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• W1982804548 endingPage "265" @default.
• W1982804548 startingPage "254" @default.
• W1982804548 abstract "We report the first sensitive high-resolution ion microprobe (SHRIMP) U–Pb zircon ages with geochemical data from metavolcanic rocks in the Lolotoi complex, Timor. The zircon U–Pb ages of two andesitic metavolcanic rocks yield a permissible range of the Middle Jurassic extrusion from 177 Ma to 174 Ma. The geochemical data indicate that the origins of the basaltic and andesitic metavolcanic rocks are products of prolonged oceanic crust and arc magmatism, respectively. They are originated from partial melting of lherzolites, providing an insight into the tectonic evolution of the forearc basements of the Banda volcanic arc. Thus, parts of the Banda forearc basement are pieces of allochthonous oceanic basalts and Jurassic arc-related andesites accreted to the Sundaland during the closure of Mesotethys, and are incorporated later into the Great Indonesian Volcanic Arc system along the southeastern margin of the Sundaland." @default.
• W1982804548 created "2016-06-24" @default.
• W1982804548 creator A5023718948 @default.
• W1982804548 creator A5024390793 @default.
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• W1982804548 date "2014-12-01" @default.
• W1982804548 modified "2023-10-16" @default.
• W1982804548 title "Evidence for the Jurassic arc volcanism of the Lolotoi complex, Timor: Tectonic implications" @default.
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• W1982804548 doi "https://doi.org/10.1016/j.jseaes.2014.05.007" @default.
• W1982804548 hasPublicationYear "2014" @default.
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