在金属矿区如何勘探矿藏,科学家正在设计一种新的方法。这个方法是基于这样一个事实:这些区域的岩石样品合有不同原子重量的氧元素。研究结果证明,氧的这些不同的同位素的存在,和25,000万年前热液体对这些矿石加热和渗透的程度有直接的关系。这种来自地心的热,引起地球表面岩石的化学变化,这可以用科学分析探查出来。 How to explore mineral deposits in metal mines, scientists are designing a new method. This method is based on the fact that the rock samples in these areas have different atomic weights of oxygen. The results of the study show that the existence of these different isotopes of oxygen is directly related to the extent to which hot liquids heat and infiltrate these ores 250 million years ago. This heat from the earth’s core causes chemical changes in the rock on Earth’s surface, which can be explored with scientific analysis.