Terceira lavas isotopic signatures and multi-scale mantle heterogeneity at the Azores Archipelago
Terceira Island mafic lavas (< 30 ka), erupted from two main active volcanic systems, were analysed in this study: Fissural zone (F), interpreted as the sub aerial expression of the Terceira Rift, and Sta Bárbara central volcano (SB), which dominates the western topography of the island. These ma...
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| Other Authors: | , , |
| Format: | article |
| Language: | eng |
| Published: |
2011
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10174/2443 |
| Country: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/2443 |