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Title: Composition and origin of facies of the Upper Freeport coal bed

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6209962

A detailed study of the Upper Freeport coal bed, in a 120-square mile area in west-central Pennsylvania, indicates that the bed which varies from 4 to 8 feet thick, can be subdivided into at least ten facies. Peat formed within a shallow lacustrine-fluvial-swamp setting that developed on a previously subaerially-exposed carbonate-rich mud. The facies probably formed in three successive stages. In the first stage, topogenous, detritus-rich, low-lying peat formed in near-neutral pH conditions and resulted in 3 to 7 banded, vitrain-poor, coal-bed facies that are enriched in semifusinite; in the second stage, soligenous(.), detritus-poor, raised peat formed in acid pH conditions that resulted in 1 to 2 banded, vitrain-rich, coal-bed facies that are enriched in micrinite and sporinite; and in the third stage, peat islands formed that produced 1 to 2 nonbanded and 1 to 2 banded coal-bed facies of limited areal extent that are enriched in inertodetrinite. An intermediate peat facies probably developed between a contemporaneous stream and facies of the second stage resulting in a coal-bed facies that contains thick vitrain and discrete clay-rich layers. Ash and sulfur isopleths of coal-bed facies that constitute each stage show the following: in the first stage, both ash and sulfur increase toward the margins of the coal body where it intertongues with fluvially deposited rocks; in the second stage, ash distribution is random, whereas sulfur variability is correlated with roof lithology; and in the third stage, concentrations of both ash and sulfur are greatest at facies margins where the facies thin abruptly.

Research Organization:
Geological Survey, Reston, VA (USA)
OSTI ID:
6209962
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 36; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English