南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景

毛景文 谢桂青 郭春丽 陈毓川. 南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J]. 岩石学报, 2007, 23(10): 2329-2338.
引用本文: 毛景文 谢桂青 郭春丽 陈毓川. 南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景[J]. 岩石学报, 2007, 23(10): 2329-2338.
Large-scale tungsten-tin mineralization in the Nanling region,South China: Metallogenic ages and corresponding geodynamic processes[J]. Acta Petrologica Sinica, 2007, 23(10): 2329-2338.
Citation: Large-scale tungsten-tin mineralization in the Nanling region,South China: Metallogenic ages and corresponding geodynamic processes[J]. Acta Petrologica Sinica, 2007, 23(10): 2329-2338.

南岭地区大规模钨锡多金属成矿作用:成矿时限及地球动力学背景

  • 基金项目:

    本文为国家重点基础研究发展计划"973"项目(编号:2007CB411405)和中国地质调查局项目(编号:1212010634001)资助成果.

Large-scale tungsten-tin mineralization in the Nanling region,South China: Metallogenic ages and corresponding geodynamic processes

  • 南岭位于华南地区中部,是我国乃至全球最主要的钨锡金属成矿省.本文基于最近几年的高精度成岩成矿测年资料和地球动力学研究进展,提出南岭地区大规模成矿作用出现于中晚侏罗世(165~150Ma),相应的构造背景是古太平洋板块向大陆俯冲,在大陆边缘弧后地区出现一系列NE向壳幔相互作用强烈的伸展带,这些伸展带与东西向古断裂的交汇部位是岩浆活动和成矿作用中心区,NE向十杭带与南岭中脊部EW向古深大断裂的交汇处形成湘南最大的钨锡矿集区.在中晚白垩世.古太平洋板块向NNE方向走滑,导致大陆岩石圈大面积伸展,相应大规模的火山活动主要出现在武夷山以东地区,但在包括南岭地区在内的华南地区广泛出现盆岭构造,NNE向的白垩纪红层-火山盆地与以花岗岩为代表的隆起相间分布,在一些盆地可见130~90Ma侵位的、面积不大却广泛分布的花岗岩及其锡多金属矿化,构成华南地区大规模锡多金属矿化作用,但这次成矿作用在南岭地区并不十分强烈.
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修回日期:  2007-05-15
刊出日期:  2007-10-31

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