Pc. Lyons et M. Mastalerz, Secretinite-reflectance and chemical data from two high volatile bituminous coals (Upper Carboniferous) of North America, INT J COAL, 45(4), 2001, pp. 281-287
Secretinite-a maceral of the inertinite group as recognized by the ICCP in
1996-is a noncellular maceral of seed fern origin. New reflectance data ind
icate that this maceral has primary anisotropy with bireflectances of 0.4%
to 0.9% in high-volatile B bituminous (Ro = 0.6%) Carboniferous coal of Nor
th America. The highest reflectance is in cross-section as opposed to longi
tudinal section. Characteristic feature of secretinite is the virtual absen
ce of Si and Al, unlike that in associated vitrinite. This indicates the ab
sence of submicron aluminosilicates in secretinite and their presence in vi
trinites. Secretinite is highly aromatic as indicated by low O/C ratios and
high contribution of aromatic hydrogen bands detected by FTIR analysis. (C
) 2001 Elsevier Science B.V. All rights reserved.