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The article discusses advancements in understanding the origins of overpressure in sedimentary basins, categorizing causes into five main types including disequilibrium compaction and fluid expansion. It highlights the evolution of identification methods from indirect to empirical approaches, emphasizing the significance of hydrocarbon generation as a primary mechanism for overpressure formation. The research also notes that the causes of overpressure vary by lithology, with organic matter influencing loggi

Author

Sebas BM

Language

EN