Implications of magma transfer between multiple reservoirs on eruption cycling

Science

Volumn 322, Issue 5899, 2008, Pages 246-248

  Elsworth, Derek ^a,b   Mattioli, Glen ^c   Taron, Joshua ^a,b   Voight, Barry ^a,b   Herd, Richard ^d  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

^b UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

^c UNIVERSITY OF ARKANSAS   (United States)

^d UNIVERSITY OF EAST ANGLIA   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION; LOWER CRUST; MAGMA; MANTLE; RESERVOIR; SURFACE FLUX; VOLCANIC ERUPTION;

ARTICLE; CARIBBEAN ISLANDS; CRUSTAL RESERVOIR; GEOMORPHOLOGY; IMAGE ANALYSIS; MAGMA EFFLUX; MATHEMATICAL COMPUTING; NONHUMAN; PRIORITY JOURNAL; SOIL EROSION; SURFACE PROPERTY; SURFACE SOIL; VOLCANO;

ATLANTIC ISLANDS; ATLANTIC OCEAN; CARIBBEAN ISLANDS; LEEWARD ISLANDS [LESSER ANTILLES]; LESSER ANTILLES; MONTSERRAT; SOUFRIERE HILLS VOLCANO;

EID: 53749084519     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1161297     Document Type: Article

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16. We thank M. Strutt, G. Ryan, and P. Williams of the Montserrat Volcano Observatory and W. Johnston for maintenance of the cGPS network on the SHV. This work is a result of partial support from NSF under awards NSF-CMS-9908590, NSF-CD-0607691, NSF-CD-0507334, and NSF-CD-0607782. The Caribbean Andesitic Lava Island Precision Seismo-geodetic Observatory (CALIPSO) Facility was supported by grants NSF-IF-0523097 and NSF-IF-0732728, and this support is gratefully acknowledged. The conclusions reported here are those of the authors.