Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

The Mississippian Antler foreland and continental margin in southern Nevada: The Eleana Formation reinterpreted

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:5171482
;  [1]
  1. Univ. of Nevada, Reno (United States)

Rocks mapped as the Mississippian Eleana Formation at the type locality on the Nevada Test Site appear to comprise two completely different, but coeval, sedimentary units. In the Eleana Range (Western Eleana Formation), the strata are siliciclastic and carbonate turbidites of Mississippian age. From immediately east of the Eleana Range to Syncline Ridge (Eastern Eleana Formation), the strata are Devonian-Mississippian mudstone and quartzite conformably overlying Devonian limestone and underlying Pennsylvanian limestone. Although the contact between the two sedimentary packages is not exposed, small-scale structures document an east-dipping fault contact and reverse motion. Sandstone petrography and stratigraphic considerations support the age data in identifying two separate Mississippian units. Sandstones from the Western Eleana are chert litharenites with significant amount of feldspar and both volcanic and sedimentary lithic grains. These rocks are interpreted to be a submarine fan deposit; southwest-directed paleocurrent indicators suggest that they were deposited in an elongate trough, filled axially from the northeast. The source of the sediments was the antler allochthon and foreland basin. The authors tentatively correlate this section with the Dale Canyon-Chainman-Diamond Peak section near Eureka, Nevada. Sandstones from the Eastern Eleana are quartz arenites with rare chert and detrital heavy minerals. These strata are tentatively interpreted to be a shallow shelf deposit, with sediments derived from the continent to the east. They tentatively correlate this section with the Guilmette-Pilot-Scotty Wash-Chainman section of eastern Nevada. These sedimentary systems are initially separated an unknown distance across the late Paleozoic continental margin.

OSTI ID:
5171482
Report Number(s):
CONF-9103128--
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (United States), Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Vol. 75:2; ISSN AABUD; ISSN 0149-1423
Country of Publication:
United States
Language:
English

Similar Records

Geometry and depositional history of the southern Antler foreland basin, Eleana FM, Nevada Test Site
Conference · Wed Mar 31 23:00:00 EST 1993 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:5023782

Stratigraphy and petroleum potential of the Mississippian Chainman Shale and Diamond Peak Formation, east-central Nevada
Conference · Sat Jun 01 00:00:00 EDT 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:5982597

Paleogeographic setting of the Late Devonian to Early Mississippian Antler foreland, eastern Nevada and western Utah
Conference · Thu Jan 31 23:00:00 EST 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:5200292