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Oxygen and sulphur isotope compositions as indicators of the origin of Mesozoic and Cenozoic evaporites from Spain

✍ Scribed by Rosa Utrilla; Catherine Pierre; Federico Orti; Juan José Pueyo

Book ID
115815362
Publisher
Elsevier Science
Year
1992
Tongue
English
Weight
973 KB
Volume
102
Category
Article
ISSN
0009-2541

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Oxygen and hydrogen isotope studies of a number of granite suites and mineral separates from the New England Batholith indicate that 6018 can be used to discriminate the major granite protoliths. The granite suites previously subdivided on the basis of mineralogical and geochemical criteria into S-t