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GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010
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Zeitschriftentitel: | Terra Nova |
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Personen und Körperschaften: | , , |
In: | Terra Nova, 24, 2012, 2, S. 148-155 |
Format: | E-Article |
Sprache: | Englisch |
veröffentlicht: |
Wiley
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Schlagwörter: |
author_facet |
Palano, Mimmo Guarrera, Elisa Mattia, Mario Palano, Mimmo Guarrera, Elisa Mattia, Mario |
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author |
Palano, Mimmo Guarrera, Elisa Mattia, Mario |
spellingShingle |
Palano, Mimmo Guarrera, Elisa Mattia, Mario Terra Nova GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 Geology |
author_sort |
palano, mimmo |
spelling |
Palano, Mimmo Guarrera, Elisa Mattia, Mario 0954-4879 1365-3121 Wiley Geology http://dx.doi.org/10.1111/j.1365-3121.2011.01049.x <jats:sec><jats:label /><jats:p>Terra Nova, 24, 148–155, 2012</jats:p></jats:sec><jats:sec><jats:title>Abstract</jats:title><jats:p>GPS measurements on Mount St. Helens spanning the 2004.00–2010.85 time interval, encompassing the 2004–2008 dome‐building eruption, were analysed. First, a local reference frame was derived to isolate the volcanic ground deformation from the background tectonic pattern related to the interactions between the Pacific, Juan de Fuca and North American plates. Secondly, the resulting ground deformation patterns were modelled to constrain magmatic sources. Results suggest a vertically elongated magma chamber centred at 8–9 km depth beneath the summit area that deflated during the beginning of the dome growth and inflated since January 2008, indicating that the same primary magma reservoir was active both during and after the eruption in a magmatic system that is persistent over the time.</jats:p></jats:sec> GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 Terra Nova |
doi_str_mv |
10.1111/j.1365-3121.2011.01049.x |
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Online |
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Geologie und Paläontologie |
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Wiley, 2012 |
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2012 |
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Wiley |
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Terra Nova |
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title |
GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_unstemmed |
GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_full |
GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_fullStr |
GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_full_unstemmed |
GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_short |
GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_sort |
gps ground deformation patterns at mount st. helens (washington, usa) from 2004 to 2010 |
topic |
Geology |
url |
http://dx.doi.org/10.1111/j.1365-3121.2011.01049.x |
publishDate |
2012 |
physical |
148-155 |
description |
<jats:sec><jats:label /><jats:p>Terra Nova, 24, 148–155, 2012</jats:p></jats:sec><jats:sec><jats:title>Abstract</jats:title><jats:p>GPS measurements on Mount St. Helens spanning the 2004.00–2010.85 time interval, encompassing the 2004–2008 dome‐building eruption, were analysed. First, a local reference frame was derived to isolate the volcanic ground deformation from the background tectonic pattern related to the interactions between the Pacific, Juan de Fuca and North American plates. Secondly, the resulting ground deformation patterns were modelled to constrain magmatic sources. Results suggest a vertically elongated magma chamber centred at 8–9 km depth beneath the summit area that deflated during the beginning of the dome growth and inflated since January 2008, indicating that the same primary magma reservoir was active both during and after the eruption in a magmatic system that is persistent over the time.</jats:p></jats:sec> |
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author | Palano, Mimmo, Guarrera, Elisa, Mattia, Mario |
author_facet | Palano, Mimmo, Guarrera, Elisa, Mattia, Mario, Palano, Mimmo, Guarrera, Elisa, Mattia, Mario |
author_sort | palano, mimmo |
container_issue | 2 |
container_start_page | 148 |
container_title | Terra Nova |
container_volume | 24 |
description | <jats:sec><jats:label /><jats:p>Terra Nova, 24, 148–155, 2012</jats:p></jats:sec><jats:sec><jats:title>Abstract</jats:title><jats:p>GPS measurements on Mount St. Helens spanning the 2004.00–2010.85 time interval, encompassing the 2004–2008 dome‐building eruption, were analysed. First, a local reference frame was derived to isolate the volcanic ground deformation from the background tectonic pattern related to the interactions between the Pacific, Juan de Fuca and North American plates. Secondly, the resulting ground deformation patterns were modelled to constrain magmatic sources. Results suggest a vertically elongated magma chamber centred at 8–9 km depth beneath the summit area that deflated during the beginning of the dome growth and inflated since January 2008, indicating that the same primary magma reservoir was active both during and after the eruption in a magmatic system that is persistent over the time.</jats:p></jats:sec> |
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imprint | Wiley, 2012 |
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institution | DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1 |
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series | Terra Nova |
source_id | 49 |
spelling | Palano, Mimmo Guarrera, Elisa Mattia, Mario 0954-4879 1365-3121 Wiley Geology http://dx.doi.org/10.1111/j.1365-3121.2011.01049.x <jats:sec><jats:label /><jats:p>Terra Nova, 24, 148–155, 2012</jats:p></jats:sec><jats:sec><jats:title>Abstract</jats:title><jats:p>GPS measurements on Mount St. Helens spanning the 2004.00–2010.85 time interval, encompassing the 2004–2008 dome‐building eruption, were analysed. First, a local reference frame was derived to isolate the volcanic ground deformation from the background tectonic pattern related to the interactions between the Pacific, Juan de Fuca and North American plates. Secondly, the resulting ground deformation patterns were modelled to constrain magmatic sources. Results suggest a vertically elongated magma chamber centred at 8–9 km depth beneath the summit area that deflated during the beginning of the dome growth and inflated since January 2008, indicating that the same primary magma reservoir was active both during and after the eruption in a magmatic system that is persistent over the time.</jats:p></jats:sec> GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 Terra Nova |
spellingShingle | Palano, Mimmo, Guarrera, Elisa, Mattia, Mario, Terra Nova, GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010, Geology |
title | GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_full | GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_fullStr | GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_full_unstemmed | GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_short | GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
title_sort | gps ground deformation patterns at mount st. helens (washington, usa) from 2004 to 2010 |
title_unstemmed | GPS ground deformation patterns at Mount St. Helens (Washington, USA) from 2004 to 2010 |
topic | Geology |
url | http://dx.doi.org/10.1111/j.1365-3121.2011.01049.x |