Terra elementum est momenti membrum est Key metallis. Sinis scriptor rara terra resource est superior et maxime est a Baiyun OBO, a rara super-magna rara terra depositum in mundum. Tamen, ex angustiis meis explorationem aliquip, rara terra Mineralization doctrina et exploratio technology, ibi fuisse diversis intellectationibus suis ingens metallum locupletam mechanism, aes corpus et efficacius et potentias rara terrae resources. In ordine ad declarare formationem mechanism de Bayan OBO depositum et aestimare potentiale opibus rara terra, Institute of Geologicum et Geophysics de Seres Academiae Scientiarum Draconum Steel et Culpa, Detailed of Geolog Survey: Multi-Map: Multi-scale comprehensive geophysical circumspectis et metallogenic investigationis in Bayan OBO. Through the joint research of geology, geochemistry, geophysics and other disciplines, the evolution process of Bayan Obo carbonatite magma and the enrichment mechanism of rare earth have been revealed, the carbonatite emplacement mechanism and structural ore-control factors have been clarified, the three-dimensional shape of the ore-bearing geological body has been constructed, and the potential rare earth resources have iam reassessed. (I) Baiyunebo area habet periti multiplex tectonic motus. Antequam in emplacement carbonate saxa, in mane-medio protererozoic sedimentary saxa (Baiyunebo Group Quartz Sandstone, conglomerate, slate, etc.) in Mining Area subeunda sunt reponi a structuram tectonicum, et in aram tectonico Schistosity providet prospera channel ad upwelling carbonated magma of ~ 1.3 billion annis (Fig. I). Distribution, attributionem et necessitudinem inter diluculo et sero de sedimentary saxa in medio proterozoic baiyunebo coetus in mining area opus est re-explorabilis.
Fig. I progressionem historiae et carbonatite emplacement de Mesoproterozoic Bayan OBO Basin
(II) Baiyunebo H8 Dolomite est Ignous carbonate petra, quae est obvious MOLESTUS contactus necessitudinem cum ambiente petra. Carbonate petra est parens petram rara terra mineralization et quoque rara terra os corporis. Et cumulus mole metalla in Bayan OBO occurrit in ~ 1.3 billion annis. Carbonic magma has a trend of evolution from iron-magnesium-calcareous, and the rare earth elements in carbonate rocks at different stages, especially light rare earth elements, show a trend of gradual enrichment. Post formationem depositum, quod subruit duo mutatio in primis Paleozoic (CDL ~ CD decies annis) et late paleozoic (CCLXXX ~ CCLX decies annis) respectively. Et transformatio processus ducitur ad activation rara terra et formatio novae mineralium, sed non manifestum praeter ex aliena rara terra.
(III) De distribution carbonate saxa revelata ab inversione eventus magnetica anomalias habet basic characteres ex oriente-West distribution. Pelagus ore et orientem ore sunt principalis areas de magnetica corporis distribution. Pelagus ore et orientem ore sunt connected carbonate petram distribution areas, et progressionem profundum carbonate saxa est magna. High magnetica anomaliae corpus humilitatem resistentibus anomaliae Corpus revelare tres dimensiva distribution carbonas petra (ore corpus) (Fig. II). In carbonatite in Bayan OBO habet in emplacement centrum et fruitur idem magma alveo in altum pars. In centro sita inter pelagus ore et orientis ore. Post emplacement of carbonated magma, quod ardua foliation formatae per replacement de mane structuram est pushed ad Occidentem (West mea) et ad orientem (huahua) respectively et ad orientalem (huahua) respectively et bifurcation et canentes fieri (Fig. III).
Fig. III spatio distribution exemplar de carbonatite in Baiyunebo Depositum
(IV) Baiyunebo carbonatitus habet magnum volumen et excelsum gradum evolutionis, quae est key factor ad eius ingens rara terra cumulus. Based on the obtained distribution range, volume and (minimum) density of carbonate rock mass (rare earth ore body), and using the 2% rare earth content of the whole rock of carbonate rock (based on the conservative average value obtained from the data over the years), it is estimated that the potential resource of shallow rare earth oxide in Baiyunebo mining area is 333 million tons, which is nearly 10 times the current recognized value of XXXVI million tons in Baiyunebo, quod nuper dimisit global totalis probatum rara terra opibus (including Bayan OBO) by Civitatum Foederatarum Geological Survey is 2.78 temporibus CXX million tons.
Inquiriy rara terra productum pis contact us
sales@shxlchem.com
Post tempus: Mar-02-2023