property of grain aggregates
Fabric
encompasses all aspects of the external
morphology of particles, including form, roundness and surface
texture
Particle shape
refers to the gross, overall morphology or
configuration of the particles
Form
measure of sharpness of the corners of a
grain, commonly measured in 2-dimension only
Roundness
refers to the microrelief features such
as scratches and pits
Surface texture
measure of sharpness of the corners of a
grain, commonly measured in 2-dimension only
Roundness
any sandstone containing considerable clay
(> 5%); framework grains poorly sorted and poorly
rounded
Immature
low clay content, but grains are still not well
sorted or well rounded
Submature
clay content is low , framework grains become
well-sorted, but not yet well rounded
Mature
essentially clay-free, and framework
grains are both well sorted and well rounded
Supermature
Stages of textural maturity
Immature
Submature
Mature
Supermature
function of the size and shape of grains and
post-depositional physical and chemical processes that bring
about compaction of sediment
Grain packing
function of the physical processes
and conditions operating at the time of deposition; can be
modified after deposition by the acitivities of organisms
(bioturbation) and to some extent by the processes of
compaction during diagenesis
Grain orientation
Arrangement of clastic grains, entirely apart form any
authigenic grains that may have crystallized
Packing
potential usefulness in paleocurrent analysis
believed to have an effect on the permeability of sedimentary rocks
to fluid movement- interest to hydrologists and petroleum
geologists may have significance in paleoenvironmental studies
Particle orientation
the ratio of pore space in a sediment or sedimentary
rock to the total volume of the rock
Porosity
3 type of primary porosity
Intergranular
Intragranukar
Intercrystalline
Enumerate 3 Secondary porosity
Solution porosity
Intercrystalline
Fracture porosity
the ability of a medium to transmit a fluid. Property of a rock that permits the passage of a fluid through the interconnected pores of the rock
Permeability