Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Depositional environment of Lower Permian Stone Corral Formation

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5785687

The Lower Permian Stone Corral Formation is a 5-8 ft thick unit of dolomitic limestone and shale in a sequence of red beds that crops out in south-central Kansas. It forms a good stratigraphic marker bed in the subsurface, where it consists mainly of anhydrite (the Cimmaron anhydrite) up to 100 ft thick. At outcrop, the formation is weathered and consists of 2 interfingering facies - a crinoidal-echinoidal grainstone (in the north) and a laminated mudstone (in the south). Both the grainstone and mudstone exhibit diagenetic alteration. The grainstone is composed of well-rounded allochems of crinoid and echinoid fragments with scattered ooids, sponge spicules, peloids, and possible foraminifers and ostracods. Layers of sponge spicules alternate with peloid or ooid layers. The mudstone facies has a clotted texture and has laminations defined by the occurrence of fenestral fabric and peloids. Dolomite occurring in the Stone Corral Formation is of secondary origin. The grainstone is interpreted as being lagoonal in origin, whereas the mudstone facies is interpreted as supratidal. The grumous (clotted) texture may indicate phreatic diagenesis. The absence of anhydrite on outcrop, where it was presumably leached by surface waters leaving the less soluble dolomite, is additional evidence for a regional disconformity above the unit on the eastern side of a large, shallow, evaporitic basin.

Research Organization:
Wichita State Univ., KS
OSTI ID:
5785687
Report Number(s):
CONF-850322-
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Vol. 69:2; ISSN AAPGB
Country of Publication:
United States
Language:
English

Similar Records

Controls on porosity development in the Devonian Reservoir at Dolarhide Field
Conference · Tue May 01 00:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA) · OSTI ID:6916668

Storm deposits (tempestites) in Ordovician cratonic carbonates (Arbuckle Group, south-central Oklahoma)
Conference · Mon Feb 28 23:00:00 EST 1983 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6436765

Lagoon and tidal flat sedimentation of the Upper Devonian Nisku Formation in southern Alberta
Conference · Sat Jun 01 00:00:00 EDT 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:5791909