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How to use leucite in a sentence

Looking for sentences and phrases with the word leucite? Here are some examples.

Sentence Examples
Additionally, lamproites may contain leucite, richterite, sanidine, and occasionally nepheline, whereas kimberlites do not.
Familiar examples include nepheline, leucite, and members of the sodalite and cancrinite groups.
Early reports of leucite from this locality were shown to be an erroneous identification of analcime.
The three commonest feldspathoids are leucite, nepheline, and sodalite.
The crystal form represents the formation of leucite as an isometric mineral.
Properties of nepheline, leucite, sodalite, and cancrinite are summarized below.
Geologic observations of this region were recorded as early as 1869 by the Hayden Survey, and by 1874 Endlich had reported leucite from Table Mountain.
A new leucite glass-ceramic with which you may fully concentrate on the important factors of the restorations, i.e. shade selection, function and surface structure.
This is not surprising since the PFM veneer that has leucite reinforcing crystals that improve fracture toughness.
Figure 3 demonstrates that during the heat-treatment program, part of the phlogopite was transformed to the forsterite and leucite phases.
The most important property of feldspar is its tendency to form crystalline mineral leucite when melted.
This statistical market research report covers feldspar, leucite, nepheline and nepheline syenite.
The amount of crystallized leucite influences properties such as strength and thermal expansion.
Cattella, Flexural strength optimisation of a leucite reinforced glass ceramic, Dental Materials Vol.
They may be of considerable size like the grey, rounded leucite crystals found on the sides of Vesuvius.
Varieties rich in leucite and haĆ¼ynite are well known.
Minerals of the feldspathoid group whose silica contents are less than those of their feldspar analogues include nephelin, leucite, sodalite, and cancrinite.
Silica minerals thus occur only in magmas containing more than about 47 percent by weight of SiO2 and are incompatible with minerals with low cation:silica ratios such as olivine, nepheline, or leucite.
The crystal form of leucite indicates the conditions under which it was crystallized, and the tetragonal structure shows that it has undergone post-crystallization inversion.
With the corresponding mixture and targeted heat treatment of these glasses, leucite crystals with a defined grain size distribution are released in the glass matrix.
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Examples from Classical Literature
They are chiefly leucite and nepheline rocks, such as leucitite, leucitophyre and nephelinite, but basalt and trachyte also occur.
They are of trachytic appearance, containing phenocysts of sanidine, leucite, augite and biotite.
They are rich in leucite, but contain also some sanidine and often much nepheline with hauyne or nosean.
The flows from Kibo include nepheline and leucite basanite lavas rich in soda felspars.
The former consist mainly of plagioclase, leucite and augite, while the latter contain olivine in addition.
The leucite is often present in two sets of crystals, both porphyritic and as an ingredient of the ground mass.
They are black or ashy-grey in colour, often vesicular, and may contain many large grey phenocysts of leucite.
In the lava of 1848 leucite was found to reach 44.9 per cent.
The leucite lavas of Niedermendig contain hayne in abundance.
Section of leucite crystal from the lava of 1868, with fluid cavities.
Nepheline appears to decrease in amount as leucite increases.
Leucite and nepheline rocks have been found in various parts of the island, especially in the south-west.
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