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Geologic setting of the hillabee metavolcanic complex and associated strata-bound sulfide deposits in the appalachian piedmont of alabama

Journal Article · · Econ. Geol.; (United States)
The frontal crystalline thrust sheet of the southern Appalachians in Alabama is a sequence of lower greenschist facies rocks known as the Talladega slate belt. This sequence is composed dominantly of metapelites and metasandstones, but it contains a distinctive metavolcanic complex, the Hillabee Greenstone, at the stratigraphic top. Sulfide deposits occur throughout the 170 km outcrop extent of the Hillabee. Low K tholeitic rocks constitute the bulk of the metavolcanic rocks; calc-alkaline quartz dacites are common. The Hillabee Greenstone appears to be the distal continentward portion of a volcanic arc system which developed during the middle Paleozoic in the southernmost Appalachians. The basal, dominantly pyroclastic part of the volcanic sequence is interlayered with the upper part of the Talladega Group, which locally contains a Lower to Middle Devonian fossil assemblage. Refs.
Research Organization:
Fla State Univ, Tallahassee, USA
OSTI ID:
6700445
Journal Information:
Econ. Geol.; (United States), Journal Name: Econ. Geol.; (United States) Vol. 77:2; ISSN ECGLA
Country of Publication:
United States
Language:
English