Diagenesis refers to the physical, chemical, and biological changes that occur to sediment or rock after its initial deposition and burial. It is a process that takes place over long periods of time, typically under the influence of heat, pressure, and fluid flow. Diagenesis can involve various processes such as compaction, cementation, dissolution, recrystallization, and the introduction or removal of minerals. These changes can alter the original texture, composition, and porosity of the sediment or rock, ultimately transforming it into a different type of sedimentary rock. Diagenesis is an important step in the formation of sedimentary rocks and can provide valuable information about the geological history of an area.
0
Anonymous
Dec 13, 2023
Explain the spectrophotometric calibration of the micropipette