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Clast
these are rock fragments with varying sizes
matrix
cementing material that bonds sediment together to form sedimentary rock
fissility
plane of weakness of mudstone (shale)
sediments
These are products of Erosion and transport of weathered rock fragments
1. Weathering of rocks
2. Erosion and transport of weathered rock fragments - sediments
3. Deposition of the sediments
4. Precipitation of the cementing material
5. Lithification
Process of origin of sedimentary rocks
Diagenesis
This is the process of Lithification (compaction and cementation) of older sediments due to the deposition of younger sediments
Diagenesis
Refers to the collective term for all the chemical, physical, and biological changes that take place after the sediments are deposited
Compaction
Refers to the process of adding sediments to the initially deposited sediments
cementation
Refers crystallization of minerals among the individual sediment grains
Detrital (Clastic) Sedimentary Rocks
Rocks that are formed from weathering, erosion, and compaction of sediments.
Chemical Sedimentary Rocks
Rocks formed from the precipitation of soluble material produced primarily by chemical weathering.
Organic Sedimentary Rocks
Rocks that are made up of organic materials from the remains of dead organisms.
1. Clast
2. particle size
3. Sorting
4. Sphericity and Roundness
5. Porosity and Permeability
6. Sediment Maturity
6 Classification of Clastic Rocks
Rock Fragments
Quartz
Clay Minerals
Feldspars
Micas
Fossils
Types of Clast
Halite
calcite
olivine
in Golidich stability series, what is the least stable and have fast Weathering
hematite
gibbsite
quarts
in Goldich stability series, what is the most stable and have low weathering
particle size
Used as a primary basis for distinguishing among various detrital sedimentary rocks.
1. Boulder
2. cobble
3. pebble
4. granule
what are the particle names of following gravel sizes:
___________ greater than 256mm
___________ 64mm to 256mm
___________ 4mm to 64mm
___________ 2mm to 4mm
Udden-Wentworth Scale
it defines gravel, sand and mud particles according to their mean diameter
gravel
a particles have diameters larger than 2.0 mm, about the size of a small grain of rice.
sand
particles have diameters between 2.0 and 0.0625 mm, the size range seen on sandpaper or between finely granulated sugar and small grains of rice.
mud
particles possess diameters smaller than 0.0625 mm, like processed flour or baby powder.
silt
particles, with diameters between 0.0625 and ~ 0.004 mm
clay
particles, whose diameters are less than 0.004 mm (4 micrometer).
sorting
Refers to the degree of similarity in particle size As the range of particle sizes decreases, sorting increases
Sphericity
It measures the degree to which a particle approaches the dimensions of a perfect sphere
porosity
It is simply the volume percentage of void spaces, called pores
Permeability
It expresses the rate of fluid flow through a rock.
clays
this sediment type usually has low hydraulic conductivity
gravel
this sediment type usually has high hydraulic conductivity
10^-6 cm/s
10^-4 cm/s
10^-2 cm/s to 10^-3 cm/s
10^-1 cm/s to 10^1 cm/s
Hydraulic conductivity of the following:
clay
Sediment Maturity
Refers to the length of time that the sediment has been in the sedimentary cycle
conglomerate
Coarse- to very coarse-grained sediments and have more spherical grains
breccia
Coarse- to very coarse-grained sediments have more angular grains
sandstone
Composed of sand-sized particles and Form in a variety of environments
pettijohn diagram
digram use in related criteria to organize sandstones into groups, similar boundaries to separate different types and related terms to name different varieties of sandstone
Shale or Mudrock
Collective term for fine-grained rocks composed of silt- and/or clay-sized particles
siltstone
claystone
mudstone
___________ silt size particle
___________ clay size particle
___________ another name for shale
chemical sedimentary rock
Rocks formed from the precipitation of dissolved ions that are carried in solution to lakes and seas.
organic
inorganic
The precipitation of materials occurs in two ways:
___________ Processes involving water-dwelling organisms
___________Processes involving evaporation and chemical activity
Allochem
It is a sand- and/or gravel-size carbonate particles
ooids
limeclast
peliods
Allochems include:
Spherical particles called ________
Clasts of carbonate sediment called ________
Smaller pellet-like particles called _________
Micrite
It is the silt- and clay-size carbonate particles in limestones and dolostones
Secretion by calcareous algae.
Micritization of pre-existing carbonate by microbes.
Mechanical abrasion of pre-existing carbonate grains.
Precipitation from solution.
The origin of carbonate mud particles or micrite:
Sparry Calcite
It is a coarse crystalline calcite cement which fills pore spaces in many limestones after deposition, formed by the precipitation of calcite from carbonate-rich solutions passing through the pore spaces in the sediment.
calcirudite or dolorudite
calcium carbonate or dolomite with size of gravel
Calcarenite or dolarenite
calcium carbonate or dolomite with modal particle size of silt
calcilutite or dololutite
calcium carbonate or dolomite with modal particle size of mud
Dunham Classification System
It emphasizes the texture of carbonate rocks, utilizing rather simple terminology
Folk Classification System
It revolutionized our understanding of carbonate rocks. It encouraged workers to pay careful attention to the components of carbonate rocks that lie at the heart of the classification scheme
limestone
Most abundant chemical sedimentary rocks
Mainly composed of calcite (CaCO3)
Coralline Limestone
Limestones made up of fossilized corals
Coquina
Limestones made up of shell fragments
trevertine
Limestones commonly found in caves
chalk
Limestones made up of the hard parts of microscopic organisms especially the coccolithophores
dripstone
Travertine that are precipitated from the endless dripping of water inside the cave.
dolostone
Rock composed of dolomite CaMgCO3
chert
Rock is composed of hard parts of an organism (like radiolaria) that is made up of microcrystalline quartz.
Flint
Dark-colored variety of chert
Jasper
Red variety of chert
Agate
Banded form of chert
bedded cherts
replacement cherts
Mode of formation:
Deposition and lithification - _________
Dissolution, migration, precipitation - ___________
evaporites
it is Rocks formed from precipitation of dissolved ions due to the evaporation of water
rock salt
rock gypsum
_________: Rock made up of Halite
_________: Rock made up of Gypsum
Organic Sedimentary Rocks
Rocks formed from the deposition of plant remains.
coal
it formed in a swamp environment where plants flourished during ancient times.
strata
the single most common and characteristic feature of sedimentary rocks
bedding plane
a flat surfaces along which rocks tend to separate or break
cross beds
layers within it that are inclined to the horizontal
graded beds
it refers to a single sedimentary layer that gradually changes from coarse at the bottom to fine at the top
ripple mark
small waves of sand that develop on the surface of a sediment layer by the action of moving water or air
mud craks
it indicate that the sediment in which they were formed was alternately wet and dry.