This term applies to hardened sediments and includes those sediments that were reorganized under low pressure and temperature conditions in seeds and other chemical and biochemical components (before actual metamorphism).
Biogenic, Biochemical and Organic Sediments: Lime, Nap, Phosphate, etc.
Chemical deposits: evaporation, iron ore and …
Azarvari sediments: Ignembrit, Tuff, Hyalucleastite, etc.
T : Rubble or trijenus stones such as lichen, hose and conglomerate.
IA : Impurity alkmical or gross debris such as fossilized shales.
Io : Impure or chemically impure or chemical ortho, such as microcrystalline limestone.
A: Alokomicals such as limestones or fossilized dolomites.
O: Orthochemical stones such as limestone or microcrystalline dolomites, anhydrites and naps.
Faber Y.K.: Chegong tells of the bilateral relationship betweenB-N seeds and their adjacent grains in the K-rock sediment and their B-distance inthe accumulation.
Accumulation: In the eyesofK and the intensityof particle compaction , the luscious particles (Tomboeder) havethe accumulationofcamels B and less porosity than the accumulationof cubes.
Note: With its increments, your spherical accumulation has become less and its porosity is eternal.
D.T. (Puberty and Dag’s Clay):
Y.T. KanyeYessenas: The more stones withthe camel’s leggedminerals, the more muturmetal it is.
Texture: The rat change of tissue in sediments that depends on three factors:
1- The absence of clay and materials in the rubble inside the stone
2 – Sortingof rotan seeds
3 – Circulation and Spherical
Note: More importantly, the factor affecting thetissue’s wrist is the energyof the K-MT location.
1- If the stone has 5% < clay, it isa premature mamchur .
2- If the stone has 5% > clay and movement and circulationof the weak, thefog of theten submachers.
3- Goodsorting and poor circulation of 5% >;
4- Good clay circulation 5% >,kh-l-clay 10 O supermechur
M. Xan Rass circulation and jurdung, photo with note: The wrist of the dag of my direct relationship with
Note:
Returnof tissue 1 – clay less than 5% and good circulation
Clay10 2 – Clay less than 5% and good matching
Machuriti Mineralogy=
Attention:
In the rocks near K-origin: The wrist ofthe T-kahn, thegeologistof the foot.
In rocks far from origin: the wristourofthe high cynologist
Sedimentary Constructions: (KrumbaN and Selas 1963)
1- Construction of the firstdeposition of the co-ordatientsa-n-zent k:
Before hardening, the lack of interference in his interactions.
2 – Construction of secondary deposition of Y.K. Genet: (Sh.M.Y. andF.Y.K.)
SHMA Yi:
1 – Conceckers van: Ball constructions, different materials with B stone cracks, note that the building
The concentrics, the radiusof the curtain, are the conceitsof vanHaqq Qi.
2- Nodwell:The type of van concecker lacks any inner order and organization.
3- NoduleSeptarA:B-shapedsupplication, with radius treks starting from the center and towards the margins of the elimination exit.
Be.
4- MlamKar-e-A: If the noduleof the mattress L, its surface is dried and water is removed and then it is removed and filled with secondary materials
Now, if secondary materials are removed, the de-yar-shaped building , calledMel’s, would have had a job.
5 – Geod: Construction of pitted spherical, with the outside surfaceof Calsdon.
6- Construction of cones in cones: Interconstrate due to the pressure, often the cheadle that is in the sedimentsof the mud ofD.10.
6.Thehingeistt: a harmful state due to pressure and dissolution.
Particles of sedimentaryrocks:
1- The debris ofthewes genie: quartz, feldspar, shards and stonenans.
2- Allocams of alligators:netraclast, ed, fessL, pellet.
3- Ortokums in the jazas: sediments which have not been derided in the face of the 1000s.
Tips:
Plutois lessof a piece of shards .
The origin ofthe croquelN and orthoclase and quartz is thegan-y and grant.
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