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Commonly accepted concept concerning the lower Paleozoic stratigraphy of northern Nevada are based on the assumption that the deep-water aspects of Ordovician to Devonian siliceous strata are due to their origin is a distant oceanic environment, and their presence where we find them is due to tectonic emplacement by the Roberts Mountain thrust.
Commonly accepted concept concerning the lower Paleozoic stratigraphy of northern Nevada are based on the assumption that the deep-water aspects of Ordovician to Devonian siliceous strata are due to their origin is a distant oceanic environment, and their presence where we find them is due to tectonic emplacement by the Roberts Mountain thrust.
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