An experimental study of dissolution and precipitation of forsterite in a thermal gradient: implications for cellular growth of olivine phenocrysts in basalt and melt inclusion formation-Reference-Cited by-同舟云学术

An experimental study of dissolution and precipitation of forsterite in a thermal gradient: implications for cellular growth of olivine phenocrysts in basalt and melt inclusion formation

Published:2019-10-29 Issue:11 Volume:174 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Laumonier Mickael^ORCID,Laporte Didier,Faure François,Provost Ariel,Schiano Pierre,Ito Kazuhiko

Funder

Agence Nationale de la Recherche

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-019-1627-x.pdf

Reference73 articles.

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2. Anderson AT Jr (1991) Hourglass inclusions: theory and application to the Bishop Rhyolitic Tuff. Am Mineral States 76:530–547

3. Andersson UB, Eklund O (1994) Cellular plagioclase intergrowths as a result of crystal-magma mixing in the Proterozoic Aland rapakivi batholith, SW Finland. Contrib Mineral Petrol 117:124–136. https://doi.org/10.1007/BF00286837

4. Armienti P, Innocenti F, Pareschi MT et al (1991) Crystal population density in not stationary volcanic systems: estimate of olivine growth rate in basalts of Lanzarote (Canary Islands). Mineral Petrol 44:181–196

5. Armienti P, Pareschi MT, Innocenti F, Pompilio M (1994) Effects of magma storage and ascent on the kinetics of crystal growth. Contrib Mineral Petrol 115:402–414

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