| 地层间断面的时间结构研究进展 |
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| 引用本文： | 吴智平,李守军,周瑶琪.地层间断面的时间结构研究进展[J].中国石油大学学报(自然科学版),1998(6). |
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| 作者姓名： | 吴智平 李守军 周瑶琪 |
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| 作者单位： | 石油大学油气资源与环境地质研究所 |
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| 基金项目： | 中国石油天然气总公司中青年创新基金 |
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| 摘 要： | 地层中的间断面代表了一段缺失（或无记录）的地质历史，不同类型的间断面通过不同类型的地层不整合面表现出来。其代表的时间结构可以分为三部分，即剥蚀掉的沉积物沉积所需的时间，剥蚀掉这些沉积物所需的时间及无沉积间断的时间。不同间断面具有不同的时间结构单元组合。文中介绍了有关剥蚀量的估算、剥蚀开始的时间及无沉积间断时间的定量研究方法，并对目前间断面研究中存在的问题进行了探讨。
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| 关 键 词： | 地层 不连续面 地质历史 时间结构 |
/ REVIEW OF THE STUDIES ON THE HIATUS SURFACES IN THE RECORDS OF STRATIGRAPHY |
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| Wu Zhiping./ REVIEW OF THE STUDIES ON THE HIATUS SURFACES IN THE RECORDS OF STRATIGRAPHY[J].Journal of China University of Petroleum,1998(6). |
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| Authors: | Wu Zhiping |
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| Institution: | Dongying: 257062 |
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| Abstract: | The hiatus surfaces in the records of stratigraphy indicate the missing of the geological history. Different hiatus surfaces are manifested by the different unconformity surfaces, and a period of time represented by a hiatus surface can be further divided into three units, including the sedimentating time of removed sediments, erosion time for removing sediments, and the time without sediments. Some quantitative means to calculate the thickness of removed sediments, the point of time for beginning erosion, and the time scale without sediments are introduced, and some questions in the studies on hiatus surfaces are discussed. |
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| Keywords: | formation discontinuity surface geologic model time units of hiatus surface |
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