Abstract
The Danfeng meta-volcanics in the Shangzhou area, Shaanxi Province are characterized by oceanic island arc volcanic geochemistry. They are a suite of low-K tholeiitic series and calc-alkaline series meta-volcanic rocks derived from different sources respectively. These meta-volcanics have high Th/Ta ratios and low contents of Ni, Ta, Ti, Y and Yb, suggesting that they were influenced by the subduction zone components. Many lines of evidence show that the Danfeng meta-volcanics were produced in an oceanic island are setting of the supra-subduction zone at the southern margin of the North China Block during the Early Paleozoic.
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This project was funded by the National Natural Science Foundation of China.
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Chengli, Z., Dingwu, Z., Song, H. et al. Geochemical characteristics of Danfeng meta-volcanic rocks in Shangzhou area, Shaanxi Province. Chin. J. of Geochem. 14, 203–211 (1995). https://doi.org/10.1007/BF02842043
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DOI: https://doi.org/10.1007/BF02842043