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Schorl and lithium-rich tourmalines are usually found in granite and granite pegmatite. Magnesium-rich tourmalines, dravites, are generally restricted to schists and marble. Tourmaline is a durable mineral and can be found in minor amounts as grains in sandstone and conglomerate, and is part of the ZTR index for highly weathered sediments. [24]
Elbaite, a sodium, lithium, aluminium boro-silicate, with the chemical composition Na(Li 1.5 Al 1.5)Al 6 Si 6 O 18 (BO 3) 3 (OH) 4, [4] is a mineral species belonging to the six-member ring cyclosilicate tourmaline group.
The reef system is protected as the Tourmaline Reef Nature Reserve (Reserva Natural Arrecife de Tourmaline), managed by the Puerto Rico Department of Natural Resources (DRNA) which provides management plans and conservation resources that limit the fishing activities in the area for the purpose of preserving its delicate ecosystem, previously threatened by the overfishing of red grouper ...
Rubellite is the red or pink variety of tourmaline and is a member of elbaite. Rubellite is also the rarest gem in its family. [2] It is occasionally mistaken for ruby. [3] These gems typically contain inclusions. [4] Notable countries where rubellite can be mined include Afghanistan, Brazil, Madagascar, Myanmar, Nigeria, Russia, and the United ...
Fluor-buergerite, [5] originally named buergerite, is a mineral species belonging to the tourmaline group. It was first described for an occurrence in rhyolitic cavities near Mexquitic, San Luis Potosi , Mexico .
The mineralogy of the gem deposits varies widely with, among others, corundum (sapphire, ruby), chrysoberyl, beryl, spinel, topaz, zircon, tourmaline, garnet being common. [2] Residual deposits are mainly found in flood plains of rivers and streams. The metamorphic types of gems constitute 90% of the gem deposits in Sri Lanka.
Tourmaline also comes in the colors: orange (sometimes called Pumpkin Tourmaline) and purple (Siberite when found in Russia, but also found in California). Radiation can be used to change the color (if I remember right, this was in a paper >30 years ago by an AT&T or Bell Labs researcher).
The existence in nature of some questionable/ doubtful minerals is very unlikely at all or at the type locality. For example, chloromagnesite Q (Y: 1872, MgCl 2) 3.AB.20 and zinkosite Q (Y: 1852, ZnSO 4) 7.AB.10. [52] [53] Some names are not names of minerals anymore, but names of a group of minerals: Micas, biotite group. [54] [nb 1] [55]