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Title: A petrographic and geochemical study of the Wilkeson Sandstone, Eocene Carbonado Formation, at the quarry near Wilkeson, Washington

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5024880

The Wilkeson Sandstone is a light-gray (N 7--8), very well-indurated, fluvial, lenticular, well-sorted, medium- to coarse-grained, arkosic sandstone. Located near the northwest corner of Mount Rainier National Park, west-central Washington State, the Wilkeson Sandstone is an important key rock that was included in part of the former Wilkeson Sandstone(s)/Wilkeson Formation (Willis, 1898). Incorporated into the Eocene Carbonado Formation (Gard, 1968), it is often referenced in Puget Group geological studies. The Wilkeson Sandstone was derived from an eastern highland of plutonic, metamorphic and marine sedimentary rocks, and contains minor carbonized wood debris, and rare siltstone and mudstone clasts. The cross-bedded, subangular, bimodal, first-cycle sand grains are cemented by silica, with secondary nodules of specular hematite. The unit weathers grayish-orange (10YR 7/4) and black (N 1). In the Wilkeson quarry, the bedding strikes north 30 degrees west, and dips 53 degrees northeast. In an effort to distinguish the Wilkeson Sandstone from other sedimentation units, 120 selected samples were analyzed for 25 major and trace elements using an automated x-ray spectrometer. Petrography was done with scanning electron and polarizing light microscopes. Heavy mineral separation also was performed.

OSTI ID:
5024880
Report Number(s):
CONF-9305259-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:5; Conference: 89. annual meeting of the Cordilleran Section and the 46th annual meeting of the Rocky Mountain Section of the Geological Society of America (GSA), Reno, NV (United States), 19-21 May 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English