Home > Articles > The gradual shift from forearc basalt-like to boninite-like magmatism during intra-oceanic subduction-initiation recorded by ophiolitic chromite deposits from Cuba > BibTeX |
@article{Domínguez-Carretero:152189, author = "Domínguez-Carretero, D. and Proenza, J. A. and Pujol-Solà, N. and Gervilla, F. and Villanova-de-Benavent, C. and Colás, V. and Núñez-Cambra, K. and Piñero-Pérez, E. and Garcia-Casco, A.", title = "{The gradual shift from forearc basalt-like to boninite-like magmatism during intra-oceanic subduction-initiation recorded by ophiolitic chromite deposits from Cuba}", year = "2025", }