生烃动力学、同位素动力学常用于烃源岩评价、油气源对比研究中。
Hydrocarbon generation kinetics and isotopic kinetics have been normally used in the evaluation of source rocks and correlation of oil, gas and their supposed source rocks.
本文研究了激光同位素中离子取出的动力学过程。
The dynamic process for ion extraction in laser isotope separation is studied.
碳同位素分馏动力学模型在不同盆地会存在差异,不仅取决于气源条件,还与聚集历史、沉积-构造史有关。
The kinetic model of carbon isotope fractionation may have difference in the different basin, which lies on gas source condition, accumulation history and sedimentary-tectonics history.
这些初步成果说明同位素填图与化学地球动力学在造山带研究中是具有重要前景的技术途径。
Theseachievements indicate that isotopic mapping and chemical geodynamics are significant and perspective approaches to researches on orogenic belts.
矿物水体系氢同位素平衡分馏系数和动力分馏系数是同位素地球化学研究中的重要参数。
The hydrogen isotope equilibrium fractionation factors and kinetic fractionation parameters are the important basic data for the study of isotope geochemistry.
对流体-岩石相互作用过程中氧同位素变化的地球化学动力学进行了系统评述,其原理和模型也可扩展到对其他元素的研究。
This article reviews geochemical kinetics of oxygen isotope exchange during fluid rock interactions, whose principles and models can also be extended to studies on other elements.
文中介绍的数学模型考虑了混合云中液、固相共存时以及冰面过饱和环境下稳定同位素的动力分馏效应。
The introduced mathematical model takes into account the action of the kinetic fractionation effect in super saturation environment at ice surface as liquid and solid phases coexist in mixed cloud.
介绍的数学模型考虑了混合云中液、固态共存时以及冰面过饱和环境下稳定同位素的动力分馏效应。
The introduced mathematical model takes into account the role of the kinetic fractionation effect in a supersaturation environment at the ice surface as liquid and solid phases coexist in mixed cloud.
介绍的数学模型考虑了混合云中液、固态共存时以及冰面过饱和环境下稳定同位素的动力分馏效应。
The introduced mathematical model takes into account the role of the kinetic fractionation effect in a supersaturation environment at the ice surface as liquid and solid phases coexist in mixed cloud.
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