dc.contributor.author |
Le Corvec, Nicolas Le |
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dc.contributor.author |
McGovern, Patrick J. (Geophysicist) |
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dc.contributor.author |
https://orcid.org/0000-0001-9647-3096 |
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dc.coverage.spatial |
Earth (Planet) |
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dc.date.accessioned |
2020-04-07T19:59:07Z |
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dc.date.available |
2020-04-07T19:59:07Z |
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dc.date.issued |
2018-09-07 |
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dc.identifier.citation |
Le Corvec N and McGovern PJ (2018) The Effect of Ocean Loading on the Growth of Basaltic Ocean Island Volcanoes and Their Magmatic Plumbing System. Front. Earth Sci. 6:119. doi: 10.3389/feart.2018.00119 |
en |
dc.identifier.other |
https://doi.org/10.3389/feart.2018.00119 |
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dc.identifier.uri |
https://hdl.handle.net/20.500.11753/1487 |
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dc.description.abstract |
Basaltic shield volcanoes most commonly form as intraplate volcanic ocean islands that arise from the ocean floor and continue to grow above the sea water level to form gigantic volcanic edifices. The volcanic edifice evolution and the internal stress distribution may be influenced by the water load of the surrounding ocean. We therefore investigate how the presence of an ocean affects the internal stress of a volcanic edifice and thus magma propagation by means of axisymmetric elastic models of a volcanic edifice overlying an elastic lithosphere. |
en |
dc.description.statementofresponsibility |
Nicolas Le Corvec and Patrick J. McGovern |
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dc.format.extent |
15 pages |
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dc.format.mimetype |
application/pdf |
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dc.language.iso |
en |
en |
dc.relation.ispartofseries |
LPI contribution ; no. 2111 |
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dc.subject |
Volcanoes |
en |
dc.title |
The Effect of Ocean Loading on the Growth of Basaltic Ocean Island Volcanoes and Their Magmatic Plumbing System |
en |
dc.type |
Article |
en |
dc.rights.license |
© 2018 Le Corvec and McGovern. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
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