Limestone
yes
Deep burial of sediments refers to the process where layers of sediment are deposited and subsequently buried by additional layers over time, leading to increased pressure and temperature. This process occurs in environments such as ocean basins, river deltas, or sedimentary basins. As sediments are buried deeper, they undergo diagenesis, which can transform them into sedimentary rock through compaction and cementation. This process is crucial in the formation of fossil fuels and other geological resources.
In a million years, sediments may undergo compaction and cementation to form sedimentary rock. They may also be uplifted due to tectonic forces and weathered into smaller particles. Overall, the sedimentary cycle will continue as new sediments are deposited on top of older ones over time.
When sediments are buried under deep layers, the increasing pressure from overlying materials leads to a process called compaction. During compaction, the grains of sediment are pressed together, reducing pore space and expelling water. This process contributes to the formation of sedimentary rocks as the sediments become more tightly packed and undergo further cementation, where minerals precipitate and bind the particles together. Ultimately, this transformation is essential for the geological cycle and the development of Earth's crust.
Limestone
yes
The final deposition of sediments usually occur in their final resting place called the deposition environment. These sediments are buried by other sediments.
yes only if they are buried for over millions of years
Sediments that are buried, compacted, and cemented together are known as sedimentary rock. Examples include sandstone, limestone, and shale. These rocks form through the accumulation of mineral and organic particles over time.
Rapidly buried by sediments
Sedimentary rock is made from ancient coral reefs buried by sediments.
it can turn into molten rock it can be heated and pressured and turn into metamorphic it can weather and turn to sediments
Deep burial of sediments refers to the process where layers of sediment are deposited and subsequently buried by additional layers over time, leading to increased pressure and temperature. This process occurs in environments such as ocean basins, river deltas, or sedimentary basins. As sediments are buried deeper, they undergo diagenesis, which can transform them into sedimentary rock through compaction and cementation. This process is crucial in the formation of fossil fuels and other geological resources.
sedimentary rock
it can turn into molten rock it can be heated and pressured and turn into metamorphic it can weather and turn to sediments
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.