| 下切古河谷高分辨率层序地层学研究的进展 |
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| 引用本文： | 李从先,张桂甲.下切古河谷高分辨率层序地层学研究的进展[J].地球科学进展,1996,11(2):216-220. |
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| 作者姓名： | 李从先 张桂甲 |
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| 作者单位： | 同济大学海洋地质与地球物理系 |
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| 摘 要： | 基面抬升、溯源堆积、依次退积叠置是下游河段古河谷厚层连续沉积产生的关键。基于此点，对现有古河谷沉积模式和高分辨率层序地层学研究的若干问题作了讨论。
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| 关 键 词： | 下切古河谷 高分辫率层序地层学 溯源堆积 |
| 收稿时间： | 1995-04-18 |
| 修稿时间： | 1995-05-29 |
PROGRESS ON HIGH RESOLUTION SEQUENCE STRATIGRAPHY IN INCISED PALEOVALLEY |
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| Li Congxian,Zhang Guijia.PROGRESS ON HIGH RESOLUTION SEQUENCE STRATIGRAPHY IN INCISED PALEOVALLEY[J].Advance in Earth Sciences,1996,11(2):216-220. |
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| Authors: | Li Congxian Zhang Guijia |
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| Institution: | Department of Marine Geology & Geophysics, Tongji University ,Shanghai 200092 |
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| Abstract: | Retrogressive aggradation is the main cause of thick continous deposits in the lower reach of the incised paleovalley when sea-level rises.On the basis of this,this paper discusses the exisiting paleovalley sedimentary model and some problems in high-resolution sequence stratigraphy study. |
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| Keywords: | ncised valley High -resolution sequense stratigraphy Retragressive aggradation |
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