下寒武统大林子组溶解蒸发岩系旋回层序及渗流构造成因
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  • 中文刊名:科学通报
  • 英文刊名:Chinese Science Bulletin
  • 作者:孟祥化 ; 葛铭 ; 旷红伟 ; 刘燕学 ; 蔡国印
  • 出版日期:2002-07-30
  • 机构:中国地质大学沉积盆地研究所,中国地质大学沉积盆地研究所,中国地质大学沉积盆地研究所,中国地质大学沉积盆地研究所,中国矿业大学资源系 北京 100083 ,北京 100083 ,北京 100083 ,北京 100083 ,北京 100083
  • 年:2002
  • 期:14
  • 出版单位:科学通报
摘要
<正>《科学通报》第44卷第16期发表了《华北中新元古代及早古生代地震灾变事件及与Rodinia的关系》[1]一文(以下简称《华北》),涉及辽宁大连下寒武统大林子组的成因问题.我们曾先后于1984~1986,1993~1995和2001年对该组地层进行过详细的旋回层序、微层序和岩石学及微组构成因研究,对大林子组中段溶解蒸发岩系进行了几至几十厘米的超微层单元逐层观测取样,进行室内显微岩石组构和化学组分分析.本文按层序、岩石组构分析和比较
引文
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