The ultramafic-granulitic associations: an indication of paleo-moho discontinuities

  • D. Vielzeuf
  • J Kornprobst
Published
1982-09-01
How to Cite
VielzeufD., & KornprobstJ. (1982). The ultramafic-granulitic associations: an indication of paleo-moho discontinuities. International Kimberlite Conference: Extended Abstracts, 3, 241-241. https://doi.org/10.29173/ikc2355
Section
Extended Abstracts: G_Geodynamics and magma genesis