王家生, 刘本培, 薛重生, 李昌年. 1999: 造山带非史密斯地层研究方法和在1:5万区调填图中的初步应用. 地质通报, 18(4): 425-430.
    引用本文: 王家生, 刘本培, 薛重生, 李昌年. 1999: 造山带非史密斯地层研究方法和在1:5万区调填图中的初步应用. 地质通报, 18(4): 425-430.
    1999: Ophiolite complex:a reconnaissance application of non Smith stratigraphic study to 1:50 000 geological mapping. Geological Bulletin of China, 18(4): 425-430.
    Citation: 1999: Ophiolite complex:a reconnaissance application of non Smith stratigraphic study to 1:50 000 geological mapping. Geological Bulletin of China, 18(4): 425-430.

    造山带非史密斯地层研究方法和在1:5万区调填图中的初步应用

    Ophiolite complex:a reconnaissance application of non Smith stratigraphic study to 1:50 000 geological mapping

    • 摘要: 根据在赣东北1∶5 万葛源幅蛇绿混杂岩区区调的实践体会,提出在区调填图中进行非史密斯地层研究的一般步骤:(1) 利用野外踏勘和前人资料,划分区内地层类型;(2) 区分岩块和基质;(3) 选择一定靶区对岩块进行成分、古生物、同位素等的细致研究,以获得年代和构造背景等信息;(4) 识别岩块、基质及与史密斯地层之间的相互接触关系,并探索其构造就位时间;(5) 重建地层序列,探讨构造演化史。

       

      Abstract: With the experience of Geyuan sheet 1∶50 000 geological mapping in the ophiolite complex in the northeast Jiangxi province,the authors put forward a proposal for non Smith stratigraphic study in geological mapping in similar areas.The study includes:(1) field reconnaissance and reinterpretation of previous data,thereafter subdivision of the stratigraphic units;(2) distinguish of adventitious rock blocks and matrixes;(3) selection of target area for detailed study of composition,paleontology and isotopes to gain data on age and tectonic setting;(4) identification of the rock blocks,matrixes and the association to non Smith stratigraphic units,and determination of timing of the tectonic emplacement;(5) re establishing stratigraphic sequence and interpreting the tectonic evolution history.

       

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