Kwiindawo ezininzi zehlabathi, kunokwenzeka ukwakha ngelitye lendalo lendawo. Iimpawu ezibonakalayo zamatye endalo ziyahluka ngokubanzi ngokusekelwe kwinani leentlobo zamatye; kukho ilitye lendalo elifanelekileyo malunga nayo yonke imfuneko yezinto zokwakha. Ayinakutsha kwaye ayifuni ukufakwa, okanye ukugquma okanye ukugquma kokukhusela. Amatye athandeka ngobuhle kwaye nganye iyingqayizivele. Ngenxa yemibala emininzi eyahlukeneyo, izakhiwo kunye nemigangatho, abakhi bezakhiwo bahlala benzima ukwenza isigqibo. Ngoko ke, iimpawu ezisisiseko zokuhlukanisa, inkqubo yophuhliso, iimpawu zomzimba, imizekelo yesicelo kunye nokwahluka koyilo kufuneka kuqondwe.
Ilitye lendalo lahlulwe ngokwamacandelo amathathu ngokusekwe kwiminyaka yalo kunye nendlela eyakhiwe ngayo:
1. I-Magmatic rock:
Umzekelo, igranite lilitye eliqinileyo elenza awona maqela amadala elitye lendalo, aquka udaka olumanzi, njl. njl. Eyona granite indala efunyenwe kwimeteorites ukuza kuthi ga ngoku yakha i4.53 yebhiliyoni kwiminyaka eyadlulayo.
2. Intlenga, njengelimestone kunye nelitye lentlabathi (ekwabizwa ngokuba ngamatye entlenga):
Ivela kwixesha lamva nje lejoloji, yenziwe ngentlenga emhlabeni okanye emanzini. Amatye eSedimentary athambe kakhulu kunamatye atshisayo. Nangona kunjalo, iidiphozithi ze-limestone e-China nazo zibuyele kwi-600 yezigidi zeminyaka eyadlulayo.
3. Amatye e-Metamorphic, afana ne-slate okanye i-marble.
Kubandakanya iintlobo zamatye ezenziwe ngamatye entlenga athe adlula kwinkqubo yenguqu. Ezi ntlobo zamatye zezexesha lamva nje lejoloji. Isileyiti senziwa malunga ne-3.5 ukuya kwi-400 yezigidi zeminyaka eyadlulayo.
Ibhastile lilitye le-metamorphic elenziwe ngamaminerali e-carbonate aphindwe kabini, aqheleke kakhulu ukuba yi-calcite okanye i-dolomite.Kwi-geology, igama lemarble libhekisa kwi-limestone ye-metamorphic, kodwa ukusetyenziswa kwayo kwi-masonry ngokubanzi kubandakanya i-limestone engalungiswanga. Ibhastile lidla ngokusetyenziswa kwimizobo nakwizinto zokwakha. Ibhastile litsala umdla wabathengi ngenkangeleko yabo entle kunye neempawu ezisebenzayo. Ngokwahlukileyo kwamanye amatye okwakha, ukuthungwa kwebhastile ngalinye kwahlukile. Ngokwakheka okucacileyo kunye nokugobileyo kugudileyo, kuthambile, kuqaqambile kwaye kutsha, okukuzisela itheko lokubonwayo kwizicelo ezahlukeneyo. Ithambile, intle, indilisekile kwaye inobuhle bokwakheka, yinto efanelekileyo yokuhombisa izakhiwo ezitofotofo, kunye nemathiriyeli yemveli yomzobo wobugcisa.
Emva konyaka ka-2000, owona mgodi webhastile wawusebenzayo wawuseAsia.Ingakumbi ishishini lendalo lebhastile laseTshayina liye laphuhla ngokukhawuleza emva kohlaziyo nokuvulwa. Ngokombala osisiseko womgangatho ogudisiweyo, ilitye lebhastile eliveliswe e-China linokwahlulwa ngokweemvaba ezisixhenxe: ezimhlophe, ezityheli, eziluhlaza, ezingwevu, ezibomvu, zekofu kunye nezimnyama. , kwaye oovimba bayo bebonke babekwa kwindawo ephezulu emhlabeni. Ngokwezibalo ezingaphelelanga, ziphantse zibe ngama-400 iintlobo zebhastile laseTshayina eziphononongweyo ukuza kuthi ga ngoku.
Njengenye yeenkampani zokuqala ezikhethekileyo kwiMable yeNdalo yaseTshayina, ilitye lomkhenkce lelinye lawona mvelisi mkhulu kunye nochwephesha wendalo waseTshayina owenziwe ngebhastile eShuitou. Sisebenza nzima ngokunyanisekileyo ukumela iMarble yaseTshayina kwaye sizise umgangatho ophezulu webhastile laseTshayina njengesiqhelo "Yenziwe eTshayina".
Ixesha lokuposa: Jul-13-2022