“…The narrowing of line widths and the decrease of g value as the sample locations approach the heat pocket caused by the sill are consistent with the results of earlier studies on kerogen in natural environments (Hwang and Pusey, 1973), asphaltene (Yen et al, 1962), and coal (Austen et al, 1965). The unusual broading of EPR spectral lines similar to that seen in the sample about 250 cm above the sill was reported by Baker (1975), but the obliteration of EPR spectra as observed in the samples immediately above and below the sill has not been previously reported.…”