key words Flashcards
sorting
The degree to which particles are the same size
Mechanically formed
sedimentary rocks result from the processes of erosion, transport and deposition of clasts
matrix
the background material of small grains in which larger grains occur
plasticity
the ability of a material to permanently change shape without fracturing
fissile
refers to the tendency of a rock to split into thin layers
Ooliths
spherical grains showing concentric banding of carbonate material. These are less than 2mm in diameter
micrite
a microcrystalline calcite, a depositional matrix of lime mud
cement
the minerals precipitated between grains in sedimentary rocks binding them together
pellets
carbonate material excreted by animals. They lack concentric structures and are normally 0.04 to 0.08mm in diameter
diagenesis
all the changes that take place in sediments at low temperatures and pressure, at or near to the earth’s surface
lithification
the process of changing unconsolidated sediment into rock
pressure dissolution
occurs where minerals dissolve as the result of applied pressure because pressure dissolution leads to a reduction of volume of the rock in which it occurs
porosity
the volume occupied by spaces in between sedimentary grains. A reduction in porosity squeezes fluid from pore spaces
peat
partly decomposed plant remains with high water content
coal
a carbon rich rock formed from fossil plant remains