| 台西盆地新生代构造的演化 |
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| 引用本文： | 钟建强,黄慈流,詹文欢,古森昌,刘海龄,刘帝光. 台西盆地新生代构造的演化[J]. 海洋与湖沼, 1996, 27(3): 271-278 |
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| 作者姓名： | 钟建强 黄慈流 詹文欢 古森昌 刘海龄 刘帝光 |
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| 作者单位： | 中国科学院南海海洋研究所!广州，510301，中国科学院南海海洋研究所!广州，510301，中国科学院南海海洋研究所!广州，510301，中国科学院南海海洋研究所!广州，510301，中国科学院南海海洋研究所!广州，510301，中国科学院南海海洋研究所!广州，510301 |
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| 基金项目： | 福建省科委重点基金!41204I1 |
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| 摘 要： | 于１９８６－１９９１年，应用地震地质方法，对台湾海峡的地震地层和地质构造进行调查，采用地震剖面资料，结合区域地质特征，对台西盆地的构造演估进行研究，认为该盆地由厦澎坳陷，乌丘屿坳陷，新竹坳陷和台湾坳陷等组成，其构造演化经历了中生代末－中始新世初始张裂，晚始新世一渐新世全面断裂，中新世构造调整，以及中新世末以来挤压－收缩－封闭等阶段，现今已成为残留陆缘裂谷盆地，是陆缘裂谷从产生到衰亡的一个典型实例。
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| 关 键 词： | 构造演化 陆缘裂谷 新生代 台西盆地 |
| 收稿时间： | 1993-05-24 |
| 修稿时间： | 1995-12-05 |
CENOZOIC TECTONIC EVOLUTION IN TAIXI BASIN |
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| Zhong Jianqiang,Huang Ciliu,Zhan Wenhuan,Gu Senchang,Liu Hailing and Liu Diguang. CENOZOIC TECTONIC EVOLUTION IN TAIXI BASIN[J]. Oceanologia Et Limnologia Sinica, 1996, 27(3): 271-278 |
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| Authors: | Zhong Jianqiang Huang Ciliu Zhan Wenhuan Gu Senchang Liu Hailing Liu Diguang |
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| Affiliation: | South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301;South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301 |
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| Abstract: | Seismic stratigraphy and geology structure in Taiwan Strait were re-searched in 1986-1991 by using the method of seismic geology. The tectonic evolu-tion of Taiki Basin is studied in this paper by utilizing the information of seismicprofiles and combining with the regional gCologic characters. It is suggested that Taikihasin is composed of Xiapeng Depression, Wuqiuyu Depression, Xinzhu Depressionand Taiwan Depression, and so on. Its tectonic evolution had undergone four stapes,that is, first spreading stage in the end of Mesozoic - Middle Eocene; secondspreading stage in Inte Eocene- Oligocene; tectonic readjustment stage in Miocene;and compression- closed stage since the end of Mierene. It has become a remainedcontinelltal rift basin now, and is a typical example of continental rift. fromgenrating to dying. |
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| Keywords: | Tectonic evolution Continental rift Cenozoic Taixi Basin |
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