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    Volume 43 Issue 9
    Sep.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(9): 3234-3251
    Sun Miao, Chen Wei, Qu Xiaoming, Ma Xudong, Ding Jishun, 2018. Petrogenesis of the Late Cretaceous Jiangba Volcanic Rocks and Its Indications for the Thinning of the Thickened Crust in Xiongmei Area, Tibet. Earth Science, 43(9): 3234-3251. doi: 10.3799/dqkx.2018.146
    Citation: Sun Miao, Chen Wei, Qu Xiaoming, Ma Xudong, Ding Jishun, 2018. Petrogenesis of the Late Cretaceous Jiangba Volcanic Rocks and Its Indications for the Thinning of the Thickened Crust in Xiongmei Area, Tibet. Earth Science, 43(9): 3234-3251. doi: 10.3799/dqkx.2018.146
    shu

    Petrogenesis of the Late Cretaceous Jiangba Volcanic Rocks and Its Indications for the Thinning of the Thickened Crust in Xiongmei Area, Tibet

    doi: 10.3799/dqkx.2018.146
    • 1.

      Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 2.

      School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • 3.

      College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

    • Received Date: 2017-12-15
    • Publish Date: 2018-09-15
      Abstract
    • The Jiangba Formation volcanic rocks are found in the Xiongmei area in recent years, however its petrogenesis is still unclear. This paper has carried out a systematic petrography, geochemistry and isotopy study on the intermediate-acid Jiangba Formation volcanic rocks in the Xiongmei area, Tibet. The zircon U-Pb age of 85.1±1.0 Ma has been obtained from the dacitic volcanic rocks. The dacitic and andesitic volcanic rocks show the typical geochemical characteristics of adakite, such as high contents of SiO2, Al2O3, Sr concentrations, Mg# values, and Sr/Y ratios, and low contents of Y and Yb. The dacitic and andesitic volcanic rocks are relatively enriched in LREEs (light rare earth elements), depleted in HREEs (heavy rare earth elements), and high (La/Yb)N values without obvious Eu anomalies. The spider diagram of the trace elements of the dacitic and andesitic volcanic rocks display enrichment in Th, Zr and Hf, and depletion in Nb, Ta and Ti. In addition, these dacitic volcanic rocks have positive zircon εHf(t) values (+2.7~+7.1), indicative of the participation of the depleted mantle in the magmatism. These signatures indicate the dacitic volcanic rocks and andesitic volcanic rocks were most likely derived from partial melting of a delaminated young lower crust. The rhyolitic volcanic rocks have relatively lower contents of MgO and TiO2 relative to the dacitic and andesitic volcanic rocks. These rocks are enriched in LREEs, depleted in HREEs, but show less fractionation between LREEs and HREEs than the dacitic and andesitic volcanic rocks, with strongly negative Eu anomalies. On spider diagram of the trace elements, the rhyolitic volcanic rocks show enrichment in Th, Rb and K, and strongly negative Eu, Sr, Ba, P and Ti. These indicate the rhyolitic volcanic rocks were likely derived from remelting of pure crust. These facts indicate a magmatic event caused by the delamination of the thickened lower crust in the Anglonggangri-Bangor magmatic arc of the middle Bangonghu-Nujiang suture zone during the Late Cretaceous.

       

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