Abstract
Joule-Thomson coefficients of crystals indicate that temperatures may increase during irreversible adiabatic release of pressure. Isenthalpic decompression provides a mechanism for “self-heating” in igneous and metamorphic processes.
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WALDBAUM, D. Temperature Changes associated with Adiabatic Decompression in Geological Processes. Nature 232, 545–547 (1971). https://doi.org/10.1038/232545a0
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DOI: https://doi.org/10.1038/232545a0
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