M
Maria Ovtcharova
Researcher at University of Geneva
Publications - 64
Citations - 3460
Maria Ovtcharova is an academic researcher from University of Geneva. The author has contributed to research in topics: Zircon & Geochronology. The author has an hindex of 28, co-authored 60 publications receiving 2889 citations. Previous affiliations of Maria Ovtcharova include ETH Zurich & Sofia University.
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Timing of the Early Triassic carbon cycle perturbations inferred from new U–Pb ages and ammonoid biochronozones.
Thomas Galfetti,Hugo Bucher,Maria Ovtcharova,Urs Schaltegger,Arnaud Brayard,Thomas Brühwiler,Nicolas Goudemand,Helmut Weissert,Peter A. Hochuli,Fabrice Cordey,Kuang Guodun +10 more
TL;DR: Based on analyses of single, thermally annealed and chemically abraded zircons, a new high-precision U-Pb age of 251.22± 0.20 Ma is established for a volcanic ash layer within the “Kashmirites densistriatus beds” of early Smithian age (Early Triassic) from the Luolou Formation (northwestern Guangxi, South China) as discussed by the authors.
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The Bushveld Complex was emplaced and cooled in less than one million years – results of zirconology, and geotectonic implications
TL;DR: The Rustenburg Layered Suite (RLS) represents Earth's oldest large igneous province ( > 370 000 km 3 ), and contains the world's largest reserves of platinum-group elements, chromium and vanadium as discussed by the authors.
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New Early to Middle Triassic U–Pb ages from South China: Calibration with ammonoid biochronozones and implications for the timing of the Triassic biotic recovery
TL;DR: In this article, new zircon U-Pb ages are proposed for late Early and Middle Triassic volcanic ash layers from the Luolou and Baifeng formations (northwestern Guangxi, South China).
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How Accurately Can We Date the Duration of Magmatic-Hydrothermal Events in Porphyry Systems?—An Invited Paper
Massimo Chiaradia,Urs Schaltegger,Richard Alan Spikings,Jörn-Frederik Wotzlaw,Maria Ovtcharova +4 more
TL;DR: In this article, the authors discuss some fundamental problems that are systematically overlooked in most geochronological studies trying to bracket the life span of porphyry systems, and they show that if these problems are not adequately taken into account and tackled the result will be that fundamentally wrong life spans of pormorphry systems will be estimated.
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Incremental growth of the Patagonian Torres del Paine laccolith over 90 k.y
TL;DR: The Miocene Paine Granite in the Torres del Paine Intrusive Complex, southern Chile, is an extraordinary example of an upper crustal mafic and granitic intrusion.