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Plant debris, algae and other organic matter buried to great depths for long periods in sedimentary basins undergoes a number of chemical and physical changes. These are collectively referred to as rank advance or maturation. They determine the basic quality parameters of any coal seams in the sedimentary succession, and whether significant hydrocarbon resources (oil and natural gas) might also be generated within the basin fill.
A research team within Biological, Earth and Environmental Sciences, in association with Pacific Power and the New South Wales Department of Mineral Resources, has been evaluating the organic maturity pattern of the sedimentary sequence in Gunnedah Basin, New South Wales. The group has been comparing the value of a number of different maturation indicators, including vitrinite reflectance and various coal quality parameters, and geological evolution. Special techniques developed during the study include chemical analysis of small organic particles (macerals) in coals and other sediments using the UNSW electron microprobe, and relating changes in key parameters to rank advance and hydrocarbon generation.
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