E
Eric Reusser
Researcher at ETH Zurich
Publications - 53
Citations - 1722
Eric Reusser is an academic researcher from ETH Zurich. The author has contributed to research in topics: Metamorphism & Explosive eruption. The author has an hindex of 20, co-authored 53 publications receiving 1479 citations. Previous affiliations of Eric Reusser include École Polytechnique Fédérale de Lausanne.
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Preliminary Characterisation of New Glass Reference Materials (GSA‐1G, GSC‐1G, GSD‐1G and GSE‐1G) by Laser Ablation‐Inductively Coupled Plasma‐Mass Spectrometry Using 193 nm, 213 nm and 266 nm Wavelengths
TL;DR: In this paper, a prototype solid state laser ablation system capable of producing wavelengths of 193 nm, 213 nm and 266 nm was used to evaluate the influence of energy density on quantitative analysis.
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Characterization of polymetamorphism in the Austroalpine basement east of the Tauern Window using garnet isopleth thermobarometry
TL;DR: Garnet in metapelites from the Wolz and Rappold Complexes of the Austroalpine basement east of the Tauern Window typically shows two distinct growth zones as mentioned in this paper.
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Deformation experiments of bubble‐ and crystal‐bearing magmas: Rheological and microstructural analysis
Mattia Pistone,Luca Caricchi,Peter Ulmer,Luigi Burlini,Paola Ardia,Eric Reusser,Federica Marone,Laurent Arbaret +7 more
TL;DR: In this paper, simple shear deformation experiments on three-phase, hydrous, haplogranitic magmas, composed of quartz crystals (24-65 vol%), CO2-rich gas bubbles (9-12 vol%) and melt in different proportions, were performed with a Paterson-type rock deformation apparatus.
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Petrology and Trace Element Budgets of High-pressure Peridotites Indicate Subduction Dehydration of Serpentinized Mantle (Cima di Gagnone, Central Alps, Switzerland)
TL;DR: The Gagnone ultramafic suite is also characterized by fluid-mobile element enrichments (B, Pb, As, Sb, Cs, Li, U, Be), which confirm derivation from variably serpentinized protoliths.
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Magmatic-to-hydrothermal crystallization in the W-Sn mineralized Mole Granite (NSW, Australia) : Part I : Crystallization of zircon and REE-phosphates over three million years-a geochemical and U-Pb geochronological study
TL;DR: In this article, it was concluded that it precipitated from a hydrothermal brine ≤ 600 °C, which is below the accepted closure temperature for U-Pb in this mineral.