The most known equation has been proposed by Barker & Pawlewicz (1986) correlating vitrinite reflectance and maximum temperature.
Is it useful to estimate the bulk of burial in orogenic sediments assuming a specific geothermal degree?
Well,
Vitrinite reflectance (Ro)
It is a measure of the thermal maturity that can be performed on plant materials and is calculated from the maximum temperature values.
Ro%= (0.0180*Tmax. °C)-7.16,
Vitrinite Reflectance (Ro%)
• Low maturity source rocks 0.0 -0.55%
• Oil window 0.55%- 1.15%
• Condensate – wet gas window 1.15% -1.40%
• Dry gas window > 1.40 %
Hydrogen Index whom correlating with Tmax to estimate the maturity and burial depth.
HI=Hydrogen Index= HI = (S2*100)/TOC%, Where.
S2= Hydrocarbon cracked from Kerogen (mg HC/g rock).
TOC% = Total organic carbon (%)
Q; Is the orogenic sediment oil-bearing horizons or not, if yes, it is useful, if not it is not useful.
Regards
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