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Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting, mantle and crustal, sources? A review

✍ Scribed by Bernard Bonin


Book ID
113774281
Publisher
Elsevier Science
Year
2004
Tongue
English
Weight
754 KB
Volume
78
Category
Article
ISSN
0024-4937

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