High-Ti amphibole as a petrogenetic indicator of magma chemistry: evidence for mildly alkalic-hybrid melts during evolution of Variscan basic–ultrabasic magmatism of Central Iberia-Reference-Cited by-同舟云学术

High-Ti amphibole as a petrogenetic indicator of magma chemistry: evidence for mildly alkalic-hybrid melts during evolution of Variscan basic–ultrabasic magmatism of Central Iberia

Published:2009-02-08 Issue:1 Volume:158 Page:69-98
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Molina José F.,Scarrow Jane H.,Montero Pilar G.,Bea Fernando

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-008-0371-4.pdf

Reference165 articles.

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2. Adam J, Green TH, Sie SH (1993) Proton microprobe determined partitioning of Rb, Sr, Ba, Y, Zr, Nb and Ta between experimentally produced amphiboles and silicate melts with variable F content. Chem Geol 109:29–49. doi: 10.1016/0009-2541(93)90060-V

3. Andersen DJ, Lindsley DH, Davidson PM (1993) QUILF-a Pascal program to assess equilibria among Fe–Mg–Ti oxides, pyroxenes, olivine and quartz. Comput Geosci 19:1333–1350. doi: 10.1016/0098-3004(93)90033-2

4. Arai S (1992) Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry. Mineral Mag (Lond) 56:173–184. doi: 10.1180/minmag.1992.056.383.04

5. Azor A, González-Lodeiro F, Simancas F (1994) Tectonic evolution of the boundary between the Central Iberian and Ossa-Morena zones (Variscan belt, southwest Spain). Tectonics 13:45–61. doi: 10.1029/93TC02724

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