Depositional environment of the Cambro-Ordovician Rose Run Formation in northeastern Ohio, and equivalent, Gatesburg Formation in northwestern Pennsylvania
Conference
·
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:5618195
- Univ. of Akron, OH (United States)
An ideal sedimentary sequence from the Rose Run Formation consists of three facies in the following order: (1) algal laminated/stromatolite facies, (2) bioturbated dolomite facies, and (3) crossbedded sandstone facies. The algal laminated/stromatolite facies is composed of fine to very fine crystalline dolomite with laminations 2-4 cm thick. Also observed in this facies are mudcracks. The bioturbated dolomite facies is a fine to medium crystalline dolomite with an average of 10% clastic constituents such as quartz, orthoclase, microcline, and glauconite. Bioturbation in this facies ranges from slight to well with burrows 0.5-3 cm in diameter. Other structures observed include rip-up clasts, pelloids, and oncolites. The cross-bedded sandstone facies is characterized by low-angle crossbedded, fine- to coarse-grained sandstones. This sandstone has on the average 79% quartz, 12% orthoclase, 6% microcline, 1% detridal chert, and 1-2% glauconite. The heavy mineral fraction consists of tourmaline and zircon in {approximately}1% concentrations. The grains are subrounded to rounded with a size range of 0.15-0.30 mm. Sedimentary structures include rip-up clasts, current ripples, herringbone crossbedding, and herringbone imbricate rip-up clasts.
- OSTI ID:
- 5618195
- Report Number(s):
- CONF-910403--
- Conference Information:
- Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 75:3
- Country of Publication:
- United States
- Language:
- English
Similar Records
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Conference
·
Sun Feb 28 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5587745
Depositional environments of Katakturuk Dolomite and Nanook Limestone, Arctic National Wildlife Refuge, Alaska
Conference
·
Thu Dec 31 23:00:00 EST 1987
·
OSTI ID:6683146
Upper Cretaceous bioturbated fine-to-medium sands: A problem for deep-water exploration in Campos Basin, Offshore Brazil
Journal Article
·
Thu Aug 01 00:00:00 EDT 1996
· AAPG Bulletin
·
OSTI ID:421059
Related Subjects
58 GEOSCIENCES
580000* -- Geosciences
CALCITE
CAMBRIAN PERIOD
CARBONATE MINERALS
CARBONATE ROCKS
DEPOSITION
DEVELOPED COUNTRIES
DOLOMITE
FELDSPARS
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FORMATIONS
GEOLOGIC HISTORY
GEOLOGY
LITHOLOGY
MINERALOGY
MINERALS
NORTH AMERICA
OHIO
ORDOVICIAN PERIOD
OXIDE MINERALS
PALEOZOIC ERA
PENNSYLVANIA
QUARTZ
ROCKS
SANDSTONES
SEDIMENTARY ROCKS
SILICATE MINERALS
STRATIGRAPHY
TOURMALINE
USA
ZIRCON
580000* -- Geosciences
CALCITE
CAMBRIAN PERIOD
CARBONATE MINERALS
CARBONATE ROCKS
DEPOSITION
DEVELOPED COUNTRIES
DOLOMITE
FELDSPARS
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FORMATIONS
GEOLOGIC HISTORY
GEOLOGY
LITHOLOGY
MINERALOGY
MINERALS
NORTH AMERICA
OHIO
ORDOVICIAN PERIOD
OXIDE MINERALS
PALEOZOIC ERA
PENNSYLVANIA
QUARTZ
ROCKS
SANDSTONES
SEDIMENTARY ROCKS
SILICATE MINERALS
STRATIGRAPHY
TOURMALINE
USA
ZIRCON