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Petrogenesis of a Late-Variscan Rhyodacite at the Ossa Morena-Central Iberian Zones Boundary, Iberian Massif, Central Portugal: Evidence for the Involvement of Lithospheric Mantle and Meta-Igneous Lower Crust

AuthID
P-00M-5CR

Author(s)

Henriques, SBA

Neiva, AMR

Dunning, GR

Tipo de Documento

Article

Year published

2016

Publicado

in CHEMIE DER ERDE-GEOCHEMISTRY, ISSN: 0009-2819

Volume: 76, Número: 3, Páginas: 429-439 (11)

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Wos^®

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Google Scholar^®

Publication Identifiers

DOI: 10.1016/j.chemer.2016.06.003

Wos: WOS:000385320400008

Source Identifiers

ISSN: 0009-2819

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Petrogenesis of a Late-Variscan Rhyodacite at the Ossa Morena-Central Iberian Zones Boundary, Iberian Massif, Central Portugal: Evidence for the Involvement of Lithospheric Mantle and Meta-Igneous Lower Crust

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Petrogenesis of a Late-Variscan Rhyodacite at the Ossa Morena-Central Iberian Zones Boundary, Iberian Massif, Central Portugal: Evidence for the Involvement of Lithospheric Mantle and Meta-Igneous Lower Crust

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