There is a correlation between paleotemperatures, color and integrity of fossilized miospores, which are being a part of organic components of geological materials. We are defining the type and intensity of organic materials catagenesis by the composition of undissolved dispersed organics, and integrity and colour of miospores. Also we are showing the capabilities of palinologic method in evaluating the hydrocarbon potential of lower carboniferous deposits of Perm region.
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