Abstract
To study the relationships between the chemical structures of coals, coal macerals, and their precursors (plant tissues), a high-volatile bituminous Upper Carboniferous coal and its constituting maceral fractions, cutinite, resinite, sporinite, vitrinite, pseudovitrinite, semifusinite, and fusinite, were investigated by Curie point pyrolysis−gas chromatography and Curie point pyrolysis−gas chromatography−mass spectrometry
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