The origin of high δ18O zircons: marbles, megacrysts, and metamorphism
The origin of high δ18O zircons: marbles, megacrysts, and metamorphism
About this item
Full title
Author / Creator
Publisher
Berlin/Heidelberg: Springer-Verlag
Journal title
Language
English
Formats
Publication information
Publisher
Berlin/Heidelberg: Springer-Verlag
Subjects
More information
Scope and Contents
Contents
The oxygen isotope ratios (δ
18
O) of most igneous zircons range from 5 to 8‰, with 99% of published values from 1345 rocks below 10‰. Metamorphic zircons from quartzite, metapelite, metabasite, and eclogite record δ
18
O values from 5 to 17‰, with 99% below 15‰. However, zircons with anomalously high δ
18
O, up to 23‰, have been...
Alternative Titles
Full title
The origin of high δ18O zircons: marbles, megacrysts, and metamorphism
Authors, Artists and Contributors
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_crossref_primary_10_1007_s00410_011_0634_3
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_crossref_primary_10_1007_s00410_011_0634_3
Other Identifiers
ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-011-0634-3
