| 中国东部及邻区中新生代大陆边缘性质讨论 |
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| 引用本文： | 丘元禧, 夏亮辉. 1994. 中国东部及邻区中新生代大陆边缘性质讨论. 地质通报, (3). |
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| 作者姓名： | 丘元禧 夏亮辉 |
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| 作者单位： | 中山大学地质系 |
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| 摘 要： | 中国东部及邻区中、新生代大陆边缘的性质，国内外学者论述颇多，众说不一。作者认为它是复合型大陆边缘，其基本特征是：由多个古陆块古陆缘复合，裂解的大陆边缘与增生的大陆边缘复合，安第斯型大陆边缘与阿尔卑斯型大陆边缘复合。还探讨了这一复合型大陆边缘形成的区域构造背景和形成机制。
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THE NATURE OF MESO-CENOZOIC CONTINENTAL MARGINS IN EASTERN CHINA AND ITS ADJACENT AREAS |
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| 1994. THE NATURE OF MESO-CENOZOIC CONTINENTAL MARGINS IN EASTERN CHINA AND ITS ADJACENT AREAS. Geological Bulletin of China, (3). |
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| Abstract: | There has been much discussion about the nature of Meso-Cenozoic continental margins ineastern China and its adjacent areas but divergent views exist. The authors consider them to becompound-type continental margins. Their basic features are compounding of ancient continentalmargins of several ancient continental margin and the accretionary continental margin and com-pounding of the Andean-type continental margin and the Alpine-type continental margin. The pa-per also discusses the regional tectonic setting and formation mechanism of this compoundingtype continental margin. |
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