Hydrous melts weaken the mantle, crystallization of pargasite and phlogopite does not: Insights from a petrostructural study of the Finero peridotites, southern Alps

Author:

Tommasi AndréaORCID,Langone Antonio,Padrón-Navarta José Alberto,Zanetti Alberto,Vauchez Alain

Funder

CNRS

MIUR

CNR

ANR

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference72 articles.

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2. A crustal-scale view at rift localization along the fossil Adriatic margin of the Alpine Tethys preserved in NW Italy;Beltrando;Tectonics,2015

3. Fingerprinting the water site in mantle olivine;Berry;Geology,2005

4. Quantitative and analysis of trace OH in garnet and pyroxenes;Bell;Am. Mineral.,1995

5. Hydroxide in olivine: a quantitative determination of the absolute amount and calibration of the IR spectrum;Bell;J. Geophys. Res., Solid Earth,2003

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