论述水-岩作用过程氧氢同位素地球化学行为特征。
The geochemical behaviors of oxygen and hydrogen isotopes in water-rock interaction are discussed.
广汉亚粘土层的元素地球化学行为表明它是在变干趋势的环境中形成的。
The element geochemistry behavior of Guanghan claypan indicated that it has the dry change tendency in the environment.
相似的地球化学性质和地球化学行为，是导致分散元素共生的基本原因。
Similar geochemical properties and behaviors are primary reason to form coexistence of some disperse elements.
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