查询词典 ores
- 与 ores 相关的网络例句 [注:此内容来源于网络,仅供参考]
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As a result of human activities such as mining and smelting of metalliferous ores, electroplating, gas exhaust, energy and fuel production, fertilizer and pesticide application, etc., metal pollution has become one of the most serious environmental problems today.
由于人类活动,例如采矿和金属矿石的冶炼,电镀,能源和燃料生产,肥料和杀虫剂应用,等等,金属污染变成今天最严重的环境问题之一。
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Gize A P%Manning D A C Aspects of the organic geochemistry and petrology of metalliferous ores New York:Plenum Press , 1993,null
庄汉平 与有机质有成因联系的金属矿床地质地球化学, 1996,(4)涂光炽中国层控矿床地球化学北京:科学出版社, 1988,null
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Sulfur isotope measurements of deposits such as those in the 1.1 Ga Duluth Complex, the Per-mo-Triassic intrusions of the Noril'sk area, and the 1.4 Ga Kabanga intrusions provide evidence for the derivation of S from both sulfide-and sulfate-bearing country rocks. The 1.3 Ga Voisey's Bay deposit provides an example where δ^34 S values of the ores commonly fall within the accepted mantle range of 0±2‰, but detailed studies of Proterozoic metasedimentary country rocks show that their weighted average δ^34 S value is also within this range.
如1.1 Ga的Duluth杂岩、Noril'sk地区二叠-三叠纪侵入岩和1.4 Ga的Kabanga侵入岩体中矿床的硫同位素测定结果证明硫来自含硫化物和硫酸盐的围岩。1.3 Ga的Voisbey's Bay矿床矿石的硫同位素δ^34 S值通常落入公认的地幔硫同位素组成范围(0±2‰)内,而对其元古宙变质沉积围岩进行的详细研究结果显示δ^34 S的平均值也在此范围。
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Sulfur isotope measurements of deposits such as those in the 1.1 Ga Duluth Complex, the Per-mo-Triassic intrusions of the Noril'sk area, and the 1.4 Ga Kabanga intrusions provide evidence for the derivation of S from both sulfide-and sulfate-bearing country rocks. The 1.3 Ga Voisey's Bay deposit provides an example where δ^34 S values of the ores commonly fall within the accepted mantle range of 0±2‰, but detailed studies of Proterozoic metasedimentary country rocks show that their weighted average δ^34 S value is also within this range.
如1.1 Ga的Duluth杂岩、Noril'sk地区二迭-三迭纪侵入岩和1.4 Ga的Kabanga侵入岩体中矿床的硫同位素测定结果证明硫来自含硫化物和硫酸盐的围岩。1.3 Ga的Voisbey's Bay矿床矿石的硫同位素δ^34 S值通常落入公认的地幔硫同位素组成范围(0±2‰)内,而对其元古宙变质沉积围岩进行的详细研究结果显示δ^34 S的平均值也在此范围。
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Sulfur isotope measurements of deposits such as those in the 1.1 Ga Duluth Complex, the Permo-Triassic intrusions of the Noril'sk area, and the 1.4 Ga Kabanga intrusions provide evidence for the derivation of S from both sulfide-and sulfate-bearing country rocks. The 1.3 Ga Voisey's Bay deposit provides an example where δ34S values of the ores commonly fall within the accepted mantle range of 0 ± 2‰, but detailed studies of Proterozoic metasedimentary country rocks show that their weighted average δ34S value is also within this range.
如1.1 Ga的Duluth杂岩、Noril'sk地区二叠-三叠纪侵入岩和1.4 Ga的Kabanga侵入岩体中矿床的硫同位素测定结果证明硫来自含硫化物和硫酸盐的围岩。1.3 Ga的Voisbey's Bay矿床矿石的硫同位素δ34S值通常落入公认的地幔硫同位素组成范围(0±2‰)内,而对其元古宙变质沉积围岩进行的详细研究结果显示δ34S的平均值也在此范围。
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Various "metasomatic textures" of ores were foimed in diagentic stage.
矿石中的&交代结构&形成于成岩期。
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The wolframite, scheelite, tantalum niobite and fine spar have uneven distribution in the raw ores. Relatively, the wolframite and scheelite have coarse embedded granularity, generally 0.8 ~ 0.04 mm. The tantalum niobite and fine spar have fine embedded granularity, generally 0.2 to 0.04 mm.
原矿中黑钨矿、白钨矿、钽铌铁矿、细晶石的嵌布粒度皆为不均匀嵌布,黑钨矿与白钨矿的嵌布粒度相对较粗,一般为0.8~0.04毫米,而钽铌铁矿及细晶石的嵌布粒度则很细,一般为0.2~0.04毫米。
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The abundant mineral resources in Hubei Province are characterized by large variety, large scale, relatively concentrated distribution, and many paragenetic and accompanying mineral ores, but by a deficiency in some energy in great demand and some badly_needed mineral resources.
湖北省矿产资源丰富,具有矿产种类多、规模大、分布相对集中、共生矿多、部分大宗能源和急需矿产资源不足的特点。
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Esistence of periclasite and wollastonite and the feature of the texture and structure of ores indicate existence of contact metamorphism in formation of the deposit.
但方镁石、硅灰石等矿物的存在和矿石结构构造的特点,表明矿床的形成还存在接触变质作用,矿床成因应属于区域变质-接触变质复合类型。
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The precent development,including development of new leaching processes and equipment and soon,in bacteria leaching of uranium and gold ores at home and abroad are described in this paper.
阐述了目前国内外微生物浸出技术在铀、金矿石中的最新进展,包括浸出新工艺的研究、浸出设备的研制等,并提出了建
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