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.
矿物成分简单，原生金属矿物只有辉锑矿和黄铁矿，脉石矿物有石英、方解石及少量重晶石，它们均充填在岩石的缝洞中。
The mineral composition is simple, only with original metallic minerals antimonite and pyrite, gangue minerals quartz, calcite and a few barites, all in the fissure or hole of the rock.
结果表明，盆地周边岩石、煤系地层为富砷岩系，构成砷的原生物源。
The study indicates that the arsenic rich rocks around the basin and coal series strata are the original arsenic sources.
原生于岩石间阴影地带的松针落叶里。
Native to shaded areas, where it grows in pine-needles on boulders.
研究结果表明：各类榴辉岩相岩石的流体包裹体均程度不同地发生了次生变化。未发现原生包裹体。
The studied results show that different secondary changes occurred in fluid inclusions of various rocks and no primary inclusion has been found.
研究结果表明：各类榴辉岩相岩石的流体包裹体均程度不同地发生了次生变化。未发现原生包裹体。
The studied results show that different secondary changes occurred in fluid inclusions of various rocks and no primary inclusion has been found.
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