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    Volume 42 Issue 3
    Mar.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(3): 357-377
    Zhang Zhenkai, Zhou Yaoqi, Peng Tianming, Yu Shanshan, Yue Huiwen, Zhou Tengfei, Liu Jiazhao, 2017. Geochemical Characteristics and Signatures of Siltstones from Laiyang Group at Lingshan Island, Qingdao, Shandong. Earth Science, 42(3): 357-377. doi: 10.3799/dqkx.2017.027
    Citation: Zhang Zhenkai, Zhou Yaoqi, Peng Tianming, Yu Shanshan, Yue Huiwen, Zhou Tengfei, Liu Jiazhao, 2017. Geochemical Characteristics and Signatures of Siltstones from Laiyang Group at Lingshan Island, Qingdao, Shandong. Earth Science, 42(3): 357-377. doi: 10.3799/dqkx.2017.027
    shu

    Geochemical Characteristics and Signatures of Siltstones from Laiyang Group at Lingshan Island, Qingdao, Shandong

    doi: 10.3799/dqkx.2017.027
    • 1.

      School of Geosciences, China University of Petroleum, Qingdao 266580, China

    • 2.

      Eighth Institute of Geology & Mineral Exploration of Shandong Province, Rizhao 276826, China

    • Received Date: 2016-09-05
    • Publish Date: 2017-03-15
      Abstract
    • Gravity flow deposits of Laiyang Group at the lower part of Lingshan island attract an increasing attention of geologists at home and abroad because of its huge thickness and unique sedimentary features. However, its weathering degree, characteristics and structural setting of provenance, and depositional environment stillremain in dispute. In this study, major elements, rare earth elements and trace elements contents of the siltstones from Laiyang Group at Lingshan Island were examined by XRF and ICP-MS. It is found that siltstones are characterized by relatively low contents of SiO2 (avg. 51.78%) and high contents of Fe2O3T (avg. 51.78%); average contents of Na2O and K2O of siltstones are 2.74% and 2.79%, respectively, the siltstones are classified as litharenites and greywackes; ΣREE contents of the samples are 153.00×10-6-254.38×10-6 (avg. 201.65×10-6), which are higher than those of UCC and PAAS; the pattern of REE is characterized by LREE enrichment, HREE depletion, moderately negative Eu abnormity and weakly negative Ce abnormity; compared with UCC, samples are enriched in LILEs, weakly enriched in HFSEs and depleted in transitional elements. Index of Compositional Variability (ICV) values of siltstones in Lingshan Island are high, which indicates the source materials are mainly primary cycle sediments, Chemical Index of Alteration (CIA) values are relatively low, which suggests that the weathering intensity of provenance is low. Element analysis indicates that felsic rocks serve as the main source rocks, including small amounts of contributions from recycled orogenic belt materials; tectonic settings of provenance belong to active continental margin and continental island arc; sedimentary environment is reducing marine environment and paleoclimate of Laiyang Period was arid. It is original for the authors to apply the statistical analysis method to determine the provenance regions more precisely according to the features of REEs, and it is concluded that the source rocks are most likely from Jiaonan Group and Penglai Group.

       

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