俯冲带和地球系统演化过程中的动力学及物质循环。
And dynamics and mass circulation in subduction zones and Earth system evolution.
毗邻的沉积盆地与造山带是大陆构造的基本单元和形成于统一地球动力学系统中的一对孪生体。
Sedimentary basin and adjacent orogenic belt are two basic tectonic units of continent and twins developed in a geodynamic system.
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.
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