW YORK STATE
By annotating each sample with a lithofacies designation, vertical and lateral trends within one rock type can be investigated. For example, black fine mudstone can be isolated from thin interbedded carbonate-rich turbidite and debris flow units to track compositional changes in the detrital fraction of the background sediments. Calcium concentrations of these mudstones are higher in the Flat Creek Shale, the lower portion of the Utica Shale, than the overlying Indian Castle Shale, and decrease westward towards the craton within the Indian Castle Shale. The ratios of detrital proxies relative to Al highlight previously unidentified changes in the bulk composition of siliciclastic detritus across two disconformities within the Indian Castle Shale. This likely relates to variation in the relative contribution of sediment derived from the cratonic interior, eroded carbonate shelf, and rising orogenic wedge, as well as possible exhumation of the Adirondack Massif. The concentrations of redox sensitive proxies increase upwards throughout the Utica Shale and towards the basin center. The broad results of this study are consistent with previous interpretations, indicating that high resolution lithologic descriptions and XRF-based elemental concentration data may reveal more cryptic changes in sediment provenance and bottom-water redox conditions within the Taconic foreland basin.