氟是骨骼和牙齿的矿化的一个重要组成部分。
Fluoride is an important element in the mineralization of bone and teeth.
暴露地表矿床、隐伏矿床、分散矿化的异常指标各不相同。
The anomalous indicatrices of surface mine, hidden deposit and dispersed mineralization are different too.
同时放牧使氮的矿化速率明显提高。
Meanwhile, grazing made rate of nitrogen mineralization increase obviously.
同时,矿化过程还受细菌生长环境的影响。
Meanwhile the mineralization process was also affected by the environment of bacteria growth.
矿化类型主要是少硫化物的蚀变岩型。
目前已探明,该区深部存在规模较大的矿化体。
There is possibly some bigger mineralizing bodies in the deep part of the deposit.
氮的净矿化速率与林型关系很大。
There is a distinct relationship between net Nitrogen mineralization rate and forest type.
通过综合研究,认为该地区金矿化与韧性剪切构造带关系密切,且具有较好的找矿前景。
Through comprehensive study, it is regarded that it has good ore-probing future in this area.
探讨矿化物质的生长方式和形成机制;
The discussion mineralization material's growth way and forms the mechanism;
探讨矿化物质的生长方式和形成机制;
The discussion mineralization material's growth way and forms the mechanism;
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