Peridotite xenoliths from Porcupine Dome, Montana, USA: depleted subcontinental lithosphere samples in an olivine-phlogopite-carbonate magma

Authors

  • B.C. Hearn

DOI:

https://doi.org/10.29173/ikc2725

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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