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Oronto Group: a petroliferous rift-fill sequence of the Mid-Continent rift system

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5378745
The Oronto Group of northern Michigan and Wisconsin includes the Copper Harbor Conglomerate, Nonesuch Formation, and Freda sandstone. These formations are part of a volcaniclastic sequence created in response to the formation of the Mid-Continent rift system. Although intercalated volcanics are found in the lower one-third of the Oronto Group, a sedimentary depositional regime was dominant. Although complex in detail, an overall depositional model for the Oronto Group is one of relatively simple transgressive-regressive relationships between alluvial, lacustrine, and fluvial environments. Important aspects of such a model include (1) all Oronto Group formations are genetically related; (2) the intervening Nonesuch Formation is, at least in part, equivalent in age to the upper Copper Harbor and the lower Freda; and (3) such rift settings can have significant hydrocarbon potential.
Research Organization:
Placid Oil Co., Dallas, TX
OSTI ID:
5378745
Report Number(s):
CONF-860624-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:5
Country of Publication:
United States
Language:
English

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