Geochronology, geochemistry and tectonic implications of Xiongshan diabasic dike swarm, northern Fujian |
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Authors: | Shengli Ren Jiliang Li Xinhua Zhou Min Sun |
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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 |
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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. |
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Keywords: | dike swarm petrochemistry Sinian-early Paleozoic back-arc basin northern Fujian |
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