它是构造地质学和地球物理学互相渗透、互相促进的一门很有前景的新兴边缘学科。
This is a newly developed marginal discipline of research, resulting from the impact and infiltration between tectonics and geophysics.
因为这些地区不仅沐浴在地球已进入的恒星门的光子能之中，而且还处于来自地心和其中极光的能量流之中。
Such regions are bathed not only in photon energy from the star gates earth has entered already but also that which flows from the center of the earth and aurora therein.
同位素地质年代学是测量年龄，利率，和历史或行星的地质资料的一门科学，运用这些见解的过程和现象可以了解地球与行星科学系。
Geochronology is the science of measuring ages, rates, and histories of geologic or planetary materials, and using these insights to understand processes and phenomena in earth and planetary science.
同位素地质年代学是测量年龄，利率，和历史或行星的地质资料的一门科学，运用这些见解的过程和现象可以了解地球与行星科学系。
Geochronology is the science of measuring ages, rates, and histories of geologic or planetary materials, and using these insights to understand processes and phenomena in earth and planetary science.
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