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mn deposit    
相关语句
  锰矿
    THE CHARACTERISTICS OF THE MIDDLE ORDOVICIAN HIGH - QUALITY Mn DEPOSIT IN CENTRAL HUNAN
    湘中中奥陶世优质锰矿主要地质特征
短句来源
    Application of Dry Filling Mining Method Through Drifting-Slicing in Heqing Mn Deposit
    进路分层干式充填采矿法在鹤庆锰矿的应用
短句来源
    Quality Management of Mining Poor and Thin Ore in Taojiang Mn Deposit
    湖南省桃江锰矿贫薄矿床开采中的质量管理
短句来源
    THE GUDUTANG MN DEPOSIT,LIJIANG
    丽江古都塘锰矿
短句来源
    This paper presents the position, distribution, stratigraphy and geotechology of Chenkou Mn Deposit.
    简单介绍了城口锰矿所处大地构造位置、分布范围、地层分布、构造特征等 ;
短句来源
更多       
  锰矿
    THE CHARACTERISTICS OF THE MIDDLE ORDOVICIAN HIGH - QUALITY Mn DEPOSIT IN CENTRAL HUNAN
    湘中中奥陶世优质锰矿主要地质特征
短句来源
    Application of Dry Filling Mining Method Through Drifting-Slicing in Heqing Mn Deposit
    进路分层干式充填采矿法在鹤庆锰矿的应用
短句来源
    Quality Management of Mining Poor and Thin Ore in Taojiang Mn Deposit
    湖南省桃江锰矿贫薄矿床开采中的质量管理
短句来源
    THE GUDUTANG MN DEPOSIT,LIJIANG
    丽江古都塘锰矿
短句来源
    This paper presents the position, distribution, stratigraphy and geotechology of Chenkou Mn Deposit.
    简单介绍了城口锰矿所处大地构造位置、分布范围、地层分布、构造特征等 ;
短句来源
更多       
  锰矿床
    Origin and application of Gaoming Mn deposit
    高明锰矿床成因及应用
短句来源
    This paper deals with the geological features of the Xinrong Fe Mn deposit and its minerogenic mechanism.
    介绍了粤西新榕铁锰矿床地质特征,分析了成矿机制。
短句来源
    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
    Ag content becomes higher far away the rockmass,Ag content is high when Ag deposit intergrows with Pb Zn and Mn deposit,it shows the secondary enrichment phenomenon.
    银矿床与铅锌、锰矿床共生时银含量高,与铜钨钼矿床共生时银含量较低; 银矿床还存在次生富集的现象。
短句来源
  锰矿床
    Origin and application of Gaoming Mn deposit
    高明锰矿床成因及应用
短句来源
    This paper deals with the geological features of the Xinrong Fe Mn deposit and its minerogenic mechanism.
    介绍了粤西新榕铁锰矿床地质特征,分析了成矿机制。
短句来源
    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
    Ag content becomes higher far away the rockmass,Ag content is high when Ag deposit intergrows with Pb Zn and Mn deposit,it shows the secondary enrichment phenomenon.
    银矿床与铅锌、锰矿床共生时银含量高,与铜钨钼矿床共生时银含量较低; 银矿床还存在次生富集的现象。
短句来源
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  mn deposit
In this paper, we present high-resolution 40Ar/39Ar ages of Mn oxides from the Xinrong Mn deposit, western Guangdong, to place numerical constraints on the timing and duration of supergene Mn enrichment.
      
Pongkor (west Java, Indonesia): a Pliocene supergene-enriched epithermal Au-Ag-(Mn) deposit
      


This paper deals with the geological features of the Xinrong Fe Mn deposit and its minerogenic mechanism. This deposit isconsidered to be a palaeowethering type stratabound Fe Mn one occurring in a fracture zone and further oxidized and enriched inQuaternary period. This metallogenic model is widespread in the Xinge district of Luoding county.

介绍了粤西新榕铁锰矿床地质特征,分析了成矿机制。认为该矿为一个在断裂破碎带中就位的层控古风化型铁锰矿床,并经第四纪进一步氧化富集。这一成矿模式在罗定新榕地区具有普遍性。

The high-quality oxidized rich Mn deposits in Lancang Group are resulted from epigenetic enrichment of stratified or stratoid silicated Mn ore-beds. The genesis of themis controlled hy weather, morphology, hydrologic regime and characteristics of primary maneaniferous formation. The outward zone of volcanic chemical sediment of Proterozoic palaeo-volcanic vents in NS direction row and the distribution area of primary silicated Mn deposits resulted from Si-Mn sedimernt formation in regional...

The high-quality oxidized rich Mn deposits in Lancang Group are resulted from epigenetic enrichment of stratified or stratoid silicated Mn ore-beds. The genesis of themis controlled hy weather, morphology, hydrologic regime and characteristics of primary maneaniferous formation. The outward zone of volcanic chemical sediment of Proterozoic palaeo-volcanic vents in NS direction row and the distribution area of primary silicated Mn deposits resulted from Si-Mn sedimernt formation in regional metamorphism are the good prospect region for this kind of Mn deposits.

澜沧群中优质氧化富锰矿是层状,似层状硅酸锰矿层表生富集作用的结果,它的形成受到气候、地貌、水文条件及原生含锰建造特征的控制,南北向排列的元古代古火山口的火山化学沉积外圈,硅锰沉积建造因区域变质作用形成的原生硅酸锰矿分布区,具有寻找这类锰矿床的良好前景。

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。

 
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