Geochemical and short-period Rayleigh wave dispersion measurements as evaluation tools to estimate Madeira island magma chambers depth

R Caldeira, C Matos, C Rosa, G Silveira, L Ribeiro, L Matias, N Dias, F Krueger, J. Nunes, D. Rosa

Publikation: Bidrag til bog/rapport/konferenceproceedingsAbstract i proceedings

Abstrakt

Madeira is an intraplate volcanic island that shows evidences of recent volcanism. In a volcanic geothermal system the heat source comes from magma emplacement at relatively shallow levels, thus knowledge of magma chamber(s) depth(s) is one of
the keys to geothermal reservoir assessment. The tentative definition of these depths in Madeira is being studied by the integration of petrographic, petrological, geochemical and geophysical methods.
OriginalsprogEngelsk
TitelProceedings of the European Geothermal Congress
UdgivelsesstedPisa
ForlagEuropean Geothermal Energy Council
Antal sider7
StatusUdgivet - 2013
BegivenhedEuropean Geothermal Congress 2013 - Pisa, Italien
Varighed: 3 jun. 20137 jun. 2013

Konference

KonferenceEuropean Geothermal Congress 2013
Land/OmrådeItalien
ByPisa
Periode3/06/137/06/13

Programområde

  • Programområde 3: Energiressourcer

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