原生水的化学性质随岩石的历史而有成分上的变化。
The chemistry of connate water can change in composition throughout the history of the rock.
以卤水、盐类矿物、原生矿物、细菌活动以及岩石分带为特征阐明了盐湖沉积中的变质和变形现象。
The brine, salt minerals, primary minerals, bacteria activity and rock zonation were characterized in discussing the metamorphic and deformation phenomenon in the salt lake deposition.
同时乌伦古河组W-1旋回原生灰色岩石分布较为局限，大致呈EW向带状展布，并向东部延伸至杜热一带。
The distribution of W-1 cycle primary gray rock trending in EW direction was localized and its east end extends to Dure which area is one of the promising propective area.
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