Abstract
Almost all of minerals in the geosphere can be identified in sedimentary rocks. However, at this point there will be more discussion only about silicate, carbonate and sulphide minerals, as they are the most common and most important in studies of the interactions of inorganic and organic matter in sedimentary rocks.
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References
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Schwarzbauer, J., Jovančićević, B. (2015). Minerals in Sediments and Their Impact on the Changes of Organic Substances in Geosphere. In: Fossil Matter in the Geosphere. Fundamentals in Organic Geochemistry. Springer, Cham. https://doi.org/10.1007/978-3-319-11938-0_3
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DOI: https://doi.org/10.1007/978-3-319-11938-0_3
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