Tidal Deposits pp 145-151 | Cite as

Tidalites in the Eureka Quartzite (Ordovician), Eastern California and Nevada

  • George deVries Klein

Abstract

The Eureka Quartzite (Ordovician) occurs as a well-exposed, cliff-forming sandstone in the Basin-and-Range Province of eastern California and Nevada over an area in excess of 200,000 sq km2 and ranges in thickness from 50 to 150 meters (Ross, 1964; Webb, 1956). Selected outcrops (Fig. 17-1; Table 17-1) contain a variety of sedimentary and biogenic structures indicating the Eureka Quartzite to be a tidalite (cf. Klein, 1971; Swett et al., 1971). The Eureka is sandwiched between the intertidal carbonates of the Ely Springs Dolomite (Chamberlin, 1975) and the Pogonip Group (Stricker, 1973). The general stratigraphic relationships are summarized in Figure 17-2.

Keywords

Quartz Sandstone Petrol Dolomite Stratigraphy 

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References

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© Springer-Verlag New York Inc. 1975

Authors and Affiliations

  • George deVries Klein

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