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In the western peripheral area of PdF we document the broadly synchronous eruptions of (1) primitive olivine and olivine\u2013clinopyroxene transitional basalts with tholeiitic affinity that are closely associated in space with (2) transitional olivine basalts with alkaline affinity, and (3) hybrid lavas, intermediate between the \u2018alkaline\u2019 and the \u2018tholeiitic\u2019 end-members. The composition of the latter overlaps with that of the lavas frequently erupted from the conduit system feeding the main summit cone. AlphaMELTS modelling, and fluid inclusion and clinopyroxene barometry, constrain the conditions of magma storage at 10\u201330\u2009km, and the ascent of magma from the upper mantle to the shallow crustal plumbing system. Variable degrees of mantle melting, together with minor source heterogeneity and contamination with cumulate-derived partial melts, contribute to the diversity of PdF magmas. However, all these processes do not represent the dominant factors that produce the large variability we found in major element composition. Indeed, the composition of basalts erupted from PdF peripheral centers is strongly controlled by polybaric olivine\u2013clinopyroxene fractionation at pressures higher than 3\u2009kbar. Crystal textures and geochemical modelling suggest that fast magma ascent is critical to prevent clinopyroxene dissolution. Conversely, long-lasting magma stagnation promotes pyroxene resorption and magma differentiation. \u2018Central\u2019 eruptions occurring close to the PdF summit cone emit variably more evolved melts, which result from olivine\u2013clinopyroxene\u2013plagioclase differentiation at intermediate\u2013shallow pressure (&amp;lt;3\u2009kbar and in most cases &amp;lt;1\u2009kbar). Deep and extensive magma mixing before injection into the crustal magma conduit system, located below the summit region, results in the apparent homogeneity of basalts erupted from the central area. As regards \u2018peripheral\u2019 eruptions, deep-seated stagnation of basaltic melts and differentiation at the mantle\u2013crust transition zone (c. 4\u2009kbar) produces a range of magma compositions. We demonstrate that rapid magma ascent from deep-seated reservoirs can bypass the central plumbing system. The eruptions of these magmas both in the central area and on the densely populated flanks have major consequences in terms of volcanic hazard at PdF.<\/jats:p>","DOI":"10.1093\/petrology\/egz045","type":"journal-article","created":{"date-parts":[[2019,10,16]],"date-time":"2019-10-16T22:20:07Z","timestamp":1571264407000},"page":"1717-1752","source":"Crossref","is-referenced-by-count":21,"title":["Eruptive Activity on the Western Flank of Piton de la Fournaise (La R\u00e9union Island, Indian Ocean): Insights on Magma Transfer, Storage and Evolution at an Oceanic Volcanic Island"],"prefix":"10.1093","volume":"60","author":[{"given":"G","family":"Boudoire","sequence":"first","affiliation":[{"name":"Laboratoire G\u00e9osciences R\u00e9union, Universit\u00e9 de La R\u00e9union, Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Saint-Denis F-97715, France"},{"name":"Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Universit\u00e9 Paris Diderot, Bourg Murat, France"}]},{"given":"Y -A","family":"Brugier","sequence":"additional","affiliation":[{"name":"Institut des Sciences de la Terre d\u2019Orl\u00e9ans (ISTO): UMR 7327, Universit\u00e9 d\u2019Orl\u00e9ans, 45071 Orl\u00e9ans, France"},{"name":"ISTO, UMR 7327, CNRS, 45071 Orl\u00e9ans, France"},{"name":"ISTO, UMR 7327, BRGM, BP 36009 Orl\u00e9ans, France"}]},{"given":"A","family":"Di Muro","sequence":"additional","affiliation":[{"name":"Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Universit\u00e9 Paris Diderot, Bourg Murat, France"},{"name":"Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Universit\u00e9 Paris Diderot, Paris F-75005, France"}]},{"given":"G","family":"W\u00f6rner","sequence":"additional","affiliation":[{"name":"GZG, Abt. Geochemie, Universit\u00e4t G\u00f6ttingen, Goldschmidtstr. 1, G\u00f6ttingen 37077, Germany"}]},{"given":"I","family":"Arienzo","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia (INGV), Osservatorio Vesuviano, Via Diocleziano 328, Napoli 80124, Italy"}]},{"given":"N","family":"Metrich","sequence":"additional","affiliation":[{"name":"Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Universit\u00e9 Paris Diderot, Paris F-75005, France"}]},{"given":"V","family":"Zanon","sequence":"additional","affiliation":[{"name":"Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Universit\u00e9 Paris Diderot, Paris F-75005, France"},{"name":"Instituto de Investiga\u00e7\u00e3o em Vulcanologia e Avalia\u00e7\u00e3o de Riscos, Universidade dos A\u00e7ores, Rua M\u00e3e de Deus, Ponta Delgada 9500-321, Portugal"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0750-4247","authenticated-orcid":false,"given":"N","family":"Braukm\u00fcller","sequence":"additional","affiliation":[{"name":"Institut f\u00fcr Geologie und Mineralogie, Universit\u00e4t zu K\u00f6ln, Z\u00fclpicher Str. 49b, K\u00f6ln 50674, Germany"}]},{"given":"A","family":"Kronz","sequence":"additional","affiliation":[{"name":"GZG, Abt. Geochemie, Universit\u00e4t G\u00f6ttingen, Goldschmidtstr. 1, G\u00f6ttingen 37077, Germany"}]},{"given":"Y","family":"Le Moigne","sequence":"additional","affiliation":[{"name":"Institut des Sciences de la Terre d\u2019Orl\u00e9ans (ISTO): UMR 7327, Universit\u00e9 d\u2019Orl\u00e9ans, 45071 Orl\u00e9ans, France"},{"name":"ISTO, UMR 7327, CNRS, 45071 Orl\u00e9ans, France"},{"name":"ISTO, UMR 7327, BRGM, BP 36009 Orl\u00e9ans, France"}]},{"given":"L","family":"Michon","sequence":"additional","affiliation":[{"name":"Laboratoire G\u00e9osciences R\u00e9union, Universit\u00e9 de La R\u00e9union, Institut de Physique du Globe de Paris (IPGP), Sorbonne Paris-Cit\u00e9, UMR 7154 CNRS, Saint-Denis F-97715, France"}]}],"member":"286","published-online":{"date-parts":[[2019,10,18]]},"reference":[{"key":"2020101720044438500_egz045-B1","doi-asserted-by":"crossref","first-page":"121","DOI":"10.1029\/2003GL018642","article-title":"Link between major flank slip and 2002\u20132003 eruption at Mt. 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