| STUDIES ON THE MESOZOIC MARGINAL ARC SYSTEM OF THE SOUTHEAST COAST AND TAIWAN IN CHINA |
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| 引用本文： | 曹荣龙,朱寿华. STUDIES ON THE MESOZOIC MARGINAL ARC SYSTEM OF THE SOUTHEAST COAST AND TAIWAN IN CHINA[J]. 中国科学B辑(英文版), 1990, 0(8) |
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| 作者姓名： | 曹荣龙 朱寿华 |
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| 作者单位： | Institute of Geochemistry，Academia Sinica，Guiyang 550002，PRC，Institute of Geochemistry，Academia Sinica，Guiyang 550002，PRC |
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| 摘 要： | The southeast coastal Zhejiang, Fujian, Guangdong provinces and Taiwan in China comprised an important area in ancient Asia where the Yenshanian continental margin magmatic arc well developed in the late Mesozoic time. It is believed that the oceanic trench and subduction zone are situated on the east side of the Central Range in Taiwan. It seems unlikely that the so-called Hercynian-Indosinian ancient island arc folded system would have occurred in this region.
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STUDIES ON THE MESOZOIC MARGINAL ARC SYSTEM OF THE SOUTHEAST COAST AND TAIWAN IN CHINA |
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| CAO RONG-LONG ZHU SHOU-HUA. STUDIES ON THE MESOZOIC MARGINAL ARC SYSTEM OF THE SOUTHEAST COAST AND TAIWAN IN CHINA[J]. Science in China(Chemistry), 1990, 0(8) |
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| Authors: | CAO RONG-LONG ZHU SHOU-HUA |
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| Abstract: | The southeast coastal Zhejiang, Fujian, Guangdong provinces and Taiwan in China comprised an important area in ancient Asia where the Yenshanian continental margin magmatic arc well developed in the late Mesozoic time. It is believed that the oceanic trench and subduction zone are situated on the east side of the Central Range in Taiwan. It seems unlikely that the so-called Hercynian-Indosinian ancient island arc folded system would have occurred in this region. |
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| Keywords: | passive margin island are marginal are recycling paired metamorphie belts |
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