Inversion of coeval shear and normal stress of Piton de la Fournaise flank displacement

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Automated identification, location, and volume estimation of rockfalls at Piton de la Fournaise volcano

Since the collapse of the Dolomieu crater floor at Piton de la Fournaise Volcano (la Réunion) in 2007, hundreds of seismic signals generated by rockfalls have been recorded daily at the Observatoire Volcanologique du Piton de la Fournaise (OVPF). To study rockfall activity over a long period of time, automated methods are required to process the available continuous seismic records. We present ...

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Lead isotopes behavior in the fumarolic environment of the Piton de la Fournaise volcano (Réunion Island)

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Solid Earth

سال: 2016

ISSN: 2169-9313,2169-9356

DOI: 10.1002/2016jb013330