「calcite」の共起表現(1語右で並び替え)

「calcite」の共起表現一覧(1語右で並び替え)

calcite

1語右で並び替え

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metal sculpture by Maurice Lemieux, entitled Calcite, affixed to the wall of the mezzanine and ill
Moreover, the calcite alabaster, being a carbonate, effervesces upo
dite, allanite, zoisite, scapolite, titanite, calcite along with numerous other Co-Ni sulfides and
s it with dissolved minerals such as sulfate, calcite, analcime, anhydrite, chalcedony, microcline,
e, o'danielite, tsumcorite, fahleite, quartz, calcite and gypsum.
ce and occurs in some common crystals such as calcite and quartz.
aguilarite, galena, chalcopyrite, sphalerite, calcite and quartz.
ssociation with zeolites, datolite, prehnite, calcite and serpentine.
formed in prehistoric seas as layers of sand, calcite and iron oxide collected around a nucleus for
ins of Germany, where the mineral occurs with calcite and barite in veins traversing porphyry.
mineral forms a solid solution series between calcite and rhodochrosite, with the color becoming re
oligoclase, together with chlorite, epidote, calcite, and actinolite.
urdochite, limonite, pyromorphite, wulfenite, calcite and quartz.
Albite, calcite, and pyrite often show polysynthetic twinning
he water contains a relatively high degree of calcite and tree branches fallen into the lake are qu
It is the most common cave carbonate after calcite and aragonite.
ed monoclinic crystals, often associated with calcite and other zeolites.
e, chondrodite, phlogopite, chlorite, quartz, calcite and dolomite.
is quite soft , with hardness 3 to 4, between calcite and fluorite.
itoite, clinohedrite, xonotlite, apophyllite, calcite and tobermorite.
tyrrellite, ferroselite, bukovite, krutaite, calcite and dolomite.
ture dependence of the solid solution between calcite and dolomite (Newton, 1989).
Thulite is often mottled with white calcite and occurs as veins and fracture fillings tra
s often found in association with serpentine, calcite, aragonite, dolomite, magnesite, hydromagnesi
ining minerals of high birefringence, such as calcite, are sometimes prepared as ultra-thin section
Jennite, afwillite, oyelite and calcite are all minerals that form in layers within s
te, bustamite, manganocalcite, glaucochroite, calcite, banalsite and alleghanyite.
copper, silver, uraninite, hematite, pyrite, calcite, barite, quartz and feldspar.
rothermal action in veins in association with calcite, barite, and siderite.
Calcite can be either dissolved by groundwater or pre
mphibole, analcime, apatite, barite, biotite, calcite, cancrinite, chalcopyrite, chlorite, diopside
quartz or calcite) cemented together at the hypotenuse (e.g. wi
It occurs with acanthite, calcite, chalcopyrite, galena, pyrite, quartz, rhodoc
Associated minerals include: calcite, chrysoberyl, cordierite, corundum, garnet, k
n minerals include montmorillonite, chlorite, calcite, colemanite, veatchite, sphalerite, pyrite, m
A calcite crystal laid upon a paper with some letters s
e remains of large bivalve molluscs developed calcite crystalization while still under water.
Through concentration and evaporation calcite crystallized on the earthen surface of the ca
Calcite crystallizes in the rhombohedral system, and
The optical axes of the calcite crystals are parallel and aligned perpendicul
n limestone caves that consists of very large calcite crystals resembling dogs' teeth (hence the na
ic matrix which causes aragonite (rather than calcite) crystals to nucleate, in much the same way t
different from the corallines, as individual calcite crystals are deposited in the cell wall of sp
Calcite crystals in fossilized clamshell, fount in Fo
st known crystal is Iceland spar, transparent calcite crystals.
cave formations (stalagmites, stalactites and calcite curtains) which in their extent and preservat
d orientation, and minerals such as quartz or calcite deform into a grain shape preferred orientati
se Pool, named so because of the shape of the calcite deposit on the back wall, is several metres i
sheer abundance of pure white and translucent calcite deposits.
sheer abundance of pure white and translucent calcite deposits.
uction marble is a stone which is composed of calcite, dolomite or serpentine which is capable of t
Garnet, calcite, dolomite and a variety of minerals may occur
tled (or white-veined) serpentine, mixed with calcite, dolomite, or magnesite, which takes a high p
ite, pyrite, hematite, arsenopyrite, bornite, calcite, dolomite, quartz, cofinite, pitchblende, nat
Associated minerals include calcite, dolomite, grossular, wollastonite, talc, dio
rix minerals dominantly include low-magnesium calcite, dolomite, and siliciclastic minerals.
