We present an interpretation of all available gravity data on Piton de la Fournaise volcano,
including a new set collected in the summit area. Using a linear programming inversion …

We present an interpretation of gravity data acquired in 1984 by the French R/V Jean
Charcot on the submarine part of the eastern flank of Piton de la Fournaise volcano. We …

The structure and mass transfers at Piton de la Fournaise volcano are investigated using
new on land and offshore measurements. The structures are defined using 2 and 3D …

The sinking of a deep drill hole (3003.5 m) for geothermal exploration in the eastern part of
the Piton de la Fournaise volcano on Réunion Island has revealed the underlying …

The aim of this work is to propose a general model of Piton de la Fournaise volcano using
information from geological and geophysical studies. Firstly, we make a graphical …

The short eruption of June 14–15 1985 was the beginning of an important cycle of activity of
Piton de la Fournaise that lasted more than two years and comprised twenty or so eruptive …

Abstract The Grand Brûlé borehole intersects a thick pile of basaltic lavas, down to 1010 m,
and a basic-ultrabasic intrusive complex, from 1010 to 3003.50 m. The lavas are, in general …

Piton de La Fournaise (Réunion Island) had shown 8 months of high activity during 2003,
including four eruptions and one intrusion. The monitoring networks, provided by the …

Dunites at the base of the Grand Brûlé intrusive body are deformed cumulates with olivine
(Fo 84.5-Fo 87.3) containing exsolution lamellae of spinel, discrete grains of chrome spinel …

Piton de La Fournaise is in a period of intense volcanic activity since 1998. To constrain the
magma dynamics responsible for this activity, we combined GPS ground deformation …