戴元裕.江西省新余太平山铁矿区叠加褶皱构造解析并论恢复复杂褶皱系的包络面的意义[J].地质找矿论丛,1986,(2):13-22
江西省新余太平山铁矿区叠加褶皱构造解析并论恢复复杂褶皱系的包络面的意义
A STRUCTURAL ANALYSIS OF SUPER IMPOSED FOLDS AT TAIPINGSHAN IRON MINE, XINYU COUNTY, JIANGXI PROVINCE, AND THE SIGNIFICANCE OF RECONSTRUCTING ENVELOPES IN THE COMPLICATED FOLD SYSTEM
  
DOI:10.6053/j.issn.1001-1412.1986.2. 002
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戴元裕 江西省吉安地区地质队 
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中文摘要:
      太平山铁矿区是江西新余铁矿田之一段,整个矿田呈近东西走向展布,东起芳洲,西至枫树下,长约60公里.矿田总体构造为一褶轴向西倾伏,轴面向北倾斜的倒转背斜(神山背斜).该背斜南翼保存完整,而北翼仅在倾伏端处残存.
英文摘要:
      The iron ore horizons and associated stratigraphic units of the studied mine have undergone multiphasic folded deformation.This paper presents a result of structural analysis in the aspect of folded sequence features,the superimposed relations and development mechanism of folds,the regularities of structural deformation and its application in exploration,based on the huge amount of field data.The significance of reconstructing envelopes in the complicated fold system with some concrete examples of using envelopes to judge large strutures,discriminate stratigraphic sequences,conduct geological mapping and assign drilling holes are also discussed.
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