| 江西广丰地区中奥陶统层序地层分析 |
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| 引用本文： | 李晓勇. 江西广丰地区中奥陶统层序地层分析[J]. 江西地质, 1997, 11(2): 20-24 |
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| 作者姓名： | 李晓勇 |
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| 作者单位： | 江西地质矿产勘查开发局地矿调研大队 |
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| 摘 要： | 本文通过对广丰县周家坞中奥陶统露头剖面层序、体系域、副层序的研究，识别出了三个不同性质的Ⅱ型层序界面和二个三级层序，确认这三个层序界面为符合实际又易于野外识别的自然界面，并对ＳＱ２中反映最大海泛期的高分辨异旋回驱动机制事件，提出可能受米兰柯维奇频率的春分点和秋分点间约２万年间隔的控制。
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| 关 键 词： | 层序地层 高频旋回 中奥陶统 江西广丰 |
AN ANALYSIS ON MIDDLE ORDOVICIAN STRATIGRAPHIC SEQUENCES IN GUANGFENG |
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| Li Xiaoyong. AN ANALYSIS ON MIDDLE ORDOVICIAN STRATIGRAPHIC SEQUENCES IN GUANGFENG[J]. Jiangxi Geology, 1997, 11(2): 20-24 |
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| Authors: | Li Xiaoyong |
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| Abstract: | Through a study on sequence stratigraphy,system domain and parastrata sequence of the Middle Ordovician outcrop profile in Zhoujiawu, Guangfeng County,three IItype sequence interfaces with different properties and two III-grade sequences were distinguished. These interfaces are real natural ones and are readily reognizable in the field. |
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| Keywords: | Sequence stratigraphy high frequency cycle the Mid-Ordovician Guangfeng Jiangxi |
| 本文献已被 CNKI 维普 等数据库收录！ |
