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1)  Mafic-ultramafic rocks
镁铁-超镁铁岩
1.
Petrogenetic epoch and geochemical characteristics of mafic-ultramafic rocks on the southern margin of Alxa massif in northern China;
阿拉善地块南缘镁铁-超镁铁岩形成时代及地球化学特征
2.
Platinum-group element geochemistry of Cretaceous mafic-ultramafic rocks in the Northern Dabie;
北大别白垩纪镁铁-超镁铁岩的铂族元素地球化学研究
3.
Ti-clinohumite (±Ti-chondrodite)+magnesite high pressure mineral assemblage has been discovered in mafic-ultramafic rocks of Maowu,Bixiling,Nanshanling in Dabieshan srea.
大别山超高压变质镁铁-超镁铁岩中钛斜硅镁石(±钛粒硅镁石)—菱镁矿组合成因樊祺诚,刘若新,徐平,张旗,赵大升,马宝林(国家地震局地质研究所。
2)  ultramafic rock
超镁铁岩
1.
Mafic-ultramafic rock association and the mineralization-forming specialization of Cr-Ni deposit;
镁铁-超镁铁岩的自然组合与铬镍矿床的成矿专属性
2.
Based on the occurrence of Dongchinling shonshugou ultramafic rock and the characteristics of the chromite mineralization as well as the mineral components, a comprehensive explanation of the mineralization characteristics of the various chromites, such as those of being as the accessory minerals and those of different types of ore, has been proposed through the analyses of Mssbaur spectra.
以东秦岭松树沟超镁铁岩体的产状和铬铁矿的产出特征为背景,结合铬铁矿的组分特征,对副矿物铬铁矿和不同矿石类型铬铁矿的穆斯堡尔谱进行成矿特征方面的解释;并通过与铬铁矿形成有关的宏观和微观地质现象分析,指出铬铁矿体是地幔岩高度熔融形成的富铬和镁的极端部分。
3.
On the basis of summarizing former relative works, this paper manily discusses the PGE distribution in ultramafic rock and the behaviour during partial melting, crystal frac-tionation, and alteration.
在总结前人工作的基础上,论述了PGE在超镁铁岩中的分布范围以及在部分熔融、结晶分异和蚀变作用过程中的行为规律。
3)  ultramafite
超镁铁岩
1.
Yingzuishan gold deposit lies in the intersection point of North Qilian Mts and South Altyn abruption, it is related to the ultramafite nearly in space.
鹰嘴山金矿床产于北祁连山与阿尔金南缘断裂的交汇部位,与超镁铁岩在空间上有密切的关系。
4)  ultramafic rocks
超镁铁岩
1.
Platinum-group element geochemistry of ultramafic rocks in Maowu, Dabie Mountains;
大别造山带毛屋超镁铁岩的铂族元素研究
5)  Ultramafic rock
超铁镁岩
6)  mafic-ultramafic rocks
镁铁-超镁铁质岩
1.
Geochemical characteristics of mafic-ultramafic rocks and their geological significance in Hongqiling mine of Jilin;
吉林红旗岭镁铁-超镁铁质岩的地球化学特征及地质意义
2.
Both copper-nickel sulfide (CNS) deposit and vanadic titianomagnetite (VTM) deposit are related to mafic-ultramafic rocks and belong to the orthomagmatic mineral deposit, but they rarely coexist on one deposit.
铜镍硫化物矿床与钒钛磁铁矿矿床虽然同属与镁铁-超镁铁质岩有关的岩浆型矿床范畴,但在一般情况下,二者是不共生的。
3.
Cu-Ni sulphide deposit related to mafic-ultramafic rocks is the main type of copper, nickel,platinum group elements(PGE) deposits.
与镁铁-超镁铁质岩密切相关的铜镍硫化物矿床是铜、镍、铂族元素(PGE)资源的重要矿床类型。
补充资料:荷兰铁
荷兰铁
  又称巨丝兰、象脚丝兰、无刺丝兰,为百合科丝兰属观叶植物。荷兰铁为常绿木本植物,在原产地株高可达10米,盆栽的株高多为l一2米。茎干粗壮、直立,褐色,有明显的叶痕,茎基部可膨大为近球状。叶窄披针形,着生于茎顶,末端急尖,长可达100厘米、宽约8~10厘米;叶革质,坚韧,全缘,绿色,无柄。喜阳也耐阴,耐旱,耐寒力强。生长适温为15~25℃,越冬温度为0℃。对土壤要求不严,以疏松、富含腐殖质的壤土为佳。
  荷兰铁常用扦插繁殖。扦插在整个生长季均可进行,但以春秋季较好。扦插时剪取10~30厘米的芽,待伤口稍晾干后基部沾上黄泥浆,扦插于干净河沙中,一个月左右即可生根。也可截取30~40厘米长的茎段,用杀菌剂消毒伤口后沾上黄泥浆,横卧于沙床,覆沙1/2~2/3,使茎段隐芽萌发;或将茎段顶端封上石蜡,插于沙床中,使上部隐芽陆续萌发。当芽体长到10厘米以上时剪下来扦插。
  荷兰铁盆栽可用园土、腐叶土和河沙等量混合作为培养土。生长季保持盆土湿润即可,避免浇水过多,引起积水,而使根部和茎干腐烂。它生命力旺盛,对肥料要求不高,生长旺盛期每月施3~2次液肥即够。荷兰铁生长要求充足的阳光,除了炎热夏季需适当遮阴外,其它季节可在全日照下生长。它喜阳也耐阴,可适应不同光线环境。但也不宜过于阴蔽,否则抽长的新叶往往不易老化且发黄,或引起徒长、叶片不健壮而下垂。荷兰铁在高温高湿条件下极易发生叶斑病,韧发时吁尖叶缘呈黑褐斑迹,严重时蔓延到叶片大部分,应及时防治。
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