Thermodynamics Of Earth Systems, October 2010, Vol. 6, No. 5
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During the past decades, thermodynamics has become an essential tool for understanding fundamental processes that have determined the structure and evolution of our planet. From the atmosphere to the ocean and sediments, from metamorphic terranes to magmatic provinces, the lower mantle, and the core, this issue of Elements illustrates how a better understanding of the manner in which free energy depends on temperature, pressure, and chemical composition allows the Earth’s activity to be better deciphered.
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