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diagenesis
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diagenesis

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The formation of sedimentary rock by diagenesis. Sand and other sediment grains are compacted and cemented together.

In geology, the physical, chemical, and biological processes by which a sediment becomes a sedimentary rock. The main processes involved include compaction of the grains, and the cementing of the grains together by the growth of new minerals deposited by percolating groundwater. As a whole, diagenesis is actually a poorly understood process.



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? Mentioned in ? References in periodicals archive
 
Sedimentary Iron formations (BIF) A A deposits Oolitic iron A A Sedimentary phosphates K K Manganese deposits A A Barite in black shales K K Diagenetic Copper in pelites K A deposits Uranium sandstones K K Discordant uranium A ?
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Unconformity uranium deposits are typically associated with fault systems and are usually formed as a result of diagenetic and hydrothermal processes.
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The burrow mottles became dolomitized later in the diagenetic process, as magnesium-rich fluids were able to pass through them, but not through the surrounding material (Kendall, 1977; Coniglio, 1999; Gingras et al.
Geology of the Parliament Buildings 5: Geology of the Manitoba ... by Young, Jeff / Geoscience Canada
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