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Heavy oxygen isotope of the olivine from the ultramafic rocks as indicator of their genesis

✍ Scribed by Pinus, G. V.

Book ID
119717116
Publisher
American Geophysical Union
Year
1971
Tongue
English
Weight
251 KB
Volume
76
Category
Article
ISSN
0148-0227

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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