"Violane", the manganese rich violet to blue variety of diopside, is quite uncommon, found in Italy, Greece, and California, according to mindat.org.
Most reports of chrome diopside are found in Libby, Montana. Though there have been reports of finding these kinds of diopside in Canada, South Africa, Russia and Brazil.
Yes, Russian diopside and chrome diopside are the same gemstone. Chrome diopside is a variety of diopside that is deep green in color due to its chromium content. It is often referred to as Russian diopside because it is primarily sourced from Russia.
chrome diopside and quartz are two different gemstones. Chrome diopside is sometime found along with quartz and hence the name.
Rarity is relative, and debateable. I think it's safe to say that diopside is not considered to be a rare mineral, though large, transparent green well-formed crystals of diopside are indeed rare, as are fine, large and clean faceted stones.
chrome diopside
Examples: ruby, emerald, diopside, tourmaline.
Russian diopside is a type of mineral composed primarily of calcium, magnesium, and silica, with the chemical formula CaMgSi2O6. It is a member of the pyroxene group of minerals and is characterized by its deep green color, often found in metamorphic rocks. The presence of chromium can enhance its color and make it more valuable as a gemstone. Russian diopside is particularly known for its vibrant hues and clarity, making it popular in jewelry.
The cast of La Vision - 2006 includes: Violane Chavet Jim Eng Barbara Milot Sean Perham
Garnet, Almandine, Grossular, Andradite, Uvarovite, Diopside, Melanite, and Spessartine.
Pyroxenite is an ultramafic igneous rock consisting essentially of minerals of the pyroxene group, such as augite and diopside
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The diopside-anorthite system refers to a binary mineral system in the context of geology and petrology, specifically concerning the solid solutions between the minerals diopside (CaMgSi2O6) and anorthite (CaAl2Si2O8). This system is significant in understanding the crystallization of igneous rocks, particularly in the formation of plagioclase and pyroxene minerals. The phase diagram of this system illustrates how temperature and composition affect the stability and formation of the two minerals, influencing the textures and properties of the resulting rocks. It plays a crucial role in the study of magmatic processes and the evolution of the Earth's crust.