Kerogen is the solid, insoluble organic matter found in sedimentary rocks that, when subjected to pyrolysis, generates oil. This article explores the historical context, types, key events, and detailed explanations related to kerogen.
Oil shales are sedimentary rocks containing significant amounts of organic material, kerogen, that can be converted into shale oil through pyrolysis, hydrogenation, or thermal dissolution.
A comprehensive guide to Sedimentology, the study of sediments and sedimentary rocks, including its history, types, key events, models, and its significance in various fields.
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