skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Clay mineral authigenesis in coal and shale from the Anthracite region, Pennsylvania

Journal Article · · American Mineralogist; (USA)
OSTI ID:6221270

Textural, chemical, and mineralogical analyses of authigenic clays in anthracite-rank coal and associated shale from eastern Pennsylvania have allowed a better understanding of the parameters controlling diagenesis and perhaps coalification in this region. Minerals in anthracite occur in distinct assemblages associated with the following microenvironments: coal matrix, two orthogonal joint sets (termed systematic and nonsystematic cleat), and a third joint set. Authigenic minerals that replaced preexisting kaolinite during the latest stage of coalification at T > 200C include NH{sub 4}-rich illite, pyrophyllite, and the following minerals, which are primarily restricted to the systematic cleat set: tosudite (R1-ordered, dioctahedral, mixed-layer chlorite/smectite), sudoite (di, trioctahedral chlorite) and rectorite (R1-ordered, mixed-layer chlorite/smectite). Alteration of smectite to illite may be responsible for formation of authigenic illite and Na-bearing illite, which are present only in the shale and coal matrix, and Fe-, Al-rich chlorite and quartz in the third joint set. Minerals in the shale, the coal matrix, and the nonsystematic cleat set are interpreted to represent authigenesis in a low-permeability environment (closed-system alteration); however, the assemblage sudoite + tosudite + rectorite in the systematic cleat set is interpreted to be the result of one or two stages of hydrothermal alteration (open-system alteration). Hydrothermal alteration may be related to large-scale basinal flow induced by Alleghanian-age uplift; such migrating fluids could also have transported heat from depth and thereby significantly increased the rate and rank of coalification in this region.

OSTI ID:
6221270
Journal Information:
American Mineralogist; (USA), Vol. 75:7-8; ISSN 0003-004X
Country of Publication:
United States
Language:
English