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Anne-Sylvie André-Mayer

Researcher at University of Lorraine

Publications -  53
Citations -  847

Anne-Sylvie André-Mayer is an academic researcher from University of Lorraine. The author has contributed to research in topics: Metamorphism & Pyrite. The author has an hindex of 17, co-authored 50 publications receiving 650 citations. Previous affiliations of Anne-Sylvie André-Mayer include Nancy-Université.

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A-type granites from the Pan-African orogenic belt in south-western Chad constrained using geochemistry, Sr–Nd isotopes and U–Pb geochronology

TL;DR: The Zabili granitic pluton (SW Chad) exposed in the Mayo Kebbi massif is dominated by a coarse-grained hornblende-biotite granite grading into a finegrained biotite granite along its southern margin this paper.
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Erratum to Boiling and vertical mineralization zoning: a case study from the Apacheta low-sulfidation epithermal gold-silver deposit, southern Peru

TL;DR: The Apacheta mine as mentioned in this paper is located in the Shila district, 600 km southeast of Lima in the Cordillera Occidental of Arequipa Province, southern Peru.
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Fluid record of rock exhumation across the brittle-ductile transition during formation of a Metamorphic Core Complex (Naxos Island, Cyclades, Greece)

TL;DR: Fluid inclusions trapped in quartz veins hosted by a leucogneiss from the southern part of the Naxos Metamorphic Core Complex (Attic-Cycladic-Massif, Greece) were studied to determine the evolution of the fluid record of metamorphic rocks during their exhumation across the ductile/brittle transition.
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Trace Element Distribution (Cu, Ga, Ge, Cd, and Fe) IN Sphalerite From the Tennessee MVT Deposits, USA, By Combined EMPA, LA-ICP-MS, Raman Spectroscopy, and Crystallography

TL;DR: In this paper, the substitution mechanisms that control the incorporation of trace elements in sphalerite and relate these mechanisms to the conditions of metal deposition were investigated and compared in two mining districts in the center (Central Tennessee Mines: CT) and east (East Tennessee Mines, ET) of Tennessee in order to understand the substitution mechanism that control incorporation of the trace elements.
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Diagenetic origin of the stratiform Cu–Co deposit at Kamoto in the Central African Copperbelt

TL;DR: In this article, the authors present Re-Os dating results for disseminated and stratiform Cu-Co sulfide pseudomorphs after anhydrite in nodules and layers from the Central African Copperbelt.