illite वाक्य
उदाहरण वाक्य
मोबाइल
- The clay soils containing montmorillonite or smectite ( swelling clays ) are more subject to alkalinity problems than illite or kaolinite clay soils.
- Early use of illite crystallinity was in the petroleum industry to determine the transition from a dry gas phase to an unproductive rock.
- Black shale results from the presence of greater than one percent carbonaceous material and indicates a chlorite, biotite and illite greens ).
- In most sedimentary rocks, mica, feldspar and less stable minerals have been reduced to clay minerals like kaolinite, illite or smectite.
- Analysis of the clay mineral illite from a section across the Windermere Supergroup permits an estimate to be made of its maximum burial depth.
- Believed to be a degradation product of paragonite, like illite it is a non-expanding, clay-sized, micaceous mineral.
- Illite crystallinity can be used to trace the low grade metamorphic transition from zeolite facies to greenschist facies ( diagenetic zone to epizone ).
- If the illite crystallinity values fall in the 0-0.25 ?? range, it corresponds with a metamorphic epizone or greenschist facies.
- These rocks contain amphibole, clay minerals such as illite, kaolinite and smectite, feldspar, plagioclase, potassium feldspar, pyroxene and quartz.
- The drying of the lake left deposits containing amphibole, illite, plagioclase feldspar, potassium feldspar, kaolinite, pyroxene, quartz and smectite.
- The neutral aluminium hydroxide sheets are found sandwiched between silicate sheets in important clay groups : the illite, kaolinite, and montmorillonite / smectite groups.
- The main rock types are sandstone and limestone, and the soil is composed almost exclusively of quartz sand grains and clay minerals ( illite ).
- Width of the illite XRD peak at one half of its height is collected and recorded with units of " ?? ( XRD angle ).
- Minerals formed by alteration processes include alunite, calcite, cristobalite, illite, jarosite, kaolinite, pyrophyllite, quartz, smectite, sulfur and tridymite.
- Greensands are green because of iron-bearing glauconite which is usually recognized as illite / mica or mixed layer illite-smectite clay by x-ray diffraction.
- Greensands are green because of iron-bearing glauconite which is usually recognized as illite / mica or mixed layer illite-smectite clay by x-ray diffraction.
- If the illite crystallinity values fall in the 0.42-1.0 ?? range, it corresponds with a metamorphic deep diagenetic zone or zeolite facies.
- If the illite crystallinity values fall in the 0.25-0.30 ?? range, it corresponds with a metamorphic high anchizone or prehnite-pumpellyite facies.
- If the illite crystallinity values fall in the 0.30-0.42 ?? range, it corresponds with a metamorphic low anchizone or prehnite-pumpellyite facies.
- In stratigraphy and tephrochronology, completely devitrified ( weathered volcanic glass ) ash-fall beds are commonly referred to as K-bentonites when the dominant clay species is illite.
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