Conduit formation and crustal microxenolith entrainment in a basaltic fissure eruption: Observations from Thríhnúkagígur Volcano, Iceland
Thríhnúkagígur Volcano, Iceland, is a composite spatter cone and lava field characteristic of basaltic fissure eruptions. Lava drainback at the end of the eruption left ~60 m of evacuated conduit, and a 4 × 104 m3 cave formed by the erosion of unconsolidated tephra by the feeder dike. Field relation...
| Hlavní autoři: | , , , , |
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| Médium: | Článek |
| Jazyk: | English |
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Volcanica
2022-08-01
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| Edice: | Volcanica |
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| On-line přístup: | http://www.jvolcanica.org/ojs/index.php/volcanica/article/view/153 |