Abstract
Kerogenis normally defined as that portion of the organic matter present in sedimentary rocks that is insoluble in ordinary organic solvents. The soluble portion, called bitumen, will be discussed in chapter 5. Lack of solubility is a direct result of the large size of kerogen molecules, which have molecular weights of several thousand or more. Each kerogen molecule is unique, because it has patchwork structures formed by the random combination of many small molecular fragments. The chemical and physical characteristics of a kerogen are strongly influenced by the type of biogenic molecules from which the kerogen is formed and by diagenetic transformations of those organic molecules.
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© 1985 International Human Resources Development Corporation
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Waples, D.W. (1985). Kerogen. In: Geochemistry in Petroleum Exploration. Geological Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5436-6_4
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DOI: https://doi.org/10.1007/978-94-009-5436-6_4
Publisher Name: Springer, Dordrecht
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