Comparative petrology of Tertiary sandstones of southern Piceance Creek Basin, Colorado
Lacustrine and fluvial sandstones of the Wasatch and Green River Formations are described as they outcrop at several localities along the southern margin of the Piceance Creek basin. The description combined with petrographic analyses of thin-section samples provide a basis for determining the provenance of the sand, as well as crude comparison of compositional and textural features that resulted from differences in depositional processes. The sandstones in marginal lacustrine settings in the Wasatch and Green River Formations are proven reservoirs for significant hydrocarbon reserves in the Uinta and Piceance Creek basins. (JMT)
Tertiary geology and oil-shale resources of the Piceance Creek basin between the Colorado and White Rivers, northwestern Colorado
From introduction: The greatest known potential oil resource in the world occurs in the oil shale of the Green River formation, and the richest and thickest deposits occur within the area of this report. The purpose of this investigation was to obtain data on the stratigraphic distribution and areal extent of the oil-shale beds and to estimate the potential oil resources in the area.
Eimeria odocoilei n. sp. from the mule deer Odocoileus h. hemionus in Washington.
SYNOPSIS. Eimeria odocoilei n. sp. is described from feces of a mule deer Odocoileus h. hemionus in Washington. Its oocysts are 26 to 28 by 22 to 26 μ. It is the second species of Eimeria described from this host.