Into esemhlabeni ilungu elibalulekileyo lezinyithi eziphambili. I-China elinqabileyo le-China elinqabileyo lomhlaba lingaphezulu kwaye ikakhulu livela eBaiyun Obo, idipozithi enkulu enqabileyo emhlabeni. Nangona kunjalo, ngenxa yokunqongophala kweenjongo zam zokuhlola, iteknoloji enqabileyo yomhlaba kunye netekhnoloji yokuphononongwa, kuye kwakho ukuqondwa okwahlukileyo kwendlela enkulu yentsimbi, izixhobo ze-ore zomzimba ezinamandla kunye nezixhobo ezinokubakho, ezithi ngokufanelekileyo izixhobo zomhlaba ezinqabileyo . Ukwenzela ukucacisa indlela yokwenziwa kwendlela ye-Bayan Obo kwaye uvavanye ubutyebi bomhlaba onqabileyo, i-geology kunye ne-geophymy ye-Chinagy ye-China ye-China ye-Baotou kunye neSteel (i-LTD . Kwaye iiyunithi zakudala ezidibeneyo zokwenza uphando oluneenkcukacha zengingqi, ukuhlaziywa kwemephu ye-1: 5000 yeMephu yeJografi, i-Multi-Indlela kunye noPhononongo oluBala oluBala kunye noPhakathi lweMfihlakalo kwi-Bayan Obo. Ngophando oludibeneyo lwe-geology, i-geochemists, igeophysics kunye nolunye uhlobo lwe-Ibon Obo lityhilwe iMagma ye-Barbonatite ye-Barbonatite kunye ne-Carbonatite yendlela ye-Ore-Collarism icacisiwe, ezontathu- Ubume obukhulu bomzimba we-ore of ore we-ore of ores, kwaye ubutyebi bomhlaba onqabileyo bubonakale. (1) Indawo yeBaiinebo ifumene intshukumo ye-tectonic. Phambi kokuba kubeka i-EMPT yamatye e-carbonate, i-rock-proterozoic protheraticary ye-proterozoic (i-baiinebor ye-temz ye-sallz, i-conlomerate, i-stramomerate yentshukumo ye-tectorical ithathelwe indawo ye-Gravel Isakhelo sekhekhe, i-My.nloni, njl njl. Ukusasazwa, uphawu kunye nolwalamano phakathi kwasekuqaleni nasemva kwexesha kwe-sedimentary rocks yeqela leBailinebo leBailinebo kwiNdawo yeMigodi kufuneka iphinde ihlolwe.
Umzobo 1 Imbali yoPhuculo lweMbali kunye ne-carbonatite emveliso ye-IsoProProzoic Bayan Obo Basin
. Iliwa le-carbonate lilitye lomzali elinqabileyo lomhlaba onqabileyo kunye noMhlaba onqabileyo onqabileyo. Ukuqokelelwa kwezinyithi ezinkulu eBayan Obo kwenzeka kwi-1,3 yezigidigidi. I-carbonic magma inemikhwa yendaleko-i-Iron-Magnareous-Collsous, kunye nezinto ezinqabileyo zomhlaba kumanzi anqabileyo, ngakumbi imilo yokukhanya enqabileyo, ibonisa imeko yokuphucula kancinci. Emva kokwenziwa kwedipozithi, yenziwa iyelenqe lazo ezimbini kwi-paleozoic yokuqala (450 ~ 400 yeminyaka) kunye nePaleozoic yePaleozoic (280 ~) ngokwahlukeneyo. Inkqubo yenguqu yakhokelela ekusebenzeni komhlaba onqabileyo kunye nokwenziwa kwezimbiwa ezintsha, kodwa kwakungekho bunye kumhlaba onqabileyo wamazwe angaphandle.
. I-ore ephambili kunye ne-East Ore yeyona ndawo iphambili yokusasazwa komzimba we-magnetic. I-ore ephambili kunye ne-East Ore iqhagamshelwe kwiindawo zokuhambisa i-carbonate, kunye nobunzulu bophuhliso lwamatye e-carbonate bukhulu. Umzimba ophakamileyo we-anomaly kunye nomzimba ophantsi wokungamelana ne-abmaly mzimba uveza ukusasazwa kwemilinganiselo emithathu yelitye le-carbonate yelitye (umzimba ore) (Fig. 2). I-carbonatite kwi-Bayan Obo ineziko le-EMPTALS kwaye iyonwabele itshaneli efanayo ye-magma kwinxalenye enzulu. Iziko liphakathi kwe-ore enkulu kunye ne-ore empuma. Emva kokubekwa kwe-magma esekwe kwi-carbma, i-stiep eyenziweyo ngokutshintshwa kwesakhiwo kwangoko ityhilwe kwi-West (i-West yam) nakwimpuma (iHuahua) ngokwakhayo (i-huhua). 3).
Umzobo 3 Imodeli yokuHamba yeSpatial ye-carbonatite kwi-bainenebo idipozithi
. Ngokusekwe kuluhlu olufumanayo lokusasazwa, ivolumu kunye (ubuncinci) ukuxinana kwe-Carbonate Rock (i-ore yomhlaba onqabileyo), kwaye usebenzisa i-2% yomhlaba onqabileyo welitye le-carbonate (ngokusekwe kwixabiso le-carredvate efunyenwe kwidatha Kwiminyaka edlulileyo, kuqikelelwa ukuba ubutyebi obungaphantsi komhlaba onqabileyo emhlabeni yi-Bainenebo yimigodi ye-bainenebo ziitoni ezizigidi ezingama-36 ezizigidi zeetoni ezizigidi ezingama-36 ezi-bainenebo, zisandula ukuqqwa kuzo zibonakaliswe emhlabeni IZIXHOBO
Imveliso enqabileyo yomhlaba i-Pls Qhagamshelana nathi
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IXESHA LOKUQALA: UMar-02-2023