Morphology and dynamics of inflated subaqueous basaltic lava flows
Abstract During eruptions onto low slopes, basaltic Pahoehoe lava can form thin lobes that progressively coalesce and inflate to many times their original thickness, due to a steady injection of magma beneath brittle and viscoelastic layers of cooled lava that develop sufficient strength to retain t...
Gorde:
| Egile Nagusiak: | , , , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Wiley
2014-06-01
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| Saila: | Geochemistry, Geophysics, Geosystems |
| Gaiak: | |
| Sarrera elektronikoa: | https://doi.org/10.1002/2014GC005274 |
| Etiketak: |
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