baddeleyite मीनिंग इन हिंदी

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It has been observed that baddeleyite without twinning is extremely rare.
Baddeleyite was first found in Sri Lanka in 1892.
It has been observed in thin section that baddeleyite forms within plagioclase grains.
Because of this, the coordination of baddeleyite was determined to be sevenfold.
This explains baddeleyite's tendency to twin along the ( 100 ) planes.
Its most naturally occurring form, with a monoclinic crystalline structure, is the mineral baddeleyite.
Zircon and baddeleyite incorporate uranium atoms into their crystalline structure as substitutes for zirconium, but strongly reject lead.
Baddeleyite forms in igneous rocks low in silica, it can be found in rocks containing potassium feldspar and plagioclase.
It occurs as interstitial grains with zirconolite, baddeleyite, and apatite associated with late stage intergrowths of quartz and feldspar.
Baddeleyite's structure is a combination of tetrahedrally coordinated oxide ions parallel to ( 100 ) with triangular coordinated oxide ions.

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