Origin of the adakite–high-Nb basalt association and its implications for postsubduction magmatism in Baja California, Mexico: Discussion

René C. Maury; Thierry Calmus; Carlos Pallares; Mathieu Benoit; Michel Grégoire; Alfredo Aguillón-Robles; Hervé Bellon; Marcel Bohn

doi:10.1130/B30043.1

Journal articles

Origin of the adakite–high-Nb basalt association and its implications for postsubduction magmatism in Baja California, Mexico: Discussion

René C. Maury ^{1, 2, *} Thierry Calmus ³ Carlos Pallares ³ Mathieu Benoit ⁴ Michel Grégoire ⁴ Alfredo Aguillón-Robles ⁵ Hervé Bellon ^{1, 2} Marcel Bohn ^{1, 2}

* Corresponding author

1 LDO - Domaines Océaniques

2 UEB - Université européenne de Bretagne - European University of Brittany

3 Estacion Regional del Noroeste

4 DTP - Dynamique terrestre et planétaire

5 Departamento de Geologia

Document type :

Journal articles

Domain :

Sciences of the Universe [physics] / Earth Sciences / Petrography

Sciences of the Universe [physics] / Earth Sciences / Geochemistry

Environmental Sciences / Global Changes

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https://hal-insu.archives-ouvertes.fr/insu-00420969
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Submitted on : Wednesday, September 30, 2009 - 11:45:38 AM
Last modification on : Tuesday, October 19, 2021 - 7:00:32 PM

Origin of the adakite–high-Nb basalt association and its implications for postsubduction magmatism in Baja California, Mexico: Discussion

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Origin of the adakite–high-Nb basalt association and its implications for postsubduction magmatism in Baja California, Mexico: Discussion

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