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PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES

崔斗烈, 董东

崔斗烈, 董东. 1991: PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES. 地质通报, (2): 126+12.
引用本文: 崔斗烈, 董东. 1991: PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES. 地质通报, (2): 126+12.
CUI Dou-lie, DONG Dong. 1991: PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES. Geological Bulletin of China, (2): 126+12.
Citation: CUI Dou-lie, DONG Dong. 1991: PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES. Geological Bulletin of China, (2): 126+12.

PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES

PROGRESSIVE TRANSFORMATION——THE THIBD MODE OF CLOSURE OF GEOSYNCLINES

  • 摘要: 笔者认为吉林省北部吉黑褶皱系,是属地槽封闭的第三种型式——递进式转化。本文就其基本特征进行了简述。
    Abstract: The author hold that the mode of closure of the Variscan geosyncline in northern Jilin is neither sudden transformation nor gradual transformation but progressive transformation.The Jilin-Heilongjiang fold system is composed of the Caledonian, Early variscan and Early Indosinian tectonic layers, covered by the platform-type sedimentary cover, formed in the stage of rejuvenation of the peripacific continental margins (unconformably again), which is just the manifestation of the third mode of closure of geosynclines. This paper briefly describes its basic characteristics.
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出版历程
  • 网络出版日期:  2023-08-17
  • 发布日期:  1991-05-14

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