Alpine-type sensu strictu(ophiolitic) peridotites: Refractory residues from partial melting or igneous sediments? A contribution to the discussion of the paper: “The origin of ultramafic and ultrabasic rocks” by P.J. Wyllie
- 30 June 1969
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 7 (5-6) , 511-516
- https://doi.org/10.1016/0040-1951(69)90020-1
Abstract
No abstract availableKeywords
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