scheelite

Tungsten was the old Swedish name for the mineral scheelite.

Conversely, synthetic scheelite is often without such a spectrum.

Two ores which have tungsten in them are wolframite and scheelite.

Along with scheelite, the wolframite series are the most important tungsten ore minerals.

This resulted in ventures such as extracting scheelite from King Island.

Cronstedt also discovered the mineral scheelite in 1751.

These factors combine to result in scheelite's high lustre and perceptible "fire", approaching that of diamond.

The ore minerals of tungsten include wolframite, scheelite, and ferberite.

Its important ores include wolframite and scheelite.

The ore consists mainly of Scheelite.

Much less common than colorless zircon is colorless scheelite.

The tetragonal crystals are hemihedral with parallel faces (like scheelite), and at times of considerable size.

The road is also known as Nevada Scheelite Mine Road.

Fluorescence of scheelite, sometimes associated with native gold, is used by geologists in the search for gold deposits.

The name was later used to describe the metal, while the ore itself was given the name scheelerz or scheelite.

It was a thriving mining town where scheelite was extracted from an open cut mine until 1974 when two underground mines were brought into production.

Scheelite was an unincorporated community in Inyo County, California.

Synthetic scheelite produced via the Czochralski process is available, but it has never been widely used as a diamond simulant.

Aside from pseudo-octahedra, scheelite may be columnar, granular, tabular or massive in habit.

Distinctly artificial curved striae and clouds of minute gas bubbles may also be observed in synthetic scheelite.

Similar materials are calcium tungstate (scheelite) and zinc tungstate.

In the southeast is Grassy, a former scheelite mining boomtown, abuzz with rumours of the mine reopening.

It forms a solid solution series with scheelite (calcium tungstate, CaWO).

Its associated minerals include pyrite, chalcopyrite, quartz, anhydrite, fluorite, and scheelite.

This compound is isostructural with the mineral scheelite (CaWO).