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Bruno Scaillet

Researcher at University of Orléans

Publications -  196
Citations -  11613

Bruno Scaillet is an academic researcher from University of Orléans. The author has contributed to research in topics: Magma & Volcano. The author has an hindex of 61, co-authored 187 publications receiving 10108 citations. Previous affiliations of Bruno Scaillet include Centre national de la recherche scientifique & Blaise Pascal University.

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A theoretical framework for volcanic degassing chemistry in a comparative planetology perspective and implications for planetary atmospheres

TL;DR: In this article, the authors show that the pressure at which degassing occurs, that is the atmospheric pressure in most sensible cases, has a prime influence on the composition of subaerial volcanic gases on planets: high surface pressure produces N 2 -and CO 2 -rich and dry volcanic gases, while low pressure promotes sulfur-rich gases.
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Badrinath-Gangotri plutons (Garhwal, India): petrological and geochemical evidence for fractionation processes in a high Himalayan leucogranite

TL;DR: The Gangotri leucogranite is the western end of the Badrinath granite, one of the largest bodies of the High Himalayan Leucogrite belt (HHL) as discussed by the authors.
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Petrological and Experimental Constraints on the Pre-eruption Conditions of Holocene Dacite from Volcan San Pedro (36 S, Chilean Andes) and the Importance of Sulphur in Silicic Subduction-related Magmas

TL;DR: In this article, an experimental and petrological study aimed at estimating the pre-eruptive conditions of a Holocene dacitic lava from Volcan San Pedro (36°S, Chilean Andes).
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The sulfur content of volcanic gases on Mars

TL;DR: In this article, the authors find that the martian mantle contains at least 3-4 times as much sulfur as its terrestrial counterpart, yielding basaltic melts richer in sulfur than those on Earth.
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Experimental Crystallization of a High-K Arc Basalt: the Golden Pumice, Stromboli Volcano (Italy)

TL;DR: In this paper, the near-liquidus crystallization of a high-K basalt (PST-9 golden pumice) from the present-day activity of Stromboli (Aeolian Islands, Italy) has been experimentally investigated between 1050 and 1175°C, at pressures from 50 to 400 MPa, for melt H2O concentrations between 1·2 and 5·5 wt % and {Delta}NNO ranging from −0·07 to +2·32.