nriperiod
Nriperiod is a diagenetic and low-maturity transformation of organic matter from Type III kerogen into Type IV kerogen in sedimentary basins. It typically occurs at temperatures between 100 and 180 degrees Celsius and under increased pressure conditions. Nriperiod represents a transitional stage between the oil window and the gas window in the evolution of organic matter.
During the nriperiod, the transformation of the organic matter is characterized by the degradation of the more
The properties of the organic matter transformed during the nriperiod are distinct from those generated during
Nriperiod knowledge has significant implications for sedimentary basin evaluations, as it regulates the potential to form