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30 Ιουλ 2019 · Understanding the mechanisms of shallow magma storage (less than ~10-km depth) is crucial to defining volcanic plumbing systems and their effect on volcano unrest. Sills are common structures to emplace shallow magma.
1 Ιαν 2018 · Lateral magma flow through sill complexes and networks can reach several hundred kilometres. Sills represent intermediate feeder structures for volcanic eruptions, and therefore better understanding of sill emplacement and evolution is essential for assessing volcanic hazards.
12 Νοε 2023 · Volcanoes can take on different shapes and sizes, ranging from gentle, shield-like structures to steep, cone-shaped mountains. Volcanic eruptions can be explosive or effusive, with varying levels of intensity. They release not only molten rock but also ash, gases, and other volcanic materials.
12 Μαΐ 2021 · At Ceduna, shield volcanoes usually overlie the sills tips, suggesting that the eruption phases correspond to the incremental emplacement of magma pulses within the sills. Volcanogenic hydrothermal vents are also associated with the sill tips, promoted by fractures within the host rock.
Image created by Volcanic Basin Petroleum Research (VBPR), Oslo, Norway (e.g. Planke et al. 2015); image relabelled. from publication: The Mechanics of Sill Propagation and Associated Venting...
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