Transition from calc-alkaline to potassium-rich magmatism in subduction environments: geochemical and Sr, Nd, Pb isotopic constraints from the island of Vulcano (Aeolian arc)
The problem of mantle metasomatism vs. crustal contamination in the genesis of arc magmas with different potassium contents has been investigated using new trace element and Sr-Nd-Pb isotopic data on the island of Vulcano, Aeolian arc. The analysed rocks range in age from 120 ka to the present day,...
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| Veröffentlicht in: | Contributions to mineralogy and petrology 2000-10, Vol.139 (6), p.684-703 |
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| container_title | Contributions to mineralogy and petrology |
| container_volume | 139 |
| creator | De Astis, Gianfilippo Peccerillo, Angelo Kempton, Pamela D. La Volpe, Luigi Wu, Tsai W. |
| description | The problem of mantle metasomatism vs. crustal contamination in the genesis of arc magmas with different potassium contents has been investigated using new trace element and Sr-Nd-Pb isotopic data on the island of Vulcano, Aeolian arc. The analysed rocks range in age from 120 ka to the present day, and cover a compositional range from basalt to rhyolite of the high-K calc-alkaline (HKCA) to shoshonitic (SHO) and potassic (KS) series. |
| doi_str_mv | 10.1007/s004100000172 |
| format | Article |
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| issn | 0010-7999 1432-0967 |
| language | eng |
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| subjects | Basalt Geology Islands Lava Mineralogy Minerals Petrology Potassium Trace elements |
| title | Transition from calc-alkaline to potassium-rich magmatism in subduction environments: geochemical and Sr, Nd, Pb isotopic constraints from the island of Vulcano (Aeolian arc) |
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