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。

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.

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通过分析发现，影响该区崩滑形成的因素有区域地质构造、地层岩性、地形地貌及气象水文条件。

The influence factors of collapse-slide are regional tectonic, stratum lithologic, geomorphic, meteorological and hydrographic characteristics of Changbai Mountain.

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花岗岩是湖南省最为发育的一类岩浆岩，由于花岗岩岩性及构造条件的不同，造就了独特的地质地貌景观。

Granite is the most common magmatic rock in Hunan Province. Many particular granitic scenic landscapes are formed for the different lithology or structure.

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