| 海平面变化、黄河改道与贝壳堤发育关系的探讨 |
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| 引用本文： | 贾艳杰. 海平面变化、黄河改道与贝壳堤发育关系的探讨[J]. 陕西师范大学学报(自然科学版), 1995, 0(Z1) |
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| 作者姓名： | 贾艳杰 |
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| 作者单位： | 天津师范大学地理学系 |
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| 摘 要： | 全新世海侵高峰过后，海平面一直处于幅度不大（约１ｍ左右）的振荡运动状态．对应四次小高海面时期，天津滨海平原上堆积了四道贝壳堤，黄河在本区入海，使贝壳堤的组成发生了变化．
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| 关 键 词： | 小高海面；黄河；河口沉积；贝壳堤 |
Correlation among relative sea-level change and Huanghe river changing channel and chenier development |
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| Jia Yanjie. Correlation among relative sea-level change and Huanghe river changing channel and chenier development[J]. Journal of Shaanxi Normal University: Nat Sci Ed, 1995, 0(Z1) |
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| Authors: | Jia Yanjie |
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| Abstract: | Research has revealed that the relative sea-level has been continuously in the state of oscillation with an amplitude of approximately 1 m, since the highist sea--level of Holocene passed. Corresponding to four the micro-high sea-level phases, four cheniers were accumulated on Tianjin coastal plain respectively in the last 5000 years. The rapid deposition in the estuary area of Huanghe river resulted in less sorts of sea-leve which made up cheniers. |
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| Keywords: | micro-high sea-level Huanghe river estuary deposits cheniers |
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