jadeite in English

noun
1
a green, blue, or white mineral that is one of the forms of jade. It is a silicate of sodium, aluminum, and iron and belongs to the pyroxene group.
In particular, it would have been good to include fancy colored sapphires (other than padparadsha), demantoid, jadeite , red beryl, and benitoite, to name a few.

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1. 4 According to Electron probe analysis , the secondary color cranny and clearance of jadeite.

2. In China and Japan, jade and jadeite are most popular for jewelry, ornaments, and incense burners.

3. Jadeite is a pyroxene, silicate of aluminum, and was not used in China to any extent until 1784.

4. 2 According to Electron probe analysis, the secondary color is formed because of the iron compounds in the cranny and clearance of jadeite.

5. The Jadeite Cabbage is green on one end and white on the other, and it has cracks and ripples.

6. Unlike the majority of almandine-jadeite eclogites, two examples contain garnets with almandine-cores and pyrope-rich rims without accompanying variation in grossular content.

7. Augite, diopside, jadeite and spodumene are four of the best-known members of the pyroxene group; however, the pyroxene group has many other members

8. Albitic jadeite, by contrast, a Na-rich analogue of tissintite, is super-silicic, vacancy-rich pyroxene with excess Si coordinated in the octahedral M1 site.

9. Most of the eclogites examined are of the almandine-jadeite type and zonal and irregular variation in grossular content of garnet and acmite, jadeite and diopside-hedenbergite content of pyroxene produce large uncertainties in temperature estimates based on Fe/Mg partitioning between garnet and clinopyroxene. Zoning pattems of increasingXMg in both clinopyroxene and garnet, and increasingXJd in clinopyroxene, suggest the introduction of Mg and Na throughout the evolution of these essentially bimineralic assemblages.

10. What makes the Jadeite Cabbage so amazing is that this anonymous master carver used the weaknesses of the jade—the two colors, the cracks, and the ripples—to make the cabbage all the more lifelike.

11. Two samples contain pyrope-rich gamets but coexisting pyroxenes are extremely magnesian and temperatures of equilibration of both primary omphacite-pyrope and secondary omphacite-almandine/pyrope-chlorite are only slightly higher (500–650° at 10 kbar) than those for almandine jadeite eclogites and estimates overlap with those of some examples of the latter type.