Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Neuberg, JW"'
Autor:
Contreras-Arratia, R, Neuberg, JW
Previous studies have found discrepancies concerning the seismic radiation between planar and curved faults: moment tensor (MT) interpretations, seismic moment estimation and waveforms change dramatically when the rupture is not planar. Therefore, as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::d18192a92d0161c6e2290ee2f2f5e3de
https://eprints.whiterose.ac.uk/168510/1/Caldera_MT.pdf
https://eprints.whiterose.ac.uk/168510/1/Caldera_MT.pdf
Publikováno v:
Journal of Volcanology and Geothermal Research. 425:107518
Since the eruption began in 1995, Soufrière Hills volcano on Montserrat has been characterised by five phases of magma extrusion and corresponding pauses. Despite a lack of eruptive surface activity since 2010, the volcano continues to show signs of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f088f688bc3cbf7d6ad153ea2e00a5bf
https://doi.org/10.1016/j.jvolgeores.2022.107518
https://doi.org/10.1016/j.jvolgeores.2022.107518
Publikováno v:
Frontiers in Earth Science, Vol 7 (2019)
For optimal monitoring of the deformation of a volcano, instrumentation should be deployed at the location most sensitive to changes at the suspected deformation source. The topographic effect on tilt depends strongly on the orientation of the deform
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ae3b4096833767ce011bb0b7d4bcd2c6
https://doi.org/10.3389/feart.2019.00317
https://doi.org/10.3389/feart.2019.00317
Autor:
Contreras-Arratia, R, Neuberg, JW
Long period (LP) signals are special seismic events observed at volcanoes, which comprise both a high frequency onset due to brittle failure and a more energetic low frequency part due to resonance in a fluid-filled conduit. They are critical for vol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::50b676f0e9cbd8da96a9e5bb92ea0060
https://eprints.whiterose.ac.uk/149518/1/Contreras-Arratia_Neuberg2019.pdf
https://eprints.whiterose.ac.uk/149518/1/Contreras-Arratia_Neuberg2019.pdf
Understanding how magma moves within a conduit is an important question that is still poorly understood. In particular, estimation of the magma ascent rate is key for interpreting monitoring signals and therefore, predicting volcanic activity. This r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::8b30ab084004cd9dd5dcc72d125cc57a
https://eprints.whiterose.ac.uk/135331/9/Thomas2019_Chapter_CrystalsBubblesAndMeltCritical.pdf
https://eprints.whiterose.ac.uk/135331/9/Thomas2019_Chapter_CrystalsBubblesAndMeltCritical.pdf
Cyclic seismicity and ground deformation patterns are observed on many volcanoes worldwide where seismic swarms and the tilt of the volcanic flanks provide sensitive tools to assess the state of volcanic activity. Ground deformation at active volcano
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::c953f5968d579ea22ee863df433a8ead
https://eprints.whiterose.ac.uk/123408/1/Neuberg_EPSL_final.pdf
https://eprints.whiterose.ac.uk/123408/1/Neuberg_EPSL_final.pdf
Autor:
Mangan, TP, Atkinson, JD, Neuberg, JW, O'Sullivan, D, Wilson, TW, Whale, TF, Neve, L, Umo, NS, Malkin, TL, Murray, BJ
Publikováno v:
PLoS ONE, 12 (1)
PLoS ONE, Vol 12, Iss 1, p e0169720 (2017)
PLoS ONE
PLoS ONE, Vol 12, Iss 1, p e0169720 (2017)
PLoS ONE
Fine particles of ash emitted during volcanic eruptions may sporadically influence cloud properties on a regional or global scale as well as influencing the dynamics of volcanic clouds and the subsequent dispersion of volcanic aerosol and gases. It h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a3117d4b838ba310674305ca76c873b5
https://hdl.handle.net/20.500.11850/128368
https://hdl.handle.net/20.500.11850/128368
Autor:
Thomas, ME, Neuberg, JW
The estimation of the magma ascent rate is key to predicting volcanic activity and relies on the understanding of how strongly the ascent rate is controlled by different magmatic parameters. Linking potential changes of such parameters to monitoring
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::9adcf3791384cf712e57f80d70c30192
https://eprints.whiterose.ac.uk/82954/3/Thomas_et_al-2014-Geochemistry,_Geophysics,_Geosystems.pdf
https://eprints.whiterose.ac.uk/82954/3/Thomas_et_al-2014-Geochemistry,_Geophysics,_Geosystems.pdf
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.