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The oxygen isotopic composition as an indicator of the genesis of “Basaltic” corundum

✍ Scribed by S. V. Vysotsky; V. V. Yakovenko; A. V. Ignat’ev; A. A. Karabtsov

Book ID
111470815
Publisher
Pleiades Publishing
Year
2009
Tongue
English
Weight
209 KB
Volume
3
Category
Article
ISSN
1819-7140

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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