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Group of non-expanding clay minerals
Illite, also called hydromica or hydromuscovite, is a group of closely related non-expanding clay minerals. Illite is a secondary mineral precipitate,
Illite
Fine-grained, clastic sedimentary rock
(especially in mid-to early Paleozoic shales) illites predominate. The transformation of smectite to illite produces silica, sodium, calcium, magnesium
Shale
Fine-grained aluminium phyllosilicates
presence of smectite clay minerals on the planet Mars. Illite group which includes the clay-micas. Illite is the only common mineral in this group. Chlorite
Clay_mineral
Technique used to classify metamorphic activity in pelitic rocks
Illite crystallinity is a technique used to classify low-grade metamorphic activity in pelitic rocks. Determining the "illite crystallinity index" allows
Illite_crystallinity
Phyllosilicate clay mineral
kaolinite decreases, while the proportion of other clay minerals such as illite (in cooler climates) or smectite (in drier climates) increases. Such climatically
Kaolinite
Phyllosilicate minerals in the smectite group
varies with source. It often occurs intermixed with chlorite, muscovite, illite, cookeite, and kaolinite. Montmorillonite can be concentrated and transformed
Montmorillonite
Trough off the coast of Japan
interest in the release of water from illite clays in subducting sediments. The conversion of smectite to illite (illitization) in subduction zones is
Nankai_Trough
Mosaic tile decoration
presence of illite, chlorite, smectite and traces of mixed layer illite/chlorite. Meknes clays belong to illitic clays, characterized by illite (54 – 61%)
Zellij
Metamorphic rock
converted to graphite. Slate is mainly composed of the minerals quartz, illite, and chlorite, which account for up to 95% of its composition. The most
Slate
Earth, a natural material
Sesquioxides —N/a 0–3 Kaolinite —N/a 3–15 Illite —N/a 25–40 Montmorillonite —N/a 60–100 Vermiculite (similar to illite) —N/a 80–150 Humus —N/a 100–300
Soil
Type of claystone, composed of absorbent smectite clay minerals
when the dominant clay species is illite (a non-swelling clay). However, in pure clay mineralogy, the term illite is more appropriate than "K-bentonite"
Bentonite
amphibole minerals) Auerlite (variety of thorite) Avalite (chromian variety of illite) Aventurine (variety of quartz) Babefphite Babingtonite Baddeleyite Baileychlore
List_of_minerals
Fine grained natural soil
Weathering of the same kind of rock under alkaline conditions produces illite. Smectite forms by weathering of igneous rock under alkaline conditions
Clay
Mineral mixture of phyllosilicates
interlayer) while poorly hydrated potassium ions are "collapsers" like in illite (totally collapsed interlayer). As the interlayer space of smectites is
Smectite
Mica mineral in the celadonite subgroup
low-temperature potassium dioctahedral mica mineral which is an end-member in the illite-aluminoceladonite solid solution series. The chemical formula for aluminoceladonite
Aluminoceladonite
Archaeological site
followed by interstratified illite and smectite. The alkaline nature of the clay can be attributed to calcite. Quartz, mica and illite are very stable substances
Isinuka Mud Caves and Sulphur Pools
Isinuka_Mud_Caves_and_Sulphur_Pools
Group of phyllosilicate minerals
Etsell, Thomas H. (16 July 2015). "Influence of Nonswelling Clay Minerals (Illite, Kaolinite, and Chlorite) on Nonaqueous Solvent Extraction of Bitumen".
Chlorite_group
Group of phyllosilicate minerals
micas". They include: Hydro-muscovite with H3O+ along with K in the X site; Illite with a K deficiency in the X site and correspondingly more Si in the Z site;
Mica
and chlorite. In argillaceous sedimentary rocks the assemblage is quartz, illite, albite, and stilpnomelane chlorite. In carbonate sediments the assemblage
Prehnite-pumpellyite_facies
Aggregates of micas
and aggregates of white (colourless) micas, typically made of muscovite, illite, or paragonite. Sericite is produced by the alteration of orthoclase or
Sericite
Mineral made of silicon and oxygen
Stráská, Jitka; Chmelík, František (January 2016). "Study of microcracking in illite-based ceramics during firing". Journal of the European Ceramic Society.
