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

Title: Late Permian age of NH[sub 4]-bearing illite in anthracite from eastern Pennsylvania. Temporal limits on coalification in the central Appalachians

Journal Article · · Geological Society of America, Bulletin; (United States)
;  [1];  [2];  [3]
  1. Univ. of Illinois, Urbana, IL (United States)
  2. Case Western Reserve Univ., Cleveland, OH (United States)
  3. Centre de Geochimie de la Surface, Strasbourg (France)

Authigenic NH[sub 4]-bearing illites in coal fractures from the Anthracite region of eastern Pennsylvania yield individual K/Ar dates of 236-253 Ma ([+-]8 m.y.) and a composite isochron of 253 Ma ([+-]8 m.y.). Rh/Sr data for the same samples indicate an isochron of 260 Ma ([+-]44 m.y.), consistent with the more precise K/Ar data. The age of NH[sub 4]-bearing illite authigenesis should reflect the time at which coal attained anthracite rank, because mineralogical and geochemical evidence indicates that NH[sub 4]-bearing illite formed exclusively during anthracite formation (T = 200-275[degree]C) from organically derived nitrogen and a kaolinite precursor. Similar Late Permian K/Ar dates for both NH[sub 4]-rich illite and K-illite in anthracite fractures and lack of correlation between percent NH[sub 4] substitution in illite and the K/Ar date suggest that NH[sub 4] does not influence significantly the closure temperature of illite and, thus, that NH[sub 4]-rich illite can be used for dating the time of authigenesis. Given the uncertainties in closure temperatures for illite as well as the maximum temperatures for anthracite formation, we consider the oldest K/Ar date of 253 Ma ([+-]8 m.y.) to be a minimum age for NH[sub 4]-illite authigenesis and anthracite formation. 33 refs., 4 figs., 4 tabs.

OSTI ID:
7271496
Journal Information:
Geological Society of America, Bulletin; (United States), Vol. 106:6; ISSN 0016-7606
Country of Publication:
United States
Language:
English