Surface uplift in the Central Andes driven by growth of the Altiplano Puna Magma Body
The Altiplano-Puna magma body is located in the world's second highest plateau, the Altiplano-Puna, but the influence of melt production in the surface uplift of the Central Andes is unclear. Perkinset al. link surface topography and isotactic modelling to constrain the melt production in the m...
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| Main Authors: | , , , , , |
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| Format: | article |
| Language: | EN |
| Published: |
Nature Portfolio
2016
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| Subjects: | |
| Online Access: | https://doaj.org/article/e6b757f7388a4ae9a5f8a29fffe75a91 |
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| Summary: | The Altiplano-Puna magma body is located in the world's second highest plateau, the Altiplano-Puna, but the influence of melt production in the surface uplift of the Central Andes is unclear. Perkinset al. link surface topography and isotactic modelling to constrain the melt production in the magma body. |
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