结果表明，煤中有机硫的存在形式是多样的，这主要取决于成煤母质、沉积环境和泥炭堆积后的成岩变化。
The research shows that the versatile occurrence of organic sulfur are determined by the pre coal material, sedimentary environment, and catagenesis.
该区有机质的丰度较高，并受控子沉积环境与沉积物类型，母质以腐泥-腐殖混合型和腐殖型为主，成熟度低，有机质的转化是多重因素复合作用的结果。
The abundance of organic matter in this area is high and belongs to a mixed sapropelic-humic type or humic type of low maturity. Transformation of organic matter is due to compound multiplex factors.
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