造巖氧化物 的英文怎麼說

中文拼音 [zàoyányǎnghuà]
造巖氧化物 英文
rock-forming oxides
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : 名詞[化學] (氣體元素) oxygen (o)
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • 氧化物 : oxide; oxyde; oxidizing material; oxidate
  • 氧化 : [化學] oxidize; oxidate; oxide; burning; rust; oxygenize; oxido-; oxy-
  1. The microscopical observation proves that the main types of granitoid rocks are granodiorite and quartz monzodiorite, and the enclave is mainly monzodiorite. the rock - forming minerals are mainly k - feldspar, plagioclase, amphiboie, biotite, quartz, magnetite, titanite, apatite, epidote, etc. the zonation of the feldspars is very popular. the dark - colored minerals, such as biotite and titanite, have been highly oxidized

    通過對本區花崗類樣品進行顯微觀察研究,知其主要的石類型為花崗閃長、石英二長閃長,其中的石包體主要為二長閃長,其為鉀長石、斜長石、角閃石、黑雲母、石英、磁鐵礦、榍石、磷灰石和綠簾石等,長石中環帶現象比較常見,黑雲母、榍石等暗色礦顏色較深,表明其程度較高。
  2. The thickening may be synthetically aroused by many factors, because of the lower maturation of source rock at forepart, the rock tar is thicker, and then many other factors impel it, which include the hydrocarbon dissipation at the process of oil and gas migration, biodegradation and bathing oxidation induced by gravity induced centripetal flow recharged by meteoric water at the basin uplift period and etc

    稠油成藏則由多因素綜合作用成,由於早期源成熟度較低,原油本身較稠,而油氣運移過程中輕質組分散失、生降解和盆地抬升剝蝕階段大氣水下滲所導致的水洗等作用則使其進一步稠
  3. Comparing with the granitoid from jiaodong guojialing in mineralogy, the minerals in the granitoid in nimu - qushui granitoid crystallized in the environment of oxidization, the granitoid has a characteristic of rich volatile components and a high content of alkali, the rock - forming minerals and accessory minerals have a characteristic of i - type granite, and the granite shows a characteristic in favor of an and cu ore formation

    通過與膠東郭家嶺地區的花崗類的礦學進行對比,可知本區花崗類礦結晶時處于狀態,具有富含揮發分的特徵,堿質含量高,及副礦表現出型花崗特徵,具有殼幔混源質,表現出有利於金、銅礦形成的花崗類的礦特徵。
  4. The zijinshan fluid system and the gonglang fluid system were driven by the stress of extrusion nappe onto the basin and the thermal driving force of magmatism. when the fluids cycling in the basin encountered the boundary of reduction - oxidation or underwent fluid mixing, phase separating and fluid boiling caused by fault - induced pressure reducing, the physical chemistry condition abruptly changed and mineralization then took place

    在盆地兩側擠壓推覆構應力及漿作用熱力驅動下,紫金山背斜和公郎弧兩大流體系統的流體在盆地中運動,當遇到還原界面或遭受流體混合、相分離及斷裂導致的減壓沸騰時,因學條件發生重大變而導致成礦作用的發生。
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