Similarities between third and fourth-order stratigraphic sequences: An example from the Permian Upper San Andres: Last Chance Canyon, Guadalupe Mountains, New Mexico

Conference · Tue May 01 04:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA)

OSTI ID:6637764

Sonnenfeld, M D ^[1]

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1. Colorado School of Mines, Golden (USA)

The upper San Andres/Cherry Canyon tongue in Last Chance constitutes a seismic-scale, unconformity bounded (third-order) depositional sequence containing mixed carbonate and siliciclastic lithologies deposited in intertidal through toe-of-slope environments. This sequence is composed of more than 12 clinoform packages that are smaller scale , higher frequency (fourth-order) depositional units or parasequences. Although shelf parasequences are asymmetric because flooding surfaces are coincident with maximum regressive surfaces, slope parasequences are relatively symmetric because transgressive deposits separate these two key surfaces. Slope parasequences within the highstand systems tract have bounding surfaces, stratal geometries, facies distributions, and siliciclastic/carbonate interrelationships that show similarities, independent of scale, to the lowstand, transgressive, and highstand systems tracts constituting the third-order sequence. Erosional surfaces and intermittent turbidite-filled channels form the basal portion of slope parasequences. Waning rates of siliciclastic sedimentation from suspension resulted in a basinally restricted, bioturbated sandstone wedge. Bedding planes within the wedge onlap the underlying parasequence boundary. These fourth-order geometries are similar to those of the third-order lowstand through transgressive systems tracts. The sandy wedge is capped by a transgressive surface. This surface is sporadically colonized by sponge-brachiopod communities, which are fourth-order analogs to the larger crinoid-bryozoan bioherms and brachiopod-sponge reefs developed on the third-order maximum flooding surface. Prograding fusulinid shoals downlap the fourth-order wedge, have fourth- and fifth-order toplap surfaces, and may be capped by regressive shelf sands. This mixed lithology package is a fourth-order analog to the third-order highstand systems tract.

• OSTI ID: 6637764
• Report Number(s): CONF-900605--
• Conference Information: Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Journal Volume: 74:5
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
580000* -- Geosciences
CARBONATE ROCKS
DEPOSITION
FEDERAL REGION VI
FOSSILS
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGY
LITHOLOGY
NEW MEXICO
NORTH AMERICA
PALEOZOIC ERA
PERMIAN PERIOD
ROCKS
SANDSTONES
SEDIMENTARY ROCKS
STRATIGRAPHY
USA