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福建福鼎石炭系及其构造环境

吴歧, 李希敏, 吴小林, 郑云钦

吴歧, 李希敏, 吴小林, 郑云钦. 1990: 福建福鼎石炭系及其构造环境. 地质通报, (4): 327-333+377. DOI: 10.12097/gbc.ZQYD199004004
引用本文: 吴歧, 李希敏, 吴小林, 郑云钦. 1990: 福建福鼎石炭系及其构造环境. 地质通报, (4): 327-333+377. DOI: 10.12097/gbc.ZQYD199004004
WU Qi, LI Xi-min, WU Xiao-lin, ZHENG Yun-qin. 1990: THE CARBONIFEROUS SYSTEM OF FUDING, FUJIAN PROVINCE, AND ITS TECTONIC SETTING. Geological Bulletin of China, (4): 327-333+377. DOI: 10.12097/gbc.ZQYD199004004
Citation: WU Qi, LI Xi-min, WU Xiao-lin, ZHENG Yun-qin. 1990: THE CARBONIFEROUS SYSTEM OF FUDING, FUJIAN PROVINCE, AND ITS TECTONIC SETTING. Geological Bulletin of China, (4): 327-333+377. DOI: 10.12097/gbc.ZQYD199004004

福建福鼎石炭系及其构造环境

THE CARBONIFEROUS SYSTEM OF FUDING, FUJIAN PROVINCE, AND ITS TECTONIC SETTING

  • 摘要: 南溪石炭系是研究东南沿海中生代火山岩基底的关键地点,笔者对该地区石炭纪的岩石地层,生物地层及岩相和沉积环境作了详细分析,提出了并非海西地槽产物,而是地层异地体的看法。
    Abstract: The Carboniferous System of Nanxi is a key window for the study of the Mesozoic volcanic rocks along the coasts of southeastern China. Through a detailed analysis of the Carboniferous stratigraphy, biostratigraphy, lithofacies and sedimentary environment of the area, the authors suggest that the Carboniferous is not the product of the Hercynian geosyncline but an allochthon.
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出版历程
  • 网络出版日期:  2023-08-17
  • 发布日期:  1990-11-14

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