Al-in-olivine thermometry evidence for the mantle plume origin of the Emeishan large igneous province
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文摘
We estimate the Al-in-olivine temperatures for the picrites in the ELIP. The maximum crystallization temperature of the ELIP (1440 °C) is ~ 250 °C higher than the average temperature of MORB. The results provide compelling evidence for the existence of thermal mantle plumes in the ELIP.

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