The Low-δ<sup>18</sup>O Late-Stage Ferrodiorite Magmas in the Skaergaard Intrusion: Result of Liquid Immiscibility, Thermal Metamorphism, or Meteoric Water Incorporation into Magma?-Reference-Cited by-同舟云学术

The Low-δ¹⁸O Late-Stage Ferrodiorite Magmas in the Skaergaard Intrusion: Result of Liquid Immiscibility, Thermal Metamorphism, or Meteoric Water Incorporation into Magma?

Published:2008-11 Issue:6 Volume:116 Page:571-586
ISSN:0022-1376
Container-title:The Journal of Geology
language:en
Short-container-title:The Journal of Geology

Author:

Bindeman I. N.,Brooks C. K.,McBirney A. R.,Taylor H. P.

Publisher

University of Chicago Press

Link

http://www.journals.uchicago.edu/doi/pdf/10.1086/591992

Reference53 articles.

1. Origin and Evolution of Silicic Magmatism at Yellowstone Based on Ion Microprobe Analysis of Isotopically Zoned Zircons

2. Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: Evidence for magmatic digestion and erosion of Pleistocene hyaloclastites

3. Volcanic arc of Kamchatka: a province with high-δ18O magma sources and large-scale 18O/16O depletion of the upper crust

4. Time constraints on the origin of large volume basalts derived from O-isotope and trace element mineral zoning and U-series disequilibria in the Laki and Grímsvötn volcanic system

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