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Title: Depositional environments of some Tertiary lignites from Alabama

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6848433

Petrographic, chemical, stratigraphic, and palynologic methods were used to reconstruct the depositional environments of some Paleocene-Eocene lignites from the Nanafalia Formation (Wilcox Group) and Naheola Formation (Midway Group) of Alabama. Stratigraphic evidence suggests that the thin lignite seams of the Naheola Formation were formed in deltaic settings; whereas,the thicker Nanafalia lignites were formed in stream channels and sinkholes developed on an eroded limestone surface. Lignites from both areas have high sulfur contents; however, the Naheola lignites have high levels of both organic and pyritic sulfur and the Nanafalia lignites have high levels or organic sulfur only. This suggests that iron was less available to the limestone-associated Nanafalia peat swamps than to the deltaic Naheola swamps. The Naheola lignites are composed primarily of banded lithotypes dominated by the huminite macerals gelinite, ulminite, and humodetrinite. Palynologic evidence suggests that the swamp flora that formed these coals contained Corylus, ferns, and palms with ferns being most common in the Naheola swamps and palms being most common in the Nanafalia. In general, differences in petrographic, chemical, and palynologic composition between the Naheola and Nanafalia lignites can readily be explained by differences in the original depositional conditions under which these deposits were formed.

OSTI ID:
6848433
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English