Devono-Mississippian sedimentary environments at the type Antler orogen at Battle Mountain, Nevada
Conference
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6461694
The Antler orogeny is a textbook example of a Paleozoic mountain building and crustal shortening event in western North America. A relatively complex geologic history of the type Antler at Battle Mountain, Nevada, is interpreted as distinct thrust plates of Lower Cambrian Scott Canyon Formation, Upper Cambrian Harmony Sandstone, and Ordovician Valmy Formation, overlain unconformably by the Middle Pennsylvanian Battle Formation. Mississippian crustal deformation and emplacement of the Roberts Mountain thrust have previously been thought to characterize the Antler orogen. Detailed sedimentology studies of the Scott Canyon and Harmony, and the relationship with the overlying Battle Formation at the type section of the Antler orogeny, cast doubt on the previously accepted geologic history. The Scott Canyon is an interbedded sequence of pillow basalts, Late Devonian radiolarian cherts, and mudstone debris flows with numerous limestone olistoliths, many containing undescribed archaeocyathid fauna. The contact of the Harmony with the Battle Formation appears channeled, but otherwise conformable, and the Battle has been interpreted as an alluvial fan facies. The paleoenvironmental interpretation of these sediments is that the Scott Canyon was deposited upon a Late Devonian active continental margin setting, with prograding fan deposits of the Harmony Sandstone, overlain by Middle Pennsylvanian fanglomerates of the Battle Formation. This conformable sequence appears to preclude any major uplift within the type Antler orogen.
- Research Organization:
- Eastern Washington Univ., Cheney (USA)
- OSTI ID:
- 6461694
- Report Number(s):
- CONF-8510489-
- Conference Information:
- Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
- Country of Publication:
- United States
- Language:
- English
Similar Records
Thrust segment from the Antler orogeny identified north of the Snake River Plain, south-central Idaho
Paleozoic stratigraphy and tectonics in northernmost Nevada: Implications for the nature of the Antler orogeny
Northwest vergent folding in the Harmony Formation, north central Nevada: Lower Paleozoic tectonics revisited
Conference
·
Wed Mar 31 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5098129
Paleozoic stratigraphy and tectonics in northernmost Nevada: Implications for the nature of the Antler orogeny
Conference
·
Wed Mar 31 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5022951
Northwest vergent folding in the Harmony Formation, north central Nevada: Lower Paleozoic tectonics revisited
Conference
·
Wed Mar 31 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5100222
Related Subjects
58 GEOSCIENCES
580201* -- Geophysics-- Seismology & Tectonics-- (1980-1989)
580300 -- Mineralogy
Petrology
& Rock Mechanics-- (-1989)
BASALT
DEPOSITION
DEVONIAN PERIOD
FEDERAL REGION IX
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGIC HISTORY
GEOLOGY
IGNEOUS ROCKS
LITHOLOGY
MISSISSIPPIAN PERIOD
MOUNTAINS
NEVADA
NORTH AMERICA
OROGENESIS
PALEOZOIC ERA
PETROLOGY
ROCKS
SEDIMENTARY ROCKS
TECTONICS
USA
VOLCANIC ROCKS
580201* -- Geophysics-- Seismology & Tectonics-- (1980-1989)
580300 -- Mineralogy
Petrology
& Rock Mechanics-- (-1989)
BASALT
DEPOSITION
DEVONIAN PERIOD
FEDERAL REGION IX
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGIC HISTORY
GEOLOGY
IGNEOUS ROCKS
LITHOLOGY
MISSISSIPPIAN PERIOD
MOUNTAINS
NEVADA
NORTH AMERICA
OROGENESIS
PALEOZOIC ERA
PETROLOGY
ROCKS
SEDIMENTARY ROCKS
TECTONICS
USA
VOLCANIC ROCKS