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thermal_maturity_2 [11/05/2023 09:33] mike_gssthermal_maturity_2 [11/05/2023 10:10] (current) mike_gss
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-A summary of microfossil groups and their uses in maturity studies+ 
 +//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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 +{{:maturity06.jpg?nolink|}} 
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 +//Spore Colour Index (SCI) is one of the most widely used techniques as increasing thermal maturity imparts a progressive, cumulative, irreversible colour change which can be measured objectively using photometers.// 
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 +{{:maturity08.jpg?nolink|}} 
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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.// 
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 +{{:maturity09.jpg?nolink|}} 
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 +//Similar fixation occurs in ostracod shells but some colour may also be imparted by the surrounding sediments.// 
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 +{{:maturity10.jpg?nolink|}} 
 +{{:maturity11.jpg?nolink|}} 
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 +//Similar fixation occurs in foram shells and is particularly sensitive to colour change at lower temperatures associated with oil generation.// 
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 +{{:maturity05.jpg?nolink|}} 
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 +//Thermal maturity parameters using vitrintie and microfossils (after Hartkopf-Froder et al., 2015)// 
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 +{{:maturity12.jpg?nolink|}} 
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thermal_maturity_2.1683797630.txt.gz · Last modified: 11/05/2023 09:33 by mike_gss

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