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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

✍ Scribed by T.P. Thayer


Book ID
118997093
Publisher
Elsevier Science
Year
1969
Tongue
English
Weight
465 KB
Volume
7
Category
Article
ISSN
0040-1951

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