Cyclic platform dolomites of Devonian Jefferson Formation, Montana and Idaho
Conference
·
· Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5376956
Preliminary field study indicates that the Devonian Jefferson Formation in southwestern Montana and adjacent parts of Idaho consists of cyclic sequences of shallow marine platformal dolomites that grade basinward into slope sediments deposited on a steepened carbonate ramp. Individual shallowing-upward, platformal cycles are 25 to < 1 m (82 to 3 ft) thick and, from top to bottom, consist of: solution-collapse breccia caps; cryptalgal dolomudstone; rare ooid dolograinstone; thin-bedded Amphipora dolowackestone; sucrosic dolostones with abundant lenticular to domal stromatoporoids; thin-bedded, fine-grained, shaly dolostones with closely spaced hardgrounds that grade upward into burrow-homogenized, irregularly bedded dolostones. Thinner cycles (< 5 m or 16 ft thick) contain fewer basal lithologies and typically consist only of cryptalgal dolomudstone with breccia caps. The 1 to 25-m thick cycles comprise larger scale sequences (30-60 m or 100-200 ft thick), in which smaller scale cycles become progressively thinner toward the top of large-scale sequences. These shallowing-upward carbonate cycles probably formed in response to glacio-eustatic sea level fluctuations. Current estimates for the time span represented by the Jefferson formation (9 m.y.), divided by the number of shallowing-upward cycles, indicate that each cycle represents an average time span of 0.6 to 1.0 m.y.. This time span suggests that either: (1) average sedimentation rates were unrealistically slow during deposition of each cycle (< 0.1-3 cm/1000 years); (2) breccia caps represent long periods of subaerial exposure (> 0.5 to about 0.2 m.y.); or (3) the Jefferson Formation was deposited during a much shorter time span than previously thought.
- Research Organization:
- Washington State Univ., Pullman
- OSTI ID:
- 5376956
- Report Number(s):
- CONF-860624-
- Conference Information:
- Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:5
- Country of Publication:
- United States
- Language:
- English
Similar Records
Cyclic platform dolomites and platform-to-basin transition of Jefferson Formation (Frasnian), southwest Montana and east-central Idaho
Outcrop analog for cyclic-shelf reservoirs, San Andres formation of Permian basin: Stratigraphic framework, permeability distribution, geostatistics, and fluid-flow modeling
Facies and diagenesis of Grayburg-San Andres dolomite reservoirs, Central Basin platform, Permian basin
Conference
·
Sat Aug 01 00:00:00 EDT 1987
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:5696909
Outcrop analog for cyclic-shelf reservoirs, San Andres formation of Permian basin: Stratigraphic framework, permeability distribution, geostatistics, and fluid-flow modeling
Journal Article
·
Fri Dec 31 23:00:00 EST 1993
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
·
OSTI ID:7134496
Facies and diagenesis of Grayburg-San Andres dolomite reservoirs, Central Basin platform, Permian basin
Conference
·
Thu May 01 00:00:00 EDT 1986
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:5167643
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USA