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YIN Ming, GUO Min, ZHANG Hai-dong. Petrogenesis and Evolution of Mesozoic Complexes from Southern Taihang Orogen[J]. Northwestern Geology, 2014, 47(3): 43-53.
Citation: YIN Ming, GUO Min, ZHANG Hai-dong. Petrogenesis and Evolution of Mesozoic Complexes from Southern Taihang Orogen[J]. Northwestern Geology, 2014, 47(3): 43-53.

Petrogenesis and Evolution of Mesozoic Complexes from Southern Taihang Orogen

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  • Received Date: June 14, 2014
  • Revised Date: August 09, 2014
  • Available Online: July 28, 2022
  • Published Date: September 04, 2014
  • Pingshun-FuShan-WuAn-HongShan complex mainly consists of olivine-gabbro-diabase, hornblende diorite, diorite, monzodiorite, syenite and granite, which have similar geochemical properties. The content of CaO, FeO, MgO, TiO and SiO2 are in linear positive correlation. The composite pluton is enriched in lithophylic elements (such as Sr, Ba, K) and LREE, but is depleted in high field strength elements (such as Nb, Ta, Ti) and HREE, and there is a weak positive Eu anomaly. The value of epsilon Nd(t) varies from -12.3 to -16.9 in FuShan complex, with that ofⅠSr ranges from 0.7056 to 0.7071; the value of epsilon Nd(t) varies from -13.8 to -18 in WuAn complex, and the value ofⅠSr is between 0.7059~0.7076. By contrast, the values of εNd (-8.2~-11) in HongShan complex is obviously higher and relatively more homogeneous than that in FuShan-WuAn complex, and the value of ISr (0.705 2~0.710 2) has a greater variety. Pb isotope ratio of PingShui complex is relatively higher, the values of (206Pb/204Pb)I, (207Pb/204Pb)I and (208Pb/204Pb)i are respectively 17.859~18.474, 15.429~15.612, 37.374~38.641, while those of FuShan complex (16.92~17.3, 15.32~15.42, 37.16~37.63), WuAn complex (16.63~17.4, 15.28~15.44, 36.78~37.3), and HongShan complex (17.28~17.74, 15.40~15.48, 37.01~38.12) change continuously. Pingshun-Fushan-Wuan complexes are probably the products of contemporaneous magma evolution, originated from the partial melting of EMI-enriched mantle, but experienced different degrees of hybridization of crust materials in the rising process. Hongshan complex also originated from the partial melting of EMI-enriched mantle, but belonged to different magmatic thermal event, and merely experienced slight hybridization of crust materials. The extensive Mesozoic Magmatic Activity of southern Taihang Mountain is probably related to the plume upwelling of Hanxing.
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