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

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

Research output: Chapter in Book/Report/Conference proceeding › Abstract in proceedings

Abstract

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.

Original language	English
Title of host publication	Proceedings of the European Geothermal Congress
Place of Publication	Pisa
Publisher	European Geothermal Energy Council
Publication status	Published - 2013
Event	European Geothermal Congress 2013 - Pisa, Italy Duration: 3 Jun 2013 → 7 Jun 2013

Conference

Conference	European Geothermal Congress 2013
Country/Territory	Italy
City	Pisa
Period	3/06/13 → 7/06/13

Programme Area

Programme Area 3: Energy Resources

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

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Caldeira, R., Matos, C., Rosa, C., Silveira, G., Ribeiro, L., Matias, L., Dias, N., Krueger, F., Nunes, J., & Rosa, D. (2013). Geochemical and short-period Rayleigh wave dispersion measurements as evaluation tools to estimate Madeira island magma chambers depth. In Proceedings of the European Geothermal Congress European Geothermal Energy Council. https://repositorio.lneg.pt/bitstream/10400.9/1750/1/35489.pdf

@inbook{ea892e0f484c4e20ab4d001aa0299e3e,

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

abstract = "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.",

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

year = "2013",

language = "English",

booktitle = "Proceedings of the European Geothermal Congress",

publisher = "European Geothermal Energy Council",

note = "European Geothermal Congress 2013 ; Conference date: 03-06-2013 Through 07-06-2013",

}

Caldeira, R, Matos, C, Rosa, C, Silveira, G, Ribeiro, L, Matias, L, Dias, N, Krueger, F, Nunes, J & Rosa, D 2013, Geochemical and short-period Rayleigh wave dispersion measurements as evaluation tools to estimate Madeira island magma chambers depth. in Proceedings of the European Geothermal Congress. European Geothermal Energy Council, Pisa, European Geothermal Congress 2013, Pisa, Italy, 3/06/13. <https://repositorio.lneg.pt/bitstream/10400.9/1750/1/35489.pdf>

TY - CHAP

T1 - Geochemical and short-period Rayleigh wave dispersion measurements as evaluation tools to estimate Madeira island magma chambers depth

AU - Caldeira, R

AU - Matos, C

AU - Rosa, C

AU - Silveira, G

AU - Ribeiro, L

AU - Matias, L

AU - Dias, N

AU - Krueger, F

AU - Nunes, J.

AU - Rosa, D.

PY - 2013

Y1 - 2013

N2 - 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.

AB - 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.

M3 - Abstract in proceedings

BT - Proceedings of the European Geothermal Congress

PB - European Geothermal Energy Council

CY - Pisa

T2 - European Geothermal Congress 2013

Y2 - 3 June 2013 through 7 June 2013

ER -

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

Abstract

Conference

Programme Area

UN SDGs

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