Sedimentary Petrology Flashcards
a broad scientific discipline that encompasses study of
all kinds of sedimentary rocks, including those that
constitute a relatively small volume of total
sedimentary rocks
sedimentary petrology
the removal of thick layers of sediments
overlying deeply buried by erosion or uplift
unloading
Rocks which form at low temperatures and pressures at the surface of Earth owing to deposition by water, wind, or ice. covers roughly 3/4 of Earth’s surface
sedimentary rocks
steps in forming sedimentary rock
weathering-erosion-transportation-deposition-diagenesis
The chemical alteration, physical, and biological
breakdown of rock during exposure to the atmosphere,
hydrosphere, and biosphere
weathering
types of weathering
mechanical/physical and chemical
the
expansion force of water as it freezes sufficient
to split any mineral or rock
freezing and thawing
– action of organisms, including animals and
plants reduces the size of rocks and minerals
organisms
Differences
in temperature in a rock give rise to differential
expansion and contraction
heating and cooling
Requires the application of some physical force or stress to be applied to the rock
→ No accompanying changes to the composition of rocks
→ Mechanical breakup increases the rock’s surface area and the surface-to-volume ratio
mechanical weathering
Grinding action, or the
rubbing of moving rock against each other.
griding or rubbing
– the disruption of soil results
in the swelling and contracting of soil beds and particles
wetting and drying
→ breakdown of minerals by chemical reactions with water, with chemicals dissolved in water, or with gases in the air.
→progression from less stable minerals to more stable minerals
chemical weathering
- the dissolving of a solid in a liquid
dissolution
process of minerals reacting with water
to form hydroxides, which usually are more soluble than
the original mineral
hydrolysis
weathering is accelerated by the
presence of hydrogen ion in water, such as that
provided by carbonic and organic acids
acidification
– involves the transfer of charged atoms
(ions) of calcium, magnesium, sodium, and potassium between
waters rich in one of the ions and a mineral rich in another
(Most effective in clays)
ion exchange
used in mineral weathering, is both the chemical combination of oxygen with a compound and the change in oxidation number of some chemical element (Reduction is the chemical process in which electrons are gained.)
oxidation and reduction
– combination of a solid mineral or
element with water
hydration
agents of erosion (GIOWW)
Gravity Ice Organism Water Wind
Agents of Sediment Transport (IWW)
Ice Water Wind
Measures smoothness of the sediment grains
roundness
long distance of transport = ______ roundness
rounded
short distance of transport = ______ roundness
angular
Measure of variation in size of sediment
grains
sorting
short distance of transport = ______ sorted
poorly
the geological process where materials, such as sediment, soil, and rocks, that have been transported by wind, water, ice, or gravity, are laid down or settled in a new location.
deposition
long distance transport = _____ sorted
well
stage of diagenesis that is from sedimentation until shallow burial
early diagenesis
Physical, chemical, and biological processes which collectively result in:
→ Transformation of sediments into sedimentary rock
→ Modification of the texture and mineralogy of the rock
diagenesis
stage of diagenesis that is from deep burial to subsequent uplift
late diagenesis
diagenetic process that squeeze or compacts sediments
compaction
diagenetic process in which there is formation of new minerals
authigenesis
diagenetic process that takes place when dissolved minerals are deposited in the tiny spaces among sediments
cementation
Basic end products, that all sedimentary processes are working to reach
quartz sandstone
shale
limestone
= all visible grains, including such ones
is incompletely weathered feldspar from the granodiorite in the simple ideal model
quartz sandstone
all clay sized grains
shale
= all dissolved minerals, including not only
calcite CaCO3, but also halite (table salt NaCl), and gypsum (CaSO4.2H2O) among others
limestone
categories of sedimentary rocks
clastic/siliciclastic rocks
chemical rocks
biochemical rocks
category of sedimentary rocks that is formed by the end products of mechanical weathering. classified according to texture and composition. made up of clast or framework grains, matrix, and cement
siliciclastic rocks