Abstract
Ordovician and Silurian rocks of the carbonate (eastern) assemblage are exposed in a window in Ordovician rocks of the siliceous and volcanic (western) assemblage of the northern part of the Toquima Range, central Nevada. The window exposes rock beneath part of the Roberts Mountains thrust, and covers an area of approximately 20 sq mi. The strata within the window resemble, and are correlated with, rocks exposed farther south in the central part of the Toquima Range and on the east in the Antelope Valley region.
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