Tag Archives: i-olivine

Okunamandla

I-Chrome Diopside: Itshe Eliyigugu Elinezici Ezihlukile Ze-Geologic

Posted on by i-miamimining
isithombe se-chrome diopside
03
uJan

I-Chrome diopside iyitshe eliyigugu elaziwa ngombala walo oluhlaza ogqamile nezici ezihlukile ze-geologic. Lelitshe eliyigugu litholakala ezindaweni ezimbalwa ezihlukene emhlabeni wonke, kuhlanganise neSiberia, eCanada nasePakistan. Kulokhu okuthunyelwe kwebhulogi, sizobhekisisa i-geology ye-chrome diopside futhi sihlole ezinye zezici zayo ezithakazelisa kakhulu.

Enye yezinto ezithakazelisa kakhulu nge-chrome diopside ukuthi yakhiwa ngenqubo ye-metamorphism. Lokhu kusho ukuthi kudalwe lapho ukucindezela okuphezulu nezimo zokushisa kubangela ushintsho ekubunjweni kwamaminerali amatshe. Le nqubo ingenzeka ngokwemvelo, njengasendabeni yokwakhiwa kwezintaba or the ukuqeqeshwa zamatshe e-metamorphic. Kungase futhi kwenziwe ngokuzenzisa, njengasesimweni sezinqubo ezithile zezimboni.

I-Chrome diopside iwuhlobo lwe-calcium magnesium silicate, okusho ukuthi yakhiwe nge-calcium, i-magnesium, namaminerali silicate. Ivame ukutholakala emadwaleni anokuqukethwe okuphezulu kwe-silica, njengemabula noma i-gneiss. Ngaphezu kombala wayo oluhlaza ohlukile, i-chrome diopside yaziwa nangokuqina kwayo nokuqina. Ine-a Ubunzima bukaMohs ka-5.5 kuya ku-6, okwenza kube nzima futhi imelane nokuguga.

Enye ye-deposit eyaziwa kakhulu ye-chrome diopside itholakala ezintabeni zase-Ural zaseSiberia. Le diphozithi yaqala ukutholwa ngasekupheleni kwawo-1800s futhi ibimbiwa itshe eliyigugu kusukela ngaleso sikhathi. Ngaphezu kweSiberia, i-chrome diopside ingatholakala naseCanada, ikakhulukazi esifundeni saseThunder Bay e-Ontario. Lapha, itshe eliyigugu litholakala kulokho okwaziwa ngokuthi “amapayipi e-diopside,” okungamapayipi entaba-mlilo asendulo akhiwa izigidi zeminyaka edlule.

Esinye isici esithakazelisayo se-geology ye-chrome diopside ukuhlotshaniswa kwayo namanye amaminerali. Kwezinye izimo, ingatholakala eceleni kwamanye amatshe ayigugu njengedayimane, i-emerald, nerubi. Ingabuye itholakale ekwakhekeni kwamatshe afanayo njengamanye amaminerali, kufaka phakathi i-pyroxene, i-amphibole, ne-olivine.

Sengiphetha, i-chrome diopside iyitshe eliyigugu elaziwa ngezici zalo ezihlukile ze-geologic. Yakhiwa ngenqubo ye-metamorphism futhi itholakala ezindaweni ezimbalwa ezihlukene emhlabeni jikelele, okuhlanganisa iSiberia, Canada, kanye nePakistan. Umbala wayo oluhlaza ohlukile, ukuqina, nokuqina kwenza kube ukukhetha okudumile kobucwebe nezinye izinto zokuhlobisa. Uma ungathanda ukufunda kabanzi mayelana ne-geology ye-chrome diopside noma amanye amatshe ayigugu, kunezinsiza eziningi ezitholakalayo ukukusiza ukuhlola lesi sihloko esithakazelisayo.

Okunamandla

I-Peridot: Umhlahlandlela Ophelele Wezazi Zomhlaba

Posted on by i-miamimining
ikristalu ye-peridot
02
uJan

I-Peridot iyitshe eliyigugu elihle osekunesikhathi laziswa ngombala walo oluhlaza ogqamile. Kodwa kuma-geologists, i-peridot ibamba ukuthakazelisa okukhethekile ngenxa yezakhiwo zayo eziyingqayizivele nokubaluleka kokwakheka komhlaba. Kulo mhlahlandlela ophelele, sizohlola izakhiwo ze-peridot, yayo ukuqeqeshwa kanye nokuvela emvelweni, kanye nokubaluleka kwayo emkhakheni wegeology.

I-Peridot iwuhlobo lwamaminerali aziwa ngokuthi i-olivine, eyenziwe ngezinto ezihlukahlukene ezihlanganisa insimbi, i-magnesium, ne-silicon. Ivame ukutholakala emadwaleni avuthayo njenge-basalt ne-gabbro, futhi ngokuvamile ihlotshaniswa nenqubo ye-plate tectonics. Eqinisweni, i-peridot ivame ukwakhiwa ngenxa yokushisa okukhulu nokucindezela ngaphakathi koqweqwe lomhlaba, okuyenza ibe ithuluzi elibalulekile lezazi zokwakheka komhlaba ezifunda umlando womhlaba nezinqubo zangaphakathi.

Esinye sezici ezihluke kakhulu ze-peridot umbala wayo oluhlaza ogqamile, obangelwa ukuba khona kwensimbi. Lo mbala ungahluka ukusuka kokuphuzi okuluhlaza kuya koluhlaza okotshani ojulile, futhi ngokuvamile uchazwa ngokuthi “okufana nepheya.” Ngaphezu kombala wayo, i-peridot nayo yaziwa ngayo ubulukhuni nokuqina, okwenza kube ukukhetha okudumile kobucwebe.

I-Peridot itholakala ezindaweni eziningi emhlabeni jikelele, ngezinye zediphozithi ezibalulekile ezitholakala ku- I-united states, China, kanye Pakistan. Itholakala futhi ngamanani amancane kwamanye amazwe anjengeBrazil, Norway, neRussia. E-United States, i-peridot ingatholakala ku Arizona, eyaziwa ngamatshe ayigugu acebile.

Njengetshe eliyigugu, i-peridot iye yaziswa amakhulu eminyaka futhi inomlando omude wokusetshenziswa ubucwebe nezinye izinto zokuhlobisa. Kuphinde kube yisinqumo esidumile sabaqoqi nabashisekayo ngenxa yezakhiwo zayo ezihlukile kanye nohlu olubanzi lwemibala. Kodwa-ke, kuma-geologists, i-peridot ingaphezu nje kwetshe eliyigugu elihle. Kuyithuluzi elibalulekile lokuqonda umlando woMhlaba nezinqubo zangaphakathi, futhi liyingxenye ebalulekile yomkhakha we-geology.

Sengiphetha, i-peridot iyiminerali ethokozisayo nebalulekile ebambe ukuthakasela okukhethekile kwezazi ze-geologists. Izici zawo eziyingqayizivele, ukuvela kwemvelo, kanye neqhaza emkhakheni we-geology kuwenza ube yingxenye ebalulekile yocwaningo loMhlaba nezinqubo zawo. Ukuthi uyisazi sokuma komhlaba or nje umthandi wamatshe ayigugu amahle, i-peridot iyimaminerali eqinisekile ukuthi izobamba ukunaka kwakho.