Toward a Continuum Geothermal Model to Explain Coexistence of Medium to High (100 to 250°C) Temperature Geothermal Systems in Martinique and Guadeloupe, French West Indies - BRGM - Bureau de recherches géologiques et minières Access content directly
Journal Articles Geothermal Research Council Transactions Year : 2014

Toward a Continuum Geothermal Model to Explain Coexistence of Medium to High (100 to 250°C) Temperature Geothermal Systems in Martinique and Guadeloupe, French West Indies

Abstract

The recent surface exploration data acquired in Martinique led to a revisit of the conceptual models of three geothermal systems in active volcanic arc context: Petite Anse in the Southwest of the island, Lamentin in the center, Montagne Pelée in the North. These three explored systems are compared with each other and with the developed Bouillante geothermal field in Guadeloupe (15 MWe). From parameters, such as reservoir temperature, duration of the geothermal system using fossils events, age and duration of magmatism, degree of equilibrium of geothermal fluid, we propose a continuum model of geothermal system including three successive stages: prograde, peak and retrograde.

Domains

Applied geology
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Dates and versions

hal-01016559 , version 1 (30-06-2014)

Identifiers

  • HAL Id : hal-01016559 , version 1

Cite

Vincent Bouchot, Alain Gadalia, Hervé Traineau, Séverine Caritg. Toward a Continuum Geothermal Model to Explain Coexistence of Medium to High (100 to 250°C) Temperature Geothermal Systems in Martinique and Guadeloupe, French West Indies. Geothermal Research Council Transactions, 2014, 38, pp.1. ⟨hal-01016559⟩

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