Geochemistry of stable oxygen and hydrogen isotopes in minerals and corundum-bearing rocks in northern Karelia as an indicator of their unusual genesis-Reference-Cited by-同舟云学术

Geochemistry of stable oxygen and hydrogen isotopes in minerals and corundum-bearing rocks in northern Karelia as an indicator of their unusual genesis

Published:2014-08-31 Issue:9 Volume:52 Page:773-782
ISSN:0016-7029
Container-title:Geochemistry International
language:en
Short-container-title:Geochem. Int.

Author:

Vysotskiy S. V.,Ignat’ev A. V.,Levitskii V. I.,Nechaev V. P.,Velivetskaya T. A.,Yakovenko V. V.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1134/S0016702914090109.pdf

Reference53 articles.

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3. I. N. Bindeman, C. K. Brooks, A. R. McBirney, and H. P. Taylor, “The low-δ18O late-stage ferrodiorite magmas in the Skaergaard Intrusion: result of liquid immiscibility, thermal metamorphism, or meteoric water incorporation into magma?,” J. Geol. 116, 571–586 (2008).

4. E. C. Pope, D. K. Bird, S. Arnorsson, Th. Fridriksson, W. A. Elders, and G. O. Fridleifsson, “Isotopic constraints on ice age fluids in active geothermal systems: Reykjanes, Iceland,” Geochim. Cosmochim. Acta 73, 4468–4488 (2009).

5. P. Blattner, G. W. Grindley, and C. J. Adams, “Low-δ18O terranes tracking Mesozoic Polar climates in the South Pacific,” Geochim. Cosmochim. Acta 61(3), 569–576 (1997).

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