“…The notion of hydrothermal influences on coal metamorphism generally did not gain traction until the 1980s with the observations of Oliver (1986Oliver ( , 1992. Just within the Appalachians, connections between the flow of thermal fluids and coal metamorphism were made with respect to the Pennsylvania Anthracite Fields (Bayan and Hower, 2012;Daniels et al, , 1994Daniels et al, , 1996Harrison et al, 2004;Hower and Gayer, 2002;Hower et al, 1993;Juster et al, 1987;Ruppert et al, 2010); western Pennsylvania bituminous coals (Zhang and Davis, 1993); the Valley Fields, Virginia (Lewis and Hower, 1990); and the Central Appalachian bituminous coals (Collins, 1993;Evans and Battles, 1999;Goldhaber et al, 2003;Hearn et al, 1987;Hower and Rimmer, 1991;Ruppert et al, 2010;Sakulpitakphon et al, 2004); and Alabama (Pashin et al, 1990;Winston, 1990).…”