Facies relationships in Mesa Rica Sandstone (Lower Cretaceous), Tucumcari Basin, east-central New Mexico
Conference
·
· Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:7176040
The Mesa Rica Sandstone, a Lower Cretaceous (Albian) cliff-forming unit in east-central New Mexico, represents a progradational fluvial-dominant deltaic system. On Mesa Rica, south of Conchas Lake, the formation is underlain by the marine (prodelta.) Tucumcari Shale, and is overlain by upper and lower delta-plain deposits of the Pajarito Shale. Clear facies interfingering between the Mesa Rica and Pajarito formations documents a direct genetic link between the two. Whether the Mesa Rica Sandstone lies unconformably on the Tucumcari Shale or is transitional to it is as yet unresolved. Three major sandstone bodies exist within the Mesa Rica formation, each capped by a thin (less than 2-m) mudstone interval. The two basal sandstone bodies record deposition of separate delta lobes; the bottom unit represents progradation toward the south-southeast (215/sup 0/), whereas the upper sandstone exhibits progradation toward the east-southeast (106/sup 0/). For each unit, lobe development was followed by abandonment, often marked by wave reworking. The third major sand body in the Mesa Rica overlies the lower units and records interdistributary deposition. Subenvironments recognized within the marine part of the delta include distal bar, bar front, bar crest, bar back, distributary channel, and beach. Intervening mudstones are similar in lithology to the overlying Pajarito Shale. These units grade southward from nonmarine upper delta plain, containing overbank and levee deposits, to marine-influenced lower delta plain.
- Research Organization:
- Univ. of New Mexico, Albuquerque
- OSTI ID:
- 7176040
- Report Number(s):
- CONF-8604186-
- Conference Information:
- Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:3
- Country of Publication:
- United States
- Language:
- English
Similar Records
Paleogeographic and stratigraphic constraints on Lower Cretaceous Mesa Rica delta system, east-central New Mexico
Deltaic deposits of the Upper Cretaceous Dad Sandstone Member of the Lewis Shale, south-central Wyoming
Lithostratigraphy of Shell 272-1 and 273-1 wells: implications as to depositional history of Baltimore Canyon Trough, Mid-Atlantic OCS
Conference
·
Thu May 01 00:00:00 EDT 1986
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:5168264
Deltaic deposits of the Upper Cretaceous Dad Sandstone Member of the Lewis Shale, south-central Wyoming
Journal Article
·
Wed Dec 31 23:00:00 EST 1986
· Mt. Geol.; (United States)
·
OSTI ID:5637528
Lithostratigraphy of Shell 272-1 and 273-1 wells: implications as to depositional history of Baltimore Canyon Trough, Mid-Atlantic OCS
Journal Article
·
Sat Aug 01 00:00:00 EDT 1981
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:5862477
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
CRETACEOUS PERIOD
FEDERAL REGION VI
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FORMATIONS
GEOLOGIC STRUCTURES
MESOZOIC ERA
MINERAL RESOURCES
NATURAL GAS DEPOSITS
NEW MEXICO
NORTH AMERICA
PETROLEUM DEPOSITS
RESERVOIR ROCK
RESOURCES
ROCKS
SANDSTONES
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
USA
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
CRETACEOUS PERIOD
FEDERAL REGION VI
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FORMATIONS
GEOLOGIC STRUCTURES
MESOZOIC ERA
MINERAL RESOURCES
NATURAL GAS DEPOSITS
NEW MEXICO
NORTH AMERICA
PETROLEUM DEPOSITS
RESERVOIR ROCK
RESOURCES
ROCKS
SANDSTONES
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
USA