Evidence for xenolith–host basalt interaction from chemical patterns in Fe–Ti-oxides from mafic granulite xenoliths of the Bakony–Balaton Volcanic field (W-Hungary)-Reference-Cited by-同舟云学术

Evidence for xenolith–host basalt interaction from chemical patterns in Fe–Ti-oxides from mafic granulite xenoliths of the Bakony–Balaton Volcanic field (W-Hungary)

Published:2008-12-02 Issue:3-4 Volume:95 Page:219-234
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Miner Petrol

Author:

Dégi Júlia,Abart Rainer,Török Kálmán,Rhede Dieter,Petrishcheva Elena

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00710-008-0035-0.pdf

Reference48 articles.

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3. Ai Y (1994) A revision of the garnet-clinopyroxene Fe2+-Mg exchange geothermometer. Contrib Mineral Petrol 115:467–473

4. Andersen DJ, Lindsley DH (1988) Internally consistent solution models for Fe–Mg–Mn–Ti oxides: Fe–Ti oxides. Am Mineral 73:714–726

5. Aragon R, McCallister RH, Harrison HR (1984) Cation diffusion in titanomagnetites. Contrib Mineral Petrol 85:174–185

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