• 本文提出矿床古风化成因认识

    In this paper, a new recognition is presented that the genesis of this ore deposit is anciently weathered eluvial deposit.

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  • 合肥地区膨胀形成于第四纪上更新世Q_3及其以前江淮冲、洪积成因类型

    The swelling soil in Hefei zone was formed at the Q3 epipleistocene of the 4th subage or before. It belongs to the type of Huaihe alluviation and diluvion.

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  • 成矿关系密切的岩石成因

    The ore forming rock series should be turbidite origin.

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  • 根据成因蓝宝石砂矿分为砂矿、洪砂矿层残坡砂矿层;洪砂矿层蓝宝石最富。

    According to I ts origin, sapphire sand strata are divided into sand wash stratum, pluvial stratum and relict drifted sand stratum, while sapphire concentrated well in drifted sand stratum.

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  • 黔东北地区氧化锰矿床系风化矿床,按其成因进一步分为矿床矿床

    Oxide manganese deposits in east-northern Guizhou are of exotic weathering deposits, further may be subdivided into two kinds of the eluvial ore deposit and the leaching-accretion deposit by genesis.

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  • 矿床成因风化型,受地层岩性控制

    Genetically, it is an eluvial deposit produced by weathering, controlled by the stratigraphy and lithology.

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  • 矿床成因第四纪

    The origin of the deposit belongs to Quarternary eluvial placer type.

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  • 洞庭湖漫滩阶地冲湖淤泥上,分布着一些次级牛轭季节性洪道成因的极软淤物。

    There are some softer accumulation horizon in the ox-bow lake and season river on the huge mucky soil of alluvial and lacustrine deposits in accumulation terrace around Dongting lake.

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  • 矿床成因类型渗流卤水一表生成因粘土型金矿床,工业类型为红土型金矿床。

    The deposit belongs to vadose hot brine-supergene genetic eluvial clay-type gold deposit and to laterite-type gold-deposit in terms of industry.

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  • 矿床成因类型渗流卤水一表生成因粘土型金矿床,工业类型为红土型金矿床。

    The deposit belongs to vadose hot brine-supergene genetic eluvial clay-type gold deposit and to laterite-type gold-deposit in terms of industry.

    youdao

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