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Embryos of TTGs in Gore Mountain garnet megacrysts from water-fluxed melting of the lower crust

Ferrero, S., Wannhoff, I., Laurent, O., Yakymchuk, C., Darling, R., Wunder, B., Borghini, A., O'Brien, P.J.·2021·Earth and Planetary Science Letters
DOI 10.1016/j.epsl.2021.117058
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  • Partial melting of mafic rocks is invoked for the origin of the Gore Mountain amphibolite in the inner part of the Adirondack domal structure.

    “Partial melting of mafic rocks is also invoked for the origin of the Gore Mountain amphibolite in the inner part of this structure, (Ferrero et al. 2021; see subsection 3.1.1.2) but the heat source (or D r a f t tectonic setting) for melting of this refractory crust is not addressed.”

    From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Ferrero et al. 2021

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Research works printed but not linked: 45

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Metadata

Authors
Ferrero, S., Wannhoff, I., Laurent, O., Yakymchuk, C., Darling, R., Wunder, B., Borghini, A., & O'Brien, P. J.
ORCID
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2021-09
Volume
569
Pages
117058
ISSN
0012-821X
DOI
10.1016/j.epsl.2021.117058
Cited by
29
References
1
Language
en
Licence
Funders
  • Bundesministerium für Bildung und Forschung
  • Deutsche Forschungsgemeinschaft (FE 1527/2-2)

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