Early Paleozoic limestones and dolomites of the shallow shelf
transitional facies belt were mapped in the southern Sulphur Spring
Range, Eureka County, Nevada. The four youngest units in the map area
are in fault contact with the Lower Devonian rocks and were probably
transported westward, along a low-angle normal fault....
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the Sevier
orogenic belt (Armstrong, 1968).
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The next major geologic event was defined by
Upper Cambrian through Middle Devonian carbonate andclastic sequences of the northern part of the Fish Creek Rangerepresent shallow-shelf sedimentation in the Cordilleranmiogeosyncline. The lower and middle Paleozoic section exposedin the northern Fish Creek Range fits well within regional facies patterns and paleogeographic reconstructions.The Upper Cambrian Dunderberg Shale was deposited in...
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Colorado Plateau (Armstrong, 1968). Sevier deformation invol-
ved large-scale eastward overthrusting in a
Paleozoic dolomites, limestones, and detrital clastic rocks
were mapped in the Bellevue Peak 15 minute quadrangle in the
southern Mahogany Hills, Nevada. Sedimentary rock units in this
area represent shallow-shelf eastern assemblage deposits.
Shallow-shelf carbonates characterized deposition from at
least Ordovician through Late Devonian time, when clastics derived
from the...