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oxidized mn deposit
相关语句
  氧化锰矿床
     Formation of the oxidized Mn deposit is controled by the primary Mn ore layer, tectonics, geomorphology, thickness and lithology of the cover rock, climate and hydrogeological condition.
     认为表生富集型氧化锰矿床的形成主要受原生含锰层、地质构造、地形地貌、顶盖层厚度、岩性、气候及水文地质等条件所制约。
短句来源
     The genesis of the deposit belongs to the compound type of oxidized Mn deposit formed from two types of condensation and leaching.
     矿床成因属淋积、凝聚两种类型共存的复合型氧化锰矿床
短句来源
  相似匹配句对
     Mn?
     Mn的分布 ,晶界高于晶内 ,但差别不大 ;
短句来源
     OXIDIZED Mn ORE TYPES AND THE ORE-FORMING CONDITIONS
     广西氧化锰矿类型及成矿条件
短句来源
     then the raw material p xylene is oxidized to p tolualdehydeby Mn (Ⅲ).
     Mn(Ⅲ)氧化对二甲苯生成对甲基苯甲醛。
短句来源
     /Mn?
     /Mn?
短句来源
     THE DEPOSIT TYPE AND WASHABILITY OF OXIDIZED ORE IN THE SANBAO AG-MN DEPOSIT,MALIPO
     麻栗坡三保银锰矿床氧化矿石的选冶性能及其矿床类型
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Geological setting, features of the ore bearing rock assemblages, depth, ore structure and texture and mineralogy of Dongping supergene-enriched Mn doposit are discribed in the paper.Formation of the oxidized Mn deposit is controled by the primary Mn ore layer, tectonics, geomorphology, thickness and lithology of the cover rock, climate and hydrogeological condition.Based on the mentioned above metallogenic model of the deposit is established. The model can be applied to mining and futher...

Geological setting, features of the ore bearing rock assemblages, depth, ore structure and texture and mineralogy of Dongping supergene-enriched Mn doposit are discribed in the paper.Formation of the oxidized Mn deposit is controled by the primary Mn ore layer, tectonics, geomorphology, thickness and lithology of the cover rock, climate and hydrogeological condition.Based on the mentioned above metallogenic model of the deposit is established. The model can be applied to mining and futher prospecting.

本文主要论述广西东平表生富集型氧化锰矿床成矿地质环境、含锰岩系地质特征,锰矿层结构,矿石矿物成分及结构构造,矿石化学组分等特征;认为表生富集型氧化锰矿床的形成主要受原生含锰层、地质构造、地形地貌、顶盖层厚度、岩性、气候及水文地质等条件所制约。文章最后讨论了锰矿化富集特征,氧化锰矿成矿模式等并指出探采意义。

WT5”BZ]The oxidized ore of Datangpo manganese deposits in Shongtao occurs in dolomite of Sinian System Tiesiao Formation, its shape appears to be bedded,lenticular or podiform, with length 800~1200m and average thickness 1.38~1.42m and average Mn's content 29.73%~36.11%.The genesis of the deposit belongs to the compound type of oxidized Mn deposit formed from two types of condensation and leaching.

贵州松桃大塘坡锰矿床氧化锰矿产于震旦系铁丝坳组白云岩中 ,呈层状、似层状、透镜状及豆荚状 ,长 80 0~ 12 0 0m ,厚度平均 1 38~ 1 4 2m ,平均含Mn2 9 73%~36 11%。矿床成因属淋积、凝聚两种类型共存的复合型氧化锰矿床。

 
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