Top X Scientia et Technology News of Rare terra in Sina in MMXXII (I)

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, debitum ad cohiberi mei explorationem aliquip, rara terra Mineralization doctrina et exploratio technology, ibi fuisse diversis intellectationibus et ingens metallum locupleti mechanism, aes corpus et efficacius et potentias rara terrae opes . Ut declarare in formatione mechanism de Bayan OBO depositum et aestimare potentiale opes rara terra, Institute of Geologicum et Geophysics de Seres Academiae Scientiarum Deployed Key Projects et cooperari cum BaoTou Ferrum et Steel (Groups et Coopered cum BaoTou Ferrum et Steel (Groups et Coopered cum BaoTou Ferrum et Steel (Groups et Coopered cum BaoTou Ferrum et Steel (Groups) Cooperavit BaoTou et Steel (Groups) Cooperavit BaoTou Ferrum et Steel (Groups) Co., . Et affiliatam unitates ad portare de detailed regional Geological Survey: Revision of I: (V) SCIENTIA Geological Map, multi-modum et 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 figura de ore-afferentem geological corpus construitur, et potentiale rara terra opibus fuisse reassessed. (I) Baiyunebo area habet periti multiplex tectonic motus. Ante emplacement carbonate saxa, in mane-medio proterozoic sedimentary saxa (Baiyunebo Group Quartz Sandstone, conglomerate, rasa, etc.) in Mining Area subeundi regional compressional tectonica et in area calculo Crustulam structuram, myononite, complicare, etc. Et nuper formatae fere EW trending et ardua tectonic schistosity providet prospera alveo ad upwelling de 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.

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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).

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Fig. III spatio distribution exemplar de carbonatite in Baiyunebo Depositum

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(IV) Baiyunebo carbonatitus habet magnum volumen et excelsum gradum evolutionis, quae est key factor ad eius ingens rara terra cumulus. Ex adeptus distribution range, volumine et (minimum) density carbonate petram massa (rara terra os corpus), et usura in II% rara terrae contentus totius petra carbonate a notitia per annos), quod est aestimari quod potentiale resource of vadum rara terra cadmiae in Baiyunebo Mining area est CCCXXXIII million talentorum, quae est fere X temporibus in Baiyunebo, quod nuper ex XXXVI decies centies in Talum Rare Resources (including Bayan OBO) by Civitatibus Foederatae Geological Survey est 2.78 temporibus CXX million tons.

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Post tempus: Mar-02-2023