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Title: Lateral and vertical variability in petrography and mineralogy of the Lower Kittanning seam, western Pennsylvania and eastern Ohio

Thesis/Dissertation ·
OSTI ID:7179054

A total of 50 channel samples and 70 subsection samples were collected. Several trends in maceral composition were observed: (1) telocollinite (well-preserved woody tissue) increases towards the center of the basin, whereas desmocollinite (highly-degraded vitrinite) increases towards the basin margins; (2) total vitrinite decreases, whereas total liptinite and inertinite both increase, towards the top of the seam; (3) desmocollinite increases, at the expense of telocollinite, towards the top of the seam. These trends are explained by differential preservation of plant material, which is influenced by the pH/Eh of waters within the peat swamp and by the rate of subsidence. Lateral trends in organic composition relate to pH conditions within the swamp and proximity to source areas: (1) syngenetic pyrite formation occurred in areas overlain by brackish shales (where both sulfate and iron were available), whereas marcasite formed epigenetically; (2) quartz content increases towards a northern source area; (3) kaolinite is predominantly authigenic and increases towards the basin margins due to its stability in relatively low pH, freshwater areas of the peat swamp; (4) detrital illite/mica (high-temperature polytype) increases towards the center of the basin due to its greater stability in marine-influenced environments. Low expandable clay contents are consistent with the level of metamorphism experienced by this coal. The distribution of Cr, Cu, Ni, Rb, and Sr can be explained by their association with clay minerals. Zr distribution reflects an influx of detrital zircon. The distribution of Be and V can be explained by their original entrapment by the organic fraction of the peat or coal as they entered the basin.

Research Organization:
Pennsylvania State Univ., University Park (USA)
OSTI ID:
7179054
Resource Relation:
Other Information: Thesis (Ph. D.)
Country of Publication:
United States
Language:
English

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