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D, O and C isotopes in podiform chromitites as fluid tracers for hydrothermal alteration processes of the Mayarí — Baracoa Ophiolitic Belt, eastern Cuba

✍ Scribed by J.A. Proenza; P. Alfonso; J.C. Melgarejo; F. Gervilla; J. Tritlla; A.E. Fallick


Book ID
117510150
Publisher
Elsevier Science
Year
2003
Tongue
English
Weight
657 KB
Volume
78-79
Category
Article
ISSN
0375-6742

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