Sentence examples for maximum burial temperature from inspiring English sources

This study has demonstrated an apparent correlation between progressive alteration (maximum burial temperature estimated by vitrinite reflectance) and changes in clay mineralogy despite nearly constant whole-rock mineral assemblages.

The Gurpi Formation has just reached the late oil window with a maximum burial temperature of 143 °C and calculated vitrinite reflectance of 1%%R o (Figs. 12a, 15).

The Pabdeh Formation with a maximum burial temperature of about 124 °C and calculated vitrinite reflectance of 0.8%%R o is interpreted to be within the main oil generation window (Figs. 12a, 16).

The Kazhdumi Formation is at an early mature stage, with a maximum burial temperature of approximately 100 °C (occurred at Late Eocene) and calculated vitrinite reflectance of 0.65 %R o (Fig. 13).

The Gurpi and Pabdeh formations are early mature with estimated maximum burial temperature and calculated vitrinite reflectance values of approximately 90 °C and 0.6%%R o, respectively (Figs. 12b, 15).

The paleotemperature of the syn-tectonic fluid is estimated to be 230°C to 260°C from fluid inclusions in quartz veins within the mélange zone (Vrolijk et al. 1988), whereas the maximum burial temperature of the wall rock is estimated to be 250°C ± 10°C from vitrinite reflectance analysis of carbonaceous material within the argillite (Rowe et al. 2011).

The Ahmadi Member and Gurpi Formation are thermally immature with maximum burial temperatures lower than 85 °C and calculated vitrinite reflectance lower than 0.5%%R o (Figs. 14, 15).

The Gurpi and Pabdeh formations, with maximum burial temperatures lower than 90 °C and calculated vitrinite reflectance lower than 0.5%%R o, are thermally immature (Figs. 15, 16).

Other studied rock units are immature in this well with estimated maximum burial temperatures lower than 80 °C and calculated vitrinite reflectance lower than 0.5%%R o (Figs. 13, 14, 15, 16).

All of the studied source rocks are thermally immature in this well, with estimated maximum burial temperatures lower than 80 °C and calculated vitrinite reflectance values lower than 0.5%%R o (Figs. 13, 14, 15, 16).

The Kazhdumi Formation and Ahmadi Member are interpreted to be early mature, with maximum burial temperatures of 106 and 97 °C and calculated vitrinite reflectance values of 0.67 %R o and 0.62 %R o, respectively (Figs. 13, 14).