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作 者:张仁杰 冯少南 徐光洪 杨德骊 鄢道平 李志宏 蒋大海 吴炜
机构地区:[1]Yichang Institute of Geology and Mineral Resources, Yichang 443003, PRC [2]Hainan Bureau of Geology and Mineral Resources, Hailkou 570001, PRC
出 处:《Science China Chemistry》1990年第2期211-222,共12页中国科学(化学英文版)
摘 要:The late Precambrian algal megafossils, Chuaria-Tawuia assemblage, were found for the first time in Bed 6 of the Shilu Group, Hainan Island, South China. Consequently. the geological age of the iron-ore deposits of the Shilu Group can be determined and placed into the Qingbaikou System. This meaningful discovery offers sufficient evidence for settling the protracted dispute over the ore-forming age of the Shilu iron deposits, and will be of great help for better understanding the evolutional history of geology and tectonics, as well as the further ore-prospecting of the Shilu-type iron-deposits both in the island and South China.The late Precambrian algal megafossils, Chuaria-Tawuia assemblage, were found for the first time in Bed 6 of the Shilu Group, Hainan Island, South China. Consequently. the geological age of the iron-ore deposits of the Shilu Group can be determined and placed into the Qingbaikou System. This meaningful discovery offers sufficient evidence for settling the protracted dispute over the ore-forming age of the Shilu iron deposits, and will be of great help for better understanding the evolutional history of geology and tectonics, as well as the further ore-prospecting of the Shilu-type iron-deposits both in the island and South China.
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