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

Sedimentation and early sulfide diagenesis of Harmon Member

Conference · · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
OSTI ID:6376555

Pyrite is ubiquitous in the Albian Harmon Member (Peace River Formation) in concentrations from less than 0.2 to 8.5 wt. %. Petrographic observations show two distinct modes of occurrence that are stratigraphically controlled. In neritic laminated mudstone, pyrite occurs dominantly as very fine-grained (< 20 ..mu..m), disseminated framboids. In moderately bioturbated pro-delta (transition zone) mudstone and siltstone, pyrite occurs as framboidal aggregates, burrow-filling cement, and rarely as a cement in peloidal muds. The preservation of primary sedimentary structures and the absence of bioturbation in neritic mudstones indicate deposition beneath anoxic to euxinic bottom waters. Elevated C/S values may further indicate a euxinic depositional environment. Consistently low /sup 34/S//sup 32/S values indicate unrestricted availability of sulfate for bacterially mediated reduction. Excess iron (relative to stoichiometric pyrite), a lack of C/S correlation, and elevated /sup 34/S//sup 32/S values show that sulfate availability was the limiting factor in transition zone sediments. Sulfate availability was probably controlled by episodic sedimentation and bioturbation.

Research Organization:
Univ. of Calgary, Alberta (Canada)
OSTI ID:
6376555
Report Number(s):
CONF-890404-
Journal Information:
AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States), Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Vol. 73:3; ISSN AABUD
Country of Publication:
United States
Language:
English