thermal_maturity_2
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| //A summary of microfossil groups and their uses in maturity studies. Numbers refer to particular biological events in Earth history (after Hartkopf-Froder et al., 2015).// | //A summary of microfossil groups and their uses in maturity studies. Numbers refer to particular biological events in Earth history (after Hartkopf-Froder et al., 2015).// | ||
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| //Spore Colour Index (SCI) is one of the most widely used techniques as increasing thermal maturity imparts a progressive, | //Spore Colour Index (SCI) is one of the most widely used techniques as increasing thermal maturity imparts a progressive, | ||
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| //Diffused carbon within the phosphatic mineral that makes up conodont fossils becomes more fixed with increasing thermal maturity resulting in a colour change. Visual comparisons are made with standard colour charts.// | //Diffused carbon within the phosphatic mineral that makes up conodont fossils becomes more fixed with increasing thermal maturity resulting in a colour change. Visual comparisons are made with standard colour charts.// | ||
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| //Similar fixation occurs in ostracod shells but some colour may also be imparted by the surrounding sediments.// | //Similar fixation occurs in ostracod shells but some colour may also be imparted by the surrounding sediments.// | ||
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| //Similar fixation occurs in foram shells and is particularly sensitive to colour change at lower temperatures associated with oil generation.// | //Similar fixation occurs in foram shells and is particularly sensitive to colour change at lower temperatures associated with oil generation.// | ||
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| //Thermal maturity parameters using vitrintie and microfossils (after Hartkopf-Froder et al., 2015)// | //Thermal maturity parameters using vitrintie and microfossils (after Hartkopf-Froder et al., 2015)// | ||
thermal_maturity_2.1683798462.txt.gz · Last modified: 11/05/2023 09:47 by mike_gss