Phosphorus hydrides are formed in a H-rich, reduction environment.
磷氢化物形成于还原性的富氢环境。
The relative enriched area of magnetic minerals may represent the favorable reduction environment of uranium deposition.
磁性矿物的相对富集区可能代表着铀沉积的理想还原环境。
It is suggested that the cauterized loss can indicate the oxidation-reduction environment or the varied depth and the salinity of water.
烧失率异常可指示氧化—还原环境或水体深浅变化以及判别水体的盐度。
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