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首页> 外文期刊>Geological Society of America Bulletin >Recycling of Paleotethyan oceanic crust: Geochemical record from postcollisional mafic igneous rocks in the Tongbai-Hong'an orogens
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Recycling of Paleotethyan oceanic crust: Geochemical record from postcollisional mafic igneous rocks in the Tongbai-Hong'an orogens

机译：古代石海壳的回收：桐柏宏安奥古森后期乳房发泡岩石的地球化学记录

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摘要

Plate tectonics can develop from oceanic subduction to continental collision, with disappearance of presubducted oceanic crust in continental subduction zones. This is typical for collisional orogens where Tethyan oceanic crust was consumed during continental convergence, with recycling of the Tethyan - oceanic crust into the mantle. However, it is difficult to trace the geochemical signature of the previously subducted oceanic crust in collisional orogens. Postcollisional mafic igneous rocks in the Tongbai-Hong'an orogens provide a geochemical record of crust-mantle interaction during Paleotethyan oceanic subduction preceding the Triassic continental collision. These mafic igneous rocks were emplaced in the Cretaceous after continental collision and exhibit oceanic-island basalt (OIB)-like trace-element distribution patterns, with enrichment of large ion litho-phile elements (LILEs) and light rare earth elements (LREEs) but no depletion of high field strength elements (HFSEs). They also show relatively depleted whole-rock Sr-Nd-Hf isotope compositions, with initial Sr-87/Sr-86 ratios of 0.7043-0.7050, epsilon(Nd)(t) values of - 1.8-4.5, and epsilon(Hf)(t) values of 4.7-10.3. Such geochemical features indicate their origin from a juvenile mantle source that contained subducted oceanic crust-derived material. Thus, we suggest that the mantle source was generated by a melt-peridotite reaction at the slab-mantle interface in the Paleotethyan oceanic subduction channel during continental collision. The original peridotite would have been characterized by depletion of melt-mobile incompatible trace elements and radiogenic Sr-Nd-Hf isotopes, corresponding to the juvenile subarc lithospheric mantle. In contrast, the subducted crust-derived material would have been characterized by enrichment of LILEs and LREEs but no depletion of - HFSEs, corresponding to felsic melts that were derived from partial melting of the subducting Paleotethyan oceanic basalt and sediment outside the rutile stability field. As such, the melt-peridotite reaction would generate pyroxenite-rich ultramafic metasomatites in the lower part of the mantle wedge, with relative enrichment of LILEs and LREEs but no depletion of HFSEs. In this model, partial melting of the metasomatites gave rise to the postcollisional mafic igneous rocks in the Tongbai-Hong'an orogens. Therefore, the postcollisional mafic igneous rocks record the recycling of Paleotethyan oceanic crust in the collisional orogen.
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    Dai Li-Qun; Zheng Fei; Zhao Zi-Fu; Zheng Yong-Fei;

  • 作者单位

    Univ Sci &

    Technol China Chinese Acad Sci CAS Key Lab Crust Mantle Mat &

    E Sch Earth &

    Space Sci Hefei 230026 Peoples R China;

    Univ Sci &

    Technol China Chinese Acad Sci CAS Key Lab Crust Mantle Mat &

    E Sch Earth &

    Space Sci Hefei 230026 Peoples R China;

    Univ Sci &

    Technol China Chinese Acad Sci CAS Key Lab Crust Mantle Mat &

    E Sch Earth &

    Space Sci Hefei 230026 Peoples R China;

    Univ Sci &

    Technol China Chinese Acad Sci CAS Key Lab Crust Mantle Mat &

    E Sch Earth &

    Space Sci Hefei 230026 Peoples R China;

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  • 正文语种 eng
  • 中图分类 地质学;
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