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- W2019223787 abstract "Vitrinite reflectance was determined for over 300 samples of coal and coaly particles in the Disturbed Belt of the southeastern Canadian Cordillera. Coalification gradients observed in deep well profiles are low, ranging from 0.10 to 0.27 log %RoR/km, and indicate that prevailing geothermal gradients have been low for most of the area since the Jurassic. An increase in maturity levels from south to north within the study area is attributed to higher paleo-heat flow in the north. Maturity profiles of deep weels in stacked thrust sheets indicate that a significant component of maturation resulted from overthrusting in some areas. In other areas, postorogenic maturation (if any) was insufficient to overprint existing levels of maturity. A time-temperature model simulating an overthrust event is described which indicates that a 5 km thick thrust sheet can account for observed maturity levels in footwall strata in some areas of the Disturbed Belt." @default.
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- W2019223787 date "1986-01-01" @default.
- W2019223787 modified "2023-10-17" @default.
- W2019223787 title "Effect of thrust faulting on organic maturation in the southeastern Canadian Cordillera" @default.
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- W2019223787 doi "https://doi.org/10.1016/0146-6380(86)90057-4" @default.
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