Vitrinite

Vitrinite is one of the primary components of coals and most sedimentary kerogens. Vitrinite is a type of maceral, where 'macerals' are organic components of coal analogous to the 'minerals' of rocks. Vitrinite has a shiny appearance resembling glass (vitreous). It is derived from the cell-wall material or woody tissue of the plants from which coal was formed. Chemically, it is composed of polymers, cellulose and lignin.The study of vitrinite reflectance (or VR) is a key method for identifying the maximum temperature history of sediments in sedimentary basins. The reflectance of vitrinite was first studied by coal explorationists attempting to diagnose the thermal maturity, or rank, of coal beds. More recently, its utility as a tool for the study of sedimentary organic matter metamorphism from kerogens to hydrocarbons has been increasingly exploited. The key attraction of vitrinite reflectance in this context is its sensitivity to temperature ranges that largely correspond to those of hydrocarbon generation (i.e. 60 to 120 °C). This means that, with a suitable calibration, vitrinite reflectance can be used as an indicator of maturity in hydrocarbon source rocks. Generally, the onset of oil generation is correlated with a reflectance of 0.5-0.6% and the termination of oil generation with reflectance of 0.85-1.1%. The onset of gas generation ('gas window') is typically associated with values of 1.0-1.3% and terminates around 3.0%. However these generation windows vary between source rocks with different kerogen types (vitrinite is typically abundant in 'Type III' kerogen-rich source rocks), so a conversion to 'Transformation Ratio' (TR) can be applied to create a kerogen-specific maturity parameter. The vitrinite reflectance value represents the highest temperature that the vitrinite maceral (and source rock) has experienced, and is routinely used in 1D burial modelling to identify geological unconformities in sedimentary sections.