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    Volume 43 Issue 1
    Jan.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(1): 57-81
    Wan Yusheng, Dong Chunyan, Xie Hangqiang, Xie Shiwen, Liu Shoujie, Bai Wenqian, Ma Mingzhu, Liu Dunyi, 2018. Formation Age of BIF-Bearing Anshan Group Supracrustal Rocks in Anshan-Benxi Area: New Evidence from SHRIMP U-Pb Zircon Dating. Earth Science, 43(1): 57-81. doi: 10.3799/dqkx.2018.004
    Citation: Wan Yusheng, Dong Chunyan, Xie Hangqiang, Xie Shiwen, Liu Shoujie, Bai Wenqian, Ma Mingzhu, Liu Dunyi, 2018. Formation Age of BIF-Bearing Anshan Group Supracrustal Rocks in Anshan-Benxi Area: New Evidence from SHRIMP U-Pb Zircon Dating. Earth Science, 43(1): 57-81. doi: 10.3799/dqkx.2018.004
    shu

    Formation Age of BIF-Bearing Anshan Group Supracrustal Rocks in Anshan-Benxi Area: New Evidence from SHRIMP U-Pb Zircon Dating

    doi: 10.3799/dqkx.2018.004

    • Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    • Received Date: 2017-06-28
    • Publish Date: 2018-01-15
      Abstract
    • Anshan-Benxi is one of the most important BIF concentration areas in the North China Craton, the BIF occurred in the Anshan Group supracrustal rocks. Using SHRIMP U-Pb zircon dating technique, 12 supracrustal samples of the Anshan Group were analyzed. Most samples present 2.50-2.55 Ga zircon ages and 2.7-3.5 Ga detrital or xenocrystal zircons are observed in some samples. Combined with previous studies, main conclusions can be drawn as follows. (1) The widespread BIF-bearing Anshan Group supracrustal rocks in the Anshan-Benxi area were deposited during the Late Neoarchean. (2) The Anshan Group supracrustal rocks were formed over a continental basement. This study confirms that Anshan-Benxi is an important conponent of the huge Late Neoarchean BIF belt along the western margin of the eastern ancient terrane, and stable tectonic environment seems to be a key factor for the formation of huge-scale BIF ore deposit.

       

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