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Dia Genesis by Ja Kov is a document available to read on EtoBox.

Diagenesis is the process of changes that sediments or sedimentary rocks undergo after deposition and during lithification at low temperatures and pressures. Key factors that influence diagenesis include hydrothermal solutions, meteoric groundwater, porosity, permeability, solubility, and time. Diagenesis alters the mineral composition and texture of rocks and can replace grains and fossils with other minerals. It is important for understanding the geological history of rocks and likelihood of economically

Author
Ja Kov
Language
EN