地壳中能够料想到的最重要的放热化学反应是硫化物的化学转变。
The most important exothermal reactions in the crust can be expected from the chemical transformations of sulfides.
举例来说，如果能由一个放热化学反应所吸收，在一个货柜内的水，这一变化在水温提供了一个衡量的数额热量补充。
For example, if the energy from an exothermic chemical reaction is absorbed in a container of water, the change in temperature of the water provides a measure of the amount of heat added.
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