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

  • B.C. Hearn
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