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勘探者或采矿公司更多地运用地质规律而不是大规模地使用电子设备发现了世界主要铀矿省。但是,在寻找特殊产地的铀矿体时,这些电子仪器仍有很大的价值。同位素比例研究表明,在多数情况下矿床的形成过程延续在几亿年以上,此情况加上矿相方面的证据,就可看出,对于大多数准整合矿床来说铀是后成的。寻找新的含铀省和主要铀矿床的最有利的环境是克拉通内的沉积物,冒地槽沉积物和在铀矿省内的山间盆地中的沉积物,特别是伴随有酸性火成岩侵入或喷发岩的地带。
Prospectors or mining companies are using geo-laws more than the large-scale use of electronic equipment to discover the world’s major uranium provinces. However, these electronic devices are still of great value in the search for uranium ore bodies in special producing areas. Isotopic ratio studies show that deposit formation continues for more than a few hundred million years in most cases. Coupled with evidence from the field, it can be seen that uranium is a successor to most quasi-integrated ore deposits. The most favorable environments for finding new uranium-bearing provinces and major uranium deposits are cratonic deposits, sag-bearing sediments and sediments in mountain basins within the uranium province, especially associated with acid igneous intrusions Or eruption rock zone.