Quartz
Process of mineral alteration
Buchans–Roberts Arm Belt of Newfoundland, these assemblages include muscovitic illite, phengite, and paragonite associated with hydrothermal alteration zones
Sericitic_alteration
Magnesium- and iron-rich extrusive igneous rock
to calcium-rich clay (montmorillonite) rather than potassium-rich clay (illite). Further weathering, particularly in tropical climates, converts the montmorillonite
Basalt
Iron-rich end member of the chlorite group
greyish-green streak. Birefringence is much lower than that of the micas, illite, montmorillonite and vermiculite, and refractive indices are higher than
Chamosite
wall rock which introduces clay minerals including kaolinite, smectite and illite. The process generally occurs at low temperatures and may occur in atmospheric
Argillic_alteration
Anion, salt, functional group or ester derived from a phosphoric acid
to the edges of clay minerals including koalinite, montmorillonite, and illite. Soil organic matter competes with phosphates for adsorption sites, so soils
Phosphate
commonly referred to as K-bentonites when the dominant clay species is illite. Other common clay species, and sometimes dominant, are montmorillonite
List of countries by bentonite production
List_of_countries_by_bentonite_production
Building material of earth and organic materials
clay content should be expansive clays, with the remainder non-expansive illite or kaolinite. Too much expansive clay results in uneven drying through the
Adobe
Geologic formation in Hungary
Sauropod tracks have been reported from the formation. It is abundant on Illite and very little Kaolinite that indicates a change from the humid-subtropical
Kecskehát_Limestone
Phyllosilicate mineral in the dioctahedral mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Muscovite
Group of rock-forming minerals
of feldspars happens by hydrolysis and produces clay minerals, including illite, smectite, and kaolinite. Hydrolysis of feldspars begins with the feldspar
Feldspar
Crushed rock found near faults
the brittle crust. Gouges dominated by clay minerals (montmorillonite, illite, and chlorite) are consistently weaker. Those with a high concentration
Fault_gouge
Phyllosilicate mineral in the pyrophyllite-talc group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Talc
Phyllosilicate mineral
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Chrysocolla
Type of sedimentary rock
kaolinite or, less commonly, other clay minerals such as montmorillonite and illite. The clays often are cemented by iron oxide minerals, carbonaceous matter
Tonstein
Genus of flowering plants
carbon changes, similar to a podzolisation process, and destruction of clay (illite-like minerals), which is the main reservoir of potassium in the soil. Although
Eucalyptus
Radiometric dating method
of illite formed by weathering was reported. This finding indirectly led to the dating of the strandflat of Western Norway from where the illite was
K–Ar_dating
Hydrous phyllosilicate mineral
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Vermiculite
Clay soil prone to swelling and shrinking
with smectite clay minerals, including montmorillonite, kaolinite, and illite group minerals, such as montmorillonite-containing bentonite, have the most
Expansive_clay
Subgroup of phyllosilicate minerals within the kaolinite-serpentine group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Serpentine_subgroup
Type of clay found in coastal regions around the world
consolidate on the seabed. Marine clays commonly contain minerals such as illite, smectite, kaolinite, and chlorite, along with varying amounts of silt,
Marine_clay
Mineral deposits from seafloor hydrothermal vents
(including Mg-rich ones) and phyllic alteration (dominated by “sericite”, mostly illite), and also silicification, deep and shallow talcose alteration, and ferruginous
Seafloor massive sulfide deposits
Seafloor_massive_sulfide_deposits
Form of aluminium hydroxide, mineral
found sandwiched between silicate sheets in important clay groups: the illite, kaolinite, and montmorillonite/smectite groups. The individual aluminium
Gibbsite
Anaerobic microorganisms using a metal as terminal electron acceptor to respirate
goethite, lepidocrocite, ferrihydrite, hydrous ferric oxide, smectite, illite, jarosite, among others. In natural systems, secondary minerals may form
Dissimilatory metal-reducing microorganisms
Dissimilatory_metal-reducing_microorganisms
Phyllosilicate mineral in the dioctahedral mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Roscoelite
Badlands in Caledon, Ontario, Canada
from 58% to 68% clay, and the dominant clay minerals, illite and chlorite. The non-swelling illite in the shales can cause high pressures with repeated
Cheltenham_Badlands
Sedimentary rocks made of mineral or rock fragments
Other important reactions include the formation of chlorite, glauconite, illite and iron oxide (if oxygenated pore water is present). The precipitation
Clastic_rock
Deterioration of rocks and minerals through exposure to the elements
table is only a rough guide to order of weathering. Some minerals, such as illite, are unusually stable, while silica is unusually unstable given the strength
Weathering
Fixed K accounts for 96-99% of soil K and is stored in feldspar, mica, and illite minerals. Exchangeable K is potassium adsorbed onto clay particles and organic
Potassium_cycle
Geologic formation found in the United States
and upper members is set where kaolinite clay becomes more abundant than illite clay. The formation is exposed in the San Juan Mountains, the Sangre de
Molas_Formation
Geotechnical characteristics of a soil related to its water content
PL, % SL, % Montmorillonite 100-900 50-100 8.5-15 Nontronite 37-72 19-27 Illite 60-120 35-60 15-17 Kaolinite 30-110 25-40 25-29 Hydrated halloysite 50-70
Atterberg_limits
Soft and porous white magnesium phyllosilicate clay
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Sepiolite
Degree to which a material becomes magnetized in an applied magnetic field
possible to quantify clay content in clastic shoreface reservoir; minerals as illite and quartz can be measured through mass magnetic susceptibility, high amounts
Magnetic_susceptibility
Mica mineral in the biotite subgroup
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Annite
Phyllosilicate mineral in the brittle mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Clintonite
Process by which soils decrease in volume
saturated specimens of clay minerals increases in the order kaolinite < illite < smectite[clarification needed]. The compression index Cc, which is defined
Soil_consolidation
spectroradiometry. Illite, for instance, is commonly observed in the vicinity of hydrothermal ore bodies. Higher concentrations of illite may indicate areas
Spectroradiometry for Earth and planetary remote sensing
Spectroradiometry_for_Earth_and_planetary_remote_sensing
four main groups of clay minerals: kaolinite, montmorillonite-smectite, illite, and chlorite. Most clays are crystalline and most are made up of three
Soil_matrix
Chemical alteration of a rock by hydrothermal and other fluids
feldspars and some other minerals into clay minerals such as kaolinite and illite. It can overprint older, higher-temperature alteration assemblages. Rarer
Metasomatism
Planets The Opening "The Medicine" — Frontline Sine Language "Neighborhoods" Illite & Magestik Legend Musab Respect the Life "Make Believe" — DJ Graffiti Bling
One_Be_Lo_discography
Rock formed by the deposition and cementation of particles
less stable minerals have been weathered to clay minerals like kaolinite, illite or smectite. Among the three major types of rock, fossils are most commonly
Sedimentary_rock
Most commonly encountered form of asbestos
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Chrysotile
Ratio of the electrical charge to the radius of an ion
the less hydrated K+ and Ca2+ cause the collapse of the interlayer. In illite, the interlayer is totally collapsed because of the presence of the poorly
Ionic_potential
Geologic formation in Scandinavia
quartz, feldspars are the abundant minerals. Clay minerals are dominated by illite, with some smectite, kaolinite, and chlorite. Pyrite is common and calcite
Alum_Shale_Formation
with soil, hundreds of feet thick in many places. Much of this soil is "Illite", and is the most common type of soil on the planet. The visible geology
Geography_of_Illinois
Prefecture-level city in Zhejiang, China
covering targets such as fluorite, pyrophyllite, lead, silver, beryllium, illite, and geothermal resources. Alunite is so abundant that sometimes Wenzhou
Wenzhou
Geological formation in the United States
(uncommonly) grayish-black shale. The primary minerals in the shale are chlorite, illite, kaolinite, and quartz. Thin to massive beds of siltstone and sandstone
Chagrin_Shale
Sedimentary rocks with ferric oxides
are precipitated as authigenic phases. These include mixed layer clays (illite – montmorillonite), quartz, potassium feldspar and carbonates as well as
Red_beds
Archaeological site in Chengdu, China
encourage the growth of bacteria, mosses and cracks. A high concentration of illite was found in its soil, which makes the site's features and objects prone
Jinsha_site
Triassic age unit of sedimentary rock in Australia
weathering is affiliated with variations in mineralogy. Chlorite and some illite are broken down, accompanied by an increase in mixed-layer clay minerals
Bringelly_Shale
Phyllosilicate mineral in the serpentine subgroup
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Lizardite
Phyllosilicate mineral
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Falcondoite
Study of magnetic properties of minerals
susceptibility × 10 − 6 {\displaystyle \times 10^{-6}} (SI) garnet 2,700 illite 410 montmorillonite 330-350 biotite 1,500-2,900 siderite 1,300-11,000 chromite
Magnetic_mineralogy
Phyllosilicate mineral in the stilpnomelane group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Franklinphilite
Organic-rich fine-grained sedimentary rock containing kerogen
carbonates. Inorganic matrix can contain quartz, feldspar, clay (mainly illite and chlorite), carbonate (calcite and dolomite), pyrite and some other minerals
Oil_shale
Early Jurassic geological formation of south-western Germany
layered on a major 60% silicate component with a pronounced dominance of illite, along with a significant amount of montmorillonite. The presence of quartz
Posidonia_Shale
District in Hebei, People's Republic of China
refractory clay, quartz sandstone, dolomite, various types of limestone, and illite. Major mines are located in Linxi Subdistrict [zh], Zhaogezhuang Subdistrict [zh]
Guye,_Tangshan
Pre-Neanderthal population in Spain
phyllosilicates, of which more than 60 percent is illite which is weakly magnetic. Paleomagnetic dating of the illite indicates that the layer is younger than
Sima_de_los_Huesos_hominins
Physico-chemical changes in sediments occurring after their deposition
Hutcheon IE, Bloch JD, Caritat PD (1994). "Silica activity and the smectite-illite reaction". Geology. 22 (6): 539–542. Bibcode:1994Geo....22..539A. doi:10
Diagenesis
Phyllosilicate mineral in the dioctahedral mica group
Brammallite is a sodium-rich analogue of illite. First described in 1943 for an occurrence in Llandybie, Wales, it was named for British geologist and
Brammallite
Phyllosilicate mineral in the dioctahedral mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Phengite
Mineral weathering prediction method
including Al-, Na- and K-rich clays such as kaolinite, montmorillonite and illite. The Goldich dissolution series can be applied to Lithosequences, which
Goldich_dissolution_series
Form of precipitation containing visible dust
chlorine and magnesium). Major minerals in order of decreasing abundance are: illite, quartz, smectite, palygorskite, kaolinite, calcite, dolomite and feldspars
Rain_dust
Subgroup of phyllosilicate minerals within the trioctahedral mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Biotite
Mica mineral in the celadonite subgroup
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Celadonite
nontronite, bentonite, chlorite, montmorillonite, beidellite, attapulgite, illite and vermiculite. The amount of these minerals in a particular soil will
Shrink–swell_capacity
Phyllosilicate mineral: group of kaolinite
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Nacrite
Dark-coloured sediments rich in organic matter
represented by a poly-component mixture of clay minerals. The minerals illite and montmorillonite predominate, chlorite and kaolinite occur in subordinate
Sapropel
Geological formation in Argentina
Bajada Colorada Formation have revealed the presence of smectite, chlorite, illite and kaolinite. The formation has provided fossils of: List of dinosaur-bearing
Bajada_Colorada_Formation
Phyllosilicate mineral in the brittle mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Margarite
Type of plaster
minerals involved in this process include montmorillonite, chlorite and illite, each adding distinct properties to the composition. Despite the chemical
Earthen_plaster
Part of the porosity in which a given fluid can flow
of iron-bearing glauconite which is usually recognized as illite/mica or mixed layer illite-smectite clay by x-ray diffraction. The glauconite per se
Effective_porosity
Phyllosilicate mineral in the dioctahedral mica group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Glauconite
Phyllosilicate mineral in the smectite group
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Nontronite
Concrete admixture: calcined kaolinite exhibiting pozzolanic reactivity
the pozzolanic activity of clay minerals: A comparison between kaolinite, illite and montmorillonite". Cement and Concrete Research. 41: 113–122. doi:10
Metakaolin
Phyllosilicate mineral in the serpentine subgroup
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Cronstedtite
Uranium mine in Saskatchewan, Canada
480 ft), surrounded by and isolated within a layer of water-impermeable illite-chlorite clay, within the Athabasca Sandstone formation. Its age is estimated
Cigar_Lake_mine
Phyllosilicate mineral in the serpentine subgroup
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Amesite
Phyllosilicate mineral
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Stilpnomelane
Mica mineral in the biotite subgroup
Fluorotetraferriphlogopite Garmite Glauconite Gorbunovite Hendricksite Illite Kinoshitalite Lepidolite Luanshiweiite Manganiceladonite Margarite Masutomilite
Phlogopite
ILLITE
ILLITE
Surname or Lastname
English
English : habitational name from the city of Lincoln, so named from an original British name Lindo- ‘lake’ + Latin colonia ‘settlement’, ‘colony’. The place was an important administrative center during the Roman occupation of Britain and in the Middle Ages it was a center for the manufacture of cloth, including the famous ‘Lincoln green’.Abraham Lincoln (1809–65), 16th president of the United States, was the son of an illiterate laborer, descended from a certain Samuel Lincoln, who had emigrated from England to MA in 1637.
Boy/Male
Arabic
Illiterate
ILLITE
ILLITE
Boy/Male
Indian, Tamil
God Murugan
Boy/Male
British, English
From the West Cottage
Girl/Female
Muslim/Islamic
Gift
Boy/Male
Hindu
Universal
Boy/Male
Arabic, Australian, Egyptian
Thankful Person
Female
English
Variant form of English Keren, KERENA means "horn (of an animal)."Â
Boy/Male
American, Australian, British, English, Teutonic
From the Willow Valley
Boy/Male
African, Hindu, Indian, Sikh, Swahili
Brave; Anything Nice
Boy/Male
English
Leader.
Boy/Male
Hindu
Possessed with skills
ILLITE
ILLITE
ILLITE
ILLITE
ILLITE
n.
A mistress; a wife; -- so used by the illiterate.
a.
Not cultivated; rude; illiterate.
a.
Ignorant of letters or books; unlettered; uninstructed; uneducated; as, an illiterate man, or people.
a.
Illiterate.
a.
Not versed in literature; illiterate.
n.
A illiterate person.
n.
A reader of lections; formerly, a person designated to read lessons to the illiterate.
n.
An instance of ignorance; a literary blunder.
n.
Want of learning; illiteracy.
a.
Not literal.
a.
Not learned; untaught; uneducated; ignorant; illiterate.
n.
The state of being illiterate, or uneducated; want of learning, or knowledge; ignorance; specifically, inability to read and write; as, the illiteracy shown by the last census.
n.
A dialect peculiar to the illiterate classes; a provincial form of speech.
pl.
of Illiteracy
a.
Rude; clownish; illiterate.