Skip to Main Content
Skip Nav Destination

This study examines and assesses a number of commonly used biomarker ratios that are routinely applied as proxies for thermal maturity. Using the organic-rich shale of the Bakken Formation and uncontaminated core cut from a single borehole within southern Saskatchewan, Canada, a series of detailed biomarker depth profiles were created based upon 18 samples sampled over an interval of 3.98 m (13 ft). Detailed analysis shows a high degree of variability in Ts/(Ts + Tm), the C29 20S/(20S + 20R) sterane, C29αββ/(ααα +...

You do not currently have access to this chapter.

Figures & Tables




Citing Books via

Close Modal

or Create an Account

Close Modal
Close Modal