Peridotite xenoliths from Porcupine Dome, Montana, USA: depleted subcontinental lithosphere samples in an olivine-phlogopite-carbonate magma
DOI:
https://doi.org/10.29173/ikc2725Downloads
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Published
1998-04-17
How to Cite
Hearn, B. (1998). Peridotite xenoliths from Porcupine Dome, Montana, USA: depleted subcontinental lithosphere samples in an olivine-phlogopite-carbonate magma. International Kimberlite Conference: Extended Abstracts, 7(1), 328–330. https://doi.org/10.29173/ikc2725
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Extended Abstracts