Experiments on silicate melt immiscibility in the system Fe2SiO4–KAlSi3O8–SiO2–CaO–MgO–TiO2–P2O5 and implications for natural magmas-Reference-Cited by-同舟云学术

Experiments on silicate melt immiscibility in the system Fe2SiO4–KAlSi3O8–SiO2–CaO–MgO–TiO2–P2O5 and implications for natural magmas

Published:2006-07-11 Issue:3 Volume:152 Page:257-274
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Bogaerts M.,Schmidt M. W.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-006-0111-6.pdf

Reference63 articles.

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2. Bender JF, Hanson GN, Bence AE (1982) The Cortland complex: evidence for large-scale liquid immiscibility involving granodiorite and diorite magmas. Earth Planet Sci Lett 58:330–344

3. Biggar GM (1970) Molybdenum as a container for melts containing iron oxide. Am Ceram Soc Bull 49:286–288

4. Biggar GM (1979) Immiscibility in tholeiites. Mineral Mag 43:543–544

5. Bigioggero B, Colombo A, Del Moro A, Gregnanin A, Macera P, Tunesi A (1994) The Oligocene Valle del Cervo pluton: an example of shoshonitic magmatism in the western Italian Alps. Mem Sci Geol 46:409–421

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