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Bureau of Economic Geology
10100 Burnet Rd. Bldg. 130
Austin
TX
78729
US
8-5
20230613
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10100 Burnet Rd. Bldg 139
Austin
Texas
78758
US
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Lyons Sandstone Continuity
<DIV STYLE="text-align:Left;"><P STYLE="font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>The Lyons Sandstone of Leonardian age crops out along the east side of the Colorado Front Range. During the Permian, a broad sea intermittently covered an area of low relief, where sediments, including the Lyons, were deposited in environments ranging from fluvial to normal marine to hypersaline. To the west, the Lyons lies conformably on the Fountain Formation of Pennsylvanian age, and to the east the red beds of the Lyons thin, become finer grained and pinch out into a siltstone, shale, and evaporitic facies. The evaporites were accumulated in two major subbasins present in the Permian. The Alliance Basin to the north and the Sterling Basin (Lee and Bethke, 1994). The Lyons Sandstone formed as a nearshore deposit, showing evidence of both shore and eolian processes, and was deposited along a band between the emergent ancestral Rocky Mountains and the evaporite basins, as is shown in the lithofacies map prepared for the GIS data base.</SPAN></SPAN></P><DIV><DIV><P><SPAN /></P></DIV></DIV></DIV>
Continuity for Lyons Sandstone, Denver Basin, Colorado
Sloss, l., 1988. Sedimentary cover North America Craton: US. The Geology of North America D-2. Geological Society of America. The Decade of North American Geology DNAG. P189
Denver, Colorado
Denver Basin
Oklahoma
Lyons Sandstone
Denver
Colorado
Lyons Sandstone
Denver Basin
Oklahoma
Access constraints: Restriction Code: other restrictions; Other Constraints: Access constraints: None
See access and use constraints information.
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