| 廊坊地区南部第四纪晚期的海相地层及海侵问题 |
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| 引用本文： | 章红晖.廊坊地区南部第四纪晚期的海相地层及海侵问题[J].第四纪研究,1986,7(2):119-128. |
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| 作者姓名： | 章红晖 |
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| 作者单位： | 河北省地质矿产局水文地质工程地质大队 |
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| 摘 要： | 位于河北平原东部的河北省大城县、文安县, 霸县、安次县、永清县及固安县(统称廊坊地区南部), 东接天津地区, 东南与沧州地区相毗连, 距渤海湾西岸100多km(图I)。该区第四系发育, 厚度可达400-500m, 夹有数层海相、海陆过渡相层。近年来一些单位对这套地层进行了广泛地研究, 并取得了一些成果。, 一般倾向认为自晚更新世以来发育了三个海相或海陆过渡相地层, 发生过三次海侵。
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THE MARINE STRATA OF THE LATE QUATERNARY PERIOD AND THE PROBLEM OF MARINE INVASIONS IN THE SOUTH OF LANGFANG DISTRICT OF HEBEI PROVINCE |
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| Institution: | The Geological team of Hydrology and Engineering of the Geologicaland Mineral Bureau of Hebei Province |
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| Abstract: | Some scientific research units concerned have published several theses and have adiscussion on the problem how many marine transanressions have occurred to the wes-tern coast of the Bