期刊
CHEMICAL GEOLOGY
卷 334, 期 -, 页码 266-279出版社
ELSEVIER
DOI: 10.1016/j.chemgeo.2012.10.033
关键词
Melt inclusion; Pb isotopes; Volatile elements; Halogen; Arc magma; Italy
资金
- Agence Nationale de la Recherche [ANR-07-BLAN-0130-01, ANR-09-BLAN-0338]
- European Synthesys FP7 Capacities Specific Program
- ERDF
- Agence Nationale de la Recherche (ANR) [ANR-09-BLAN-0338, ANR-07-BLAN-0130] Funding Source: Agence Nationale de la Recherche (ANR)
Nineteen olivine-hosted melt inclusions from seven volcanoes (Etna, Stromboli, Vulcano, Ustica, Alicudi, Marsili and Vavilov) from the southern Italy region were analyzed for abundances of major, trace, and volatile elements, along with Pb isotope ratios (Pb-207/Pb-206, Pb-208/Pb-206 and Pb-206/Pb-204). The systematics of primary volatile (in particular F and Cl) compositions and Pb isotopes identify three main geochemically distinct mantle sources for this region: (1) a component with radiogenic Pb (Pb-207/Pb-206 = 0.780) and low volatile element abundances typified by the Etnean melt inclusions, (2) a component with moderately radiogenic Pb (Pb-207/Pb-206 = 0.798) and high volatile abundance mainly associated with Sommata magmas, and (3) a component with moderate volatile abundances associated with a MORB-like Pb-207/Pb-206 (0.830). The variation of F/Nd and Pb isotopes among the southern Italy melt inclusions reflects mixing between a slightly modified depleted mantle (DMM-EMII mixture) and radiogenic (HIMU-like) mantle components expressed in Pb isotope space, superimposed by slab-derived metasomatic components represented by F/Nd (F/Nd > 30). (C) 2012 Elsevier B.V. All rights reserved.
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