Tag Archives: Iso lekati le-Chrysoberyl

I-Geology ye-Chrysoberyl: Ukwakheka, Isenzeko, kanye Nezimpawu

itshe eliyigugu le-chrysoberyl

I-Chrysoberyl iyitshe eliyigugu elingandile futhi elaziswa kakhulu eliye laziswa amakhulu eminyaka ngobuhle balo obumangalisayo nokuqina. Naphezu kokuthandwa kwalo, nokho, abantu abaningi bangase bangazi nge-geology ethakazelisayo ngemuva kwaleli tshe eliyigugu. Kulokhu okuthunyelwe kwebhulogi, sizohlola ukuqeqeshwa, ukwenzeka, nezici ze-chrysoberyl kumongo we-geological.

I-Chrysoberyl iwuhlobo lwamaminerali e-silicate akhiwa i-beryllium, i-aluminium, ne-oxygen. Kuyilungu le- i-beryl umndeni, ohlanganisa i-emerald, aquamarine, futhi morganite. I-Chrysoberyl ihlukile kulawa matshe ayigugu ngoba inombala ophuzi-oluhlaza ohlukile kuya kumbala onsundu-ophuzi, obangelwa ukuba khona kokungcola kwe-chromium nensimbi.

I-Chrysoberyl ivamise ukutholakala emadwaleni e-metamorphic kanye ne-igneous, akhiwa ngokushisa nokucindezela komsebenzi we-tectonic. Ingatholakala futhi kuma-alluvial deposits, akhiwa ngokuguguleka nokuthuthwa kwamadwala ngamanzi.

Esinye sezenzakalo eziphawuleka kakhulu ze-chrysoberyl sisezintabeni zase-Ural zaseRussia, lapho itholakala khona emica schist kanye ne-gneiss formations. Itholakala nakwezinye izingxenye zeYurophu, kanye naseBrazil, eMadagascar naseSri Lanka. Kwe I-united states, i-chrysoberyl ingatholakala ku Alabama, California, Futhi Virginia.

Ngokuya ngezici zayo zomzimba, i-chrysoberyl yaziwa ngobulukhuni bayo obungavamile nokuqina. Inobunzima obungu-8.5 esikalini se-Mohs, okuyenza ibe ngelinye lamatshe ayigugu anzima kakhulu. Iphinde imelane kakhulu nokunwaya, okwenza kube ukukhetha okudumile ukusetshenziswa kobucwebe.

I-Chrysoberyl inesakhiwo sekristalu esihlukile, esibonakala ngokuma kwayo okuyi-hexagonal. Amakristalu ngokuvamile mancane, futhi avame ukwenzeka ngamaqoqo, okunganikeza itshe eliyigugu ukuguqubala. or ukubukeka kobisi.

Kunezinhlobo ezimbili eziyinhloko ze-chrysoberyl: i-chrysoberyl evamile kanye ne-cat's eye chrysoberyl. I-chrysoberyl evamile iyindlela evame kakhulu yetshe eliyigugu, futhi ibonakala ngombala wayo ophuzi-oluhlaza kuya kumbala onsundu-ophuzi. Ngakolunye uhlangothi, i-chrysoberyl yeso lekati iyivelakancane kakhulu futhi ibonakala ngokuxoxa okuhlukile, noma umphumela "weso lekati", obangelwa ukufakwa okuncane okuhambisanayo okubonisa ukukhanya ngendlela ethile.

Ngaphezu kokusetshenziswa kwayo njengetshe eliyigugu, i-chrysoberyl inenani lezinye izinto ezithokozisayo kanye nezakhiwo. Isetshenziswa ekukhiqizeni ama-abrasives ekhwalithi ephezulu, futhi iphinde isetshenziswe njengento ephikisayo, okusho ukuthi ikwazi ukumelana namazinga okushisa aphezulu futhi imelana nokuncibilika.

Sekukonke, i-chrysoberyl iyitshe eliyigugu elithakazelisayo neliyingqayizivele elinomlando ocebile nohlukahlukene we-geological. Ukuqina kwayo okungavamile, ukuqina, nobuhle bayo kuyenza ibe itshe eliyigugu elifunwa kakhulu abaqoqi nabathanda ubucwebe emhlabeni jikelele. Ngakho-ke, ngokuzayo lapho ubona ucezu lobucwebe be-chrysoberyl, thatha isikhashana ukwazisa i-geology ethokozisayo ngemuva kwaleli tshe eliyigugu elihle.