Upper Cretaceous tempestites in Mancos and Mesaverde formations - a model for shallow-shelf sandstone reservoirs
Conference
·
· Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6828731
The sedimentologic features that characterize the pinchout of Mesaverde Group sandstones into the Mancos Shale are spectacularly exposed along the Book Cliffs in east-central Utah. We traced the upper portion of the Blackhawk Formation of the Mesaverde Group as it graded into Mancos Shale, and observed textural trends and sedimentary structures which match those that are observed in modern tempestites formed on siliciclastic shelves. The upper-most portion of the Mancos consists of upward coarsening sequences of mudrocks that exhibit large-scale scour and fill structures and slump features. Above the Mancos, sandstone units of the Blackhawk Formation commonly display sole marks within partial Bouma sequences, and sandstone units higher in the section consist of hummocky cross-strata sets grading up to asymmetrical ripple sets. These units represent tempestites that were deposited by wave-modulated, wind-driven currents generated by storms as they crossed the mud-dominated western shelf of the Cretaceous seaway. Tempestite sequences can be traced up depositional dip into tongues of prograding shoreface sandstones. The moving of large quantities of sand and silt-sized siliciclastics out onto mud-dominated shelf environments appears to be a major process along margins of epicontinental seaways. We believe that these movements are storm-generated, and that sands, which later became petroleum reservoirs, were placed in shelf settings in the form of tempestites. In particular, many petroleum-bearing Cretaceous sandstones in Wyoming, Colorado, and Utah that have previously been interpreted as either deltaic-coastal bars or ''shallow-water turbidites,'' are actually tempestites.
- Research Organization:
- Univ. of Iowa, Iowa City
- OSTI ID:
- 6828731
- Report Number(s):
- CONF-8405216-
- Conference Information:
- Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 68:4
- Country of Publication:
- United States
- Language:
- English
Similar Records
Depositional model for a muddy shelf-sand complex and their relationship to reservoir development: Mancos B interval of Late Cretaceous Mancos Shale, northwest Colorado and northeast Utah
Deltaic coals of the ferron sandstone member of the Mancos shale: predictive model for cretaceous coals of the western interior
Genetic sequences and unconformities in shallow marine to fluvial depositional systems, Mesaverde Group, north-central Wyoming
Conference
·
Fri May 01 00:00:00 EDT 1987
· AAPG Bull.; (United States)
·
OSTI ID:6311278
Deltaic coals of the ferron sandstone member of the Mancos shale: predictive model for cretaceous coals of the western interior
Conference
·
Mon Dec 31 23:00:00 EST 1979
· Resour. Ser. - Colo. Geol. Surv.; (United States)
·
OSTI ID:5218294
Genetic sequences and unconformities in shallow marine to fluvial depositional systems, Mesaverde Group, north-central Wyoming
Conference
·
Thu Feb 28 23:00:00 EST 1991
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
·
OSTI ID:5529064
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
COLORADO
CRETACEOUS PERIOD
FEDERAL REGION VIII
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FORMATIONS
MESOZOIC ERA
MINERAL RESOURCES
NORTH AMERICA
PETROLEUM DEPOSITS
RESERVOIR ROCK
RESOURCES
ROCKS
SANDSTONES
SEDIMENTARY ROCKS
SEDIMENTATION
SHALES
USA
UTAH
WYOMING
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
COLORADO
CRETACEOUS PERIOD
FEDERAL REGION VIII
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FORMATIONS
MESOZOIC ERA
MINERAL RESOURCES
NORTH AMERICA
PETROLEUM DEPOSITS
RESERVOIR ROCK
RESOURCES
ROCKS
SANDSTONES
SEDIMENTARY ROCKS
SEDIMENTATION
SHALES
USA
UTAH
WYOMING