STUDIES ON THE MESOZOIC MARGINAL ARC SYSTEM OF THE SOUTHEAST COAST AND TAIWAN IN CHINA  

作　　者：曹荣龙 朱寿华 

机构地区：[1]Institute of Geochemistry, Academia Sinica, Guiyang 550002, PRC

出　　处：《Science China Chemistry》1990年第8期980-992,共13页中国科学（化学英文版）

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.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.

关 键 词：passive MARGIN island ARE MARGINAL ARE recycling paired metamorphie BELTS 

分 类 号：O6[理学—化学]