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The aluminum-in-olivine thermometer for mantle peridotites — Experimental versus empirical calibration and potential applications
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文摘
Experimental calibration of the Al-in-olivine thermometer for garnet peridotites Applicable to olivines from garnet peridotites with an estimated accuracy of ~ ± 20 °C Not applicable to spinel-bearing peridotites, Al vs V-plot may be used to distinguish the facies of single olivine grains Applicability to garnet harzburgites (and lherzolites) makes Al-in-olivine thermometer an important tool in mantle studies

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