2020
DOI: 10.1038/s41467-020-17759-4
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Deep long period volcanic earthquakes generated by degassing of volatile-rich basaltic magmas

Abstract: Deep long-period (DLP) earthquakes observed beneath active volcanoes are sometimes considered as precursors to eruptions. Their origin remains, however, unclear. Here, we present a possible DLP generating mechanism related to the rapid growth of gas bubbles in response to the slow decompression of over-saturated magma. For certain values of the gas and bubble content, the elastic deformation of surrounding rocks forced by the expanding bubbly magma can be fast enough to generate seismic waves. We show that amp… Show more

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Cited by 40 publications
(26 citation statements)
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“…Deep long-period earthquakes (DLPs) associated with volcanoes have been observed in the mid-lower crust or mantle (Aso and Tsai 2014;Melnik et al 2020;Wech et al 2020). Although their origin is enigmatic, some studies have linked DLPs to an exsolved MVP.…”
Section: Seismicity and Strain Signals Related To The Migration Of Vo...mentioning
confidence: 99%
See 1 more Smart Citation
“…Deep long-period earthquakes (DLPs) associated with volcanoes have been observed in the mid-lower crust or mantle (Aso and Tsai 2014;Melnik et al 2020;Wech et al 2020). Although their origin is enigmatic, some studies have linked DLPs to an exsolved MVP.…”
Section: Seismicity and Strain Signals Related To The Migration Of Vo...mentioning
confidence: 99%
“…These events are not linked to eruptions but have been ascribed to the second boiling of deep (near-Moho) magma intrusions. Other interpretations of DLPs include thermal stresses set up by cooling magmas (Aso and Tsai 2014) and rapid changes of magmatic pressure in the lower crust caused by rapid nucleation and growth of gas bubbles in response to the slow upwelling of volatile-saturated magma (Melnik et al 2020). The latter explanation for the Klyuchevskoy volcanic group relates to primary melts that may contain ≤ 4 wt% H 2 O and 0.6 wt% CO 2 , which would cause volatile saturation at 800 MPa (~ 30 km).…”
Section: Seismicity and Strain Signals Related To The Migration Of Vo...mentioning
confidence: 99%
“…S-wave dominated signals can arise from volumetric sources with non-spherical geometries (e.g. Melnik et al, 2020) or from singleforce sources associated with fast local pressure variations (Shapiro et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…One should finally note that the predominance of S-waves in the seismic signals does not necessarily establish a shear rupture mechanism. S-wave dominated signals can arise from volumetric sources with non-spherical geometries [e.g., 66] or from single-force sources associated with fast local pressure variations [85].…”
Section: Introductionmentioning
confidence: 99%