Synthesis of monticellite–forsterite and merwinite–forsterite symplectites in the CaO–MgO–SiO2 model system: influence of temperature and water content on microstructure evolution-Reference-Cited by-同舟云学术

Synthesis of monticellite–forsterite and merwinite–forsterite symplectites in the CaO–MgO–SiO2 model system: influence of temperature and water content on microstructure evolution

Published:2017-12-21 Issue:1 Volume:173 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Remmert P.,Heinrich W.,Wunder B.,Morales L.,Wirth R.,Rhede D.,Abart R.^ORCID

Funder

Deutsche Forschungsgemeinschaft

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/article/10.1007/s00410-017-1429-y/fulltext.html

Reference43 articles.

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3. Abart R, Heuser D, Habler G (2014) Mechanisms of myrmekite formation: case study form the Weinsberg granite, Maldanubian zone, Upper Austria. Contrib Miner Pet 168:2–14

4. Altherr R, Kalt A (1996) Metamorphic evolution of ultrahigh-pressure garnet peridotites from the Variscan Vosges Mts. (France). Chem Geol 134(1–3):27–47

5. Ashworth J, Chambers A (2000) Symplectic reaction in olivine and the controls of intergrowth spacing in symplectites. J Pet 41:285–304

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