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DOI10.1038/s41561-022-00960-z
Eruption at basaltic calderas forecast by magma flow rate
Galetto F.;   Acocella V.;   Hooper A.;   Bagnardi M.
发表日期2022
ISSN1752-0894
起始页码580
结束页码584
卷号15期号:7
英文摘要Forecasting eruption is the ultimate challenge for volcanology. While there has been some success in forecasting eruptions hours to days beforehand, reliable forecasting on a longer timescale remains elusive. Here we show that magma inflow rate, derived from surface deformation, is an indicator of the probability of magma transfer towards the surface, and thus eruption, for basaltic calderas. Inflow rates ≥0.1 km3 yr−1 promote magma propagation and eruption within 1 year in all assessed case studies, whereas rates <0.01 km3 yr−1 do not lead to magma propagation in 89% of cases. We explain these behaviours with a viscoelastic model where the relaxation timescale controls whether the critical overpressure for dyke propagation is reached or not. Therefore, while surface deformation alone is a weak precursor of eruption, estimating magma inflow rates at basaltic calderas provides improved forecasting, substantially enhancing our capacity of forecasting weeks to months ahead of a possible eruption. © 2022, The Author(s), under exclusive licence to Springer Nature Limited.
语种英语
scopus关键词basalt; deformation; magma; model; timescale
来源期刊Nature Geoscience
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/262173
作者单位Dipartimento di Scienze, Università degli Studi di Roma Tre, Rome, Italy
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Galetto F.; Acocella V.; Hooper A.; Bagnardi M.. Eruption at basaltic calderas forecast by magma flow rate[J],2022,15(7).
APA Galetto F.; Acocella V.; Hooper A.; Bagnardi M..(2022).Eruption at basaltic calderas forecast by magma flow rate.Nature Geoscience,15(7).
MLA Galetto F.; Acocella V.; Hooper A.; Bagnardi M.."Eruption at basaltic calderas forecast by magma flow rate".Nature Geoscience 15.7(2022).
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