Geological remote sensing of Palaeogene rocks in the Wind River Basin, Wyoming, USARemote sensing studies of Palaeogene sediments in the Wind River Basin (Wyoming) were used for mapping stratigraphic units, sedimentary features and facies, and structural patterns. Thematic Mapper principal component images for the central and eastern Wind River Basin along with geological investigations and spectral analyses allowed: mapping of the Fort Union, Wind River, and Wagon Bed formations (Fm) and their subunits; recognition of two subunits in the Wind River Fm, one of which can be traced for 75 km; determination of sediment source and depositional environment of units within the Wind River Fm; correlation of the Wagon Bed Fm across the basin; and apparent confirmation of different sources of volcanic debris in the western and southeastern exposures of the Wagon Bed Fm.
Krishtalka, L. (Carnegie Museum of Natural History Pittsburgh, PA, United States)
Stucky, R. K. (Carnegie Museum of Natural History Pittsburgh, PA, United States)
Redline, A. D. (Carnegie Museum of Natural History Pittsburgh, PA, United States)
Date Acquired
September 5, 2013
Publication Date
August 1, 1988
Publication Information
Publication: ESA, Proceedings of the 1988 International Geoscience and Remote Sensing Symposium (IGARSS) '88 on Remote Sensing: Moving Towards the 21st Century, Volume 2