Crustal structure of the eastern Acambay Graben, central Mexico, from integrated geophysical data
The Acambay graben is a ∼70 km long E–W seismically active structure located within the Trans-Mexican Volcanic Belt (TMVB). Quaternary volcanism has contributed to shaping the graben morphology and reported hydrothermal activity suggests the existence of potential geothermal reservoirs. Our work ai...
Furkejuvvon:
| Váldodahkkit: | , , , , , , |
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| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Universidad Nacional Autónoma de México
2018-11-01
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| Ráidu: | Revista Mexicana de Ciencias Geológicas |
| Fáttát: | |
| Liŋkkat: | https://rmcg.unam.mx/index.php/rmcg/article/view/864 |
| Fáddágilkorat: |
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