Investigating the source characteristics of long-period (LP) seismic events recorded on Piton de la Fournaise volcano, La Réunion

Files in This Item:
File Description SizeFormat 
Zecevic 2013 Investig source.pdf1.65 MBAdobe PDFDownload
Title: Investigating the source characteristics of long-period (LP) seismic events recorded on Piton de la Fournaise volcano, La Réunion
Authors: Zecevic, Megan
De Barros, Louis
Bean, Christopher J.
O'Brien, G. S.
Brenguier, Florent
Permanent link: http://hdl.handle.net/10197/5664
Date: 15-May-2013
Online since: 2014-06-23T14:21:27Z
Abstract: Magmatic and hydrothermal processes play a significant role in generating seismicity at active volcanoes. These signals can be recorded at the surface and can be used to obtain an insight into the volcano's internal dynamics. Long period (LP) events are of particular interest as they often accompany or precede volcanic eruptions, but they are still not well understood. Piton de la Fournaise volcano, La Réunion Island, is one of the most active volcanoes in the world however LP events are rarely recorded there. A seismic network of 20 broadband seismometers has been operational on Piton de la Fournaise volcano since November 2009. Between November 2009 and January 2011 the volcano erupted five times, but only 15 LP events were recorded. Three of these eruptions were preceded by LP events, and several LP events were recorded during an intrusive phase. A family of three repeating LP events exists within the dataset. In order to characterize these events we locate and perform moment tensor inversion on the LP family. The LP events are located within the summit crater at shallow depths (< 200 m below the surface). Inversions show that the source mechanism is best represented by a tensile crack with horizontal crack geometry. We also investigate the relationship between LP occurrence and eruptive characteristics (size of the eruption, deformation of the edifice, etc.), and we find that the events exist only during flank eruptions and can be generated by the activity of the hydrothermal system and/or by the deformation inside the crater.
Type of material: Journal Article
Publisher: Elsevier
Journal: Journal of Volcanology and Geothermal Research
Volume: 258
Issue: 15 May 2013
Start page: 1
End page: 11
Copyright (published version): 2013 Elsevier
Keywords: Long-period eventsPiton de la Fournaise volcanoMoment tensor inversionVolcano seismologySeismology
DOI: 10.1016/j.jvolgeores.2013.04.009
Language: en
Status of Item: Peer reviewed
Appears in Collections:Earth Sciences Research Collection

Show full item record

SCOPUSTM   
Citations 50

9
Last Week
0
Last month
checked on Feb 20, 2019

Google ScholarTM

Check

Altmetric


This item is available under the Attribution-NonCommercial-NoDerivs 3.0 Ireland. No item may be reproduced for commercial purposes. For other possible restrictions on use please refer to the publisher's URL where this is made available, or to notes contained in the item itself. Other terms may apply.