It occurs associated with: sibirskite, calcite, dolomite, garnet, magnetite and pyroxene.
In carbonate sediments the assemblage is calcite, dolomite, quartz, clays, talc, and muscovite
dizing aqueous fluids restricted laterally by calcite filled joints.
gh short it was extremely well decorated with calcite formations and ended in a large chamber with
Jewel Cave contains all the common types of calcite formations, such as stalactites, stalagmites,
In order to protect the calcite formations, novices are not allowed to enter
Found in association with calcite, franklinite, willemite, hardystonite and cli
Minerals found at the site include Calcite, Goethite, Purple Fluorite, Baryte, Galena, R
e, probertite, glauberite, trona, mirabilite, calcite, gypsum and halite.
Gangue minerals are calcite, gypsum, pyrite, iron oxide, and barite.
(called skeletal or fenster crystals), gold, calcite, halite (salt), and water (ice).
hat contain calcium carbonate (CaCO3; mineral calcite) in a lime kiln.
s as white hexagonal crystals associated with calcite in cavites in Carrara marble of the Italian A
istently northwards and numerous “fist-sized” calcite inclusions within the limestones both solid a
fter polymorph aragonite over the more common calcite is favored in the presence of a magnetic fiel
net, wollastonite and other minerals in which calcite is an important component.
Manganoan calcite is sometimes confused with rhodochrosite.
ingernail (Mohs hardness 1.5 to 2), while the calcite kind is too hard to be scratched in this way
es, pyroxenites, amphibole, apatite, biotite, calcite, magnetite, monazite, nepheline, pyrite, pyro
Associated minerals include azurite, calcite, malachite, and smithsonite.
Orange to yellow boltwoodite on dark calcite matrix from Namibia (size: 5.2 x 3 x 2cm)
ints in the limestone with varying amounts of calcite mineralization and tufa growth around groundw
ints in the limestone with varying amounts of calcite mineralization.
et, uraninite in the Australian deposit; with calcite, monazite, bastnasite, thorite, uranothorite
ral crystalline stone (such as quartz, beryl, calcite, obsidian, or amethyst, it may display the na
cognized in many minerals, including; quartz, calcite, olivine, pyroxenes, micas, feldspars, halite
mperature and pressure, and tends to alter to calcite on scales of 107 to 108 years.
jor types are limestone, which is composed of calcite or aragonite (different crystal forms of CaCO
oportion of, calcium carbonate in the form of calcite or aragonite.
Manganoan calcite or Manganocalcite is a variety of calcite ric
Spilite is veined by calcite or chalcedony, and vesicles and cavities are
Calcite, or calcium carbonate, chemical formula CaCO3
The body (theca) was covered with calcite plates with a number of openings.
It consists of minute calcite plates (coccoliths) shed from micro-organisms
-Thompson prism, except that two right-angled calcite prisms are spaced with an air-gap instead of
It consists of two right-angled calcite prisms that are cemented together by their lo
he Wollaston prism consists of two orthogonal calcite prisms, cemented together on their base (trad
Such cements are typically composed of calcite, quartz or clay minerals.
burite, babingtonite, epidote, native copper, calcite, quartz and zeolites.
calcite, quartz), has no unusual results.
are infilled with a secondary mineral such as calcite, quartz, chlorite or one of the zeolites.
Sovite is often a medium to coarse grained calcite rock with variable accessory amphibole, bioti
minerals, such as fluorite, opal, willemite, calcite, ruby and sodalite.
es within the water column, the corresponding calcite saturation of seawater decreases and the shel
e calcitic ooids were typically formed during calcite sea intervals, especially during the Ordovici
epsut, the White Chapel of Senusret I and the calcite shrine of Amenhotep II.
tions before the rebuilding of Amenhotep II's calcite shrine: Urban unit with mudbricks walls of Sa
known as corallites defined by a skeleton of calcite, similar in appearance to a honeycomb.
Rugose corals have a skeleton made of calcite that is often fossilized.
As the water ran through the canals, calcite was slowly but steadily deposited on their wa
Interaction with oil can reduce SO4 creating calcite, water, and hydrogen sulfide (H2S).
two prisms of a birefringent material such as calcite, which are cemented together.
a form of black, bituminous bearing marble or calcite which produces an unpleasant odour when struc
mination of the matrix of sandy limestone and calcite which make up all the fossils.
composed of lamellar radial hyaline (glassy) calcite, with typically globular chambers and single
the scarp face of Myreton Hill leads to some calcite workings which date from the Napoleonic Wars.