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Geochronology, geochemistry and tectonic implications of Xiongshan diabasic dike swarm, northern Fujian
Authors:Shengli Ren  Jiliang Li  Xinhua Zhou  Min Sun
Institution:(1) Department of Earth Science, China University of Geosciences, 100083 Beijing, China;(2) Institute of Geology, Chinese Academy of Sciences, 100029 Beijing, China;(3) Department of Earth Sciences, University of Hong Kong, Hong Kong
Abstract:Sm/Nd isotopic age determination showed that Xiongshan dike swarm was at 585.7 Ma ± 30 Ma. The trace element geochemistry and Sr/Nd/Pb isotope gemhemistry studies indicate that the dike swarm was products of back-arc basin spreading ridge and the magma originated from the depleted mantle region which was metasomatized by LILE-rich liquids/melts derived from subduction slab. Project supported by the National Natural Science Foundation of China.
Keywords:dike swarm  petrochemistry  Sinian-early Paleozoic  back-arc basin  northern Fujian
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