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Paper No. 25
Presentation Time: 8:00 AM-6:00 PM


KHANDAKER, Nazrul I.1, VONDRA, Carl F.2, SEIFERT, Karl E.3, SHAMI, Malek1, CARDINALE, Rochelle4 and CHATURGAN, Thakur5, (1)Geology Discipline, Earth and Physical Sciences, York College Of CUNY, 94-20, Guy R. Brewer Blvd, Jamaica, NY 11451, (2)Geological and Atmospheric Sciences, Iowa State University, Ames, IA 50011, (3)Dept. of Geological & Atmospheric Sciences, Iowa State University, 4618 Dover Dr, Ames, IA 50014, (4)Iowa Dept. of Natural Resources (DNR), Wallace Building, 502 East Ninth Street, Des Moines, IA 50319, (5)Brown and Caldwell, 110 Commerce Drive, Allendale, NJ 07401,

The Peay bentonites belong to the basal Frontier Formation (Bighorn Basin, north-central Wyoming), primarily outcrop in the Bighorn Basin, rest on an extensively bioturbated sandstone unit, the Peay Sandstone, and are generally the thinner bentonitic unit. Beds of very light gray to greenish gray bentonite are also abundant in the lower Frontier units between Kaycee and Mayoworth (Powder River Basin) and are very rarely as much as 3 m thick. Bentonite occurs within the interstratified shale, sandstone, and siltstone sequences of the lower Frontier unit throughout much of the southwestern Powder River Basin. The purpose of this study is to use field, geochemical, petrological, and zircon morphology data to establish a chemical fingerprint of the original ash composition and to provide a tectonic and provenance interpretation. Peay units show distinct mineralogy consisting of quartz, kaolinite, illite, smectite, mixed-layer clays, K-feldspar, plagioclase, chlorite, calcite, and dolomite. Fairly uniform concentrations of SiO2, Na2O, CaO, MgO, Al2O3, Zr, Ti, Nb, and Ni have been noted in the Peay bentonites, such consistent concentrations of these elements in Peay bentonite samples imply that they have not been strongly modified by secondary processes. Peay bentonite samples show a consistent geochemical trend towards the alkali basalt field. On the basis of the similarity in gross stratigraphic development, feldspar compositions and trace element geochemistry, the source for the Peay bentonites is most likely located in the same general area. This is further supported by the presence of Ti-rich augite and the distinctive zircon morphology. The uniformity of composition and similarity in stratigraphic development of Peay bentonites over the region studied argues strongly against the contemporaneous involvement of several extrabasinal volcanoes. Evidence for active Cretaceous volcanism in the Idaho and in south-central Montana has been documented by Gill and Cobban, 1973. The Peay bentonites broadly correlate to the emplacement of batholiths in this region. Igneous rocks in northern Idaho and north-central Montana have yielded isotopic dates similar to those of the Peay bentonites (ca 90 Ma; Obradovich, 1993; Obradovich and Cobban 1975).

Funded by a PSC-CUNY Research Grant awarded to the author.

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