In 1984, a survey of the bathymetry (Seabeam), the gravity and magnetic fields of the submarine east flank of Piton de la Fournaise was performed with R/V "Jean Charcot ". Piton de la Fournaise is one of the most active volcanoes in the world. It is a basaltic shield volcano which occupies the southeast third of Reunion Island in the southwestern Indian Ocean. Three main types of volcanic or volcano-tectonic features have been identified on the Seabeam map
International audienceThis work presents the first exhaustive study of the entire surface of the Reu...
SIGLECNRS T Bordereau / INIST-CNRS - Institut de l'Information Scientifique et TechniqueFRFranc
International audienceThe morphology of Piton de la Fournaise volcano results from the succession of...
In 1984, a Seabeam bathymetric survey and the measurement of the gravity and magnetic fields of the ...
International audienceThe aim of this work is to propose a general model of Piton de la Fournaise vo...
An Audio Magnetotelluric (AMT) profile has been carried out across the Plaine des Sables, a former c...
International audienceThe internal structure of La Réunion (Indian Ocean) is investigated using grav...
La Réunion is a huge volcanic oceanic complex of which most of the volume is submerged. Its internal...
The island of La Réunion is made up of two main shield volcanoes: Piton des Neiges and Piton de la F...
International audienceHistorical and other recent lavas from Piton de la Fournaise (La Réunion Islan...
International audienceIn April 2007, a caldera collapsed at the Dolomieu summit crater of Piton de L...
International audienceThis work presents the first exhaustive study of the entire surface of the Reu...
SIGLECNRS T Bordereau / INIST-CNRS - Institut de l'Information Scientifique et TechniqueFRFranc
International audienceThe morphology of Piton de la Fournaise volcano results from the succession of...
In 1984, a Seabeam bathymetric survey and the measurement of the gravity and magnetic fields of the ...
International audienceThe aim of this work is to propose a general model of Piton de la Fournaise vo...
An Audio Magnetotelluric (AMT) profile has been carried out across the Plaine des Sables, a former c...
International audienceThe internal structure of La Réunion (Indian Ocean) is investigated using grav...
La Réunion is a huge volcanic oceanic complex of which most of the volume is submerged. Its internal...
The island of La Réunion is made up of two main shield volcanoes: Piton des Neiges and Piton de la F...
International audienceHistorical and other recent lavas from Piton de la Fournaise (La Réunion Islan...
International audienceIn April 2007, a caldera collapsed at the Dolomieu summit crater of Piton de L...
International audienceThis work presents the first exhaustive study of the entire surface of the Reu...
SIGLECNRS T Bordereau / INIST-CNRS - Institut de l'Information Scientifique et TechniqueFRFranc
International audienceThe morphology of Piton de la Fournaise volcano results from the succession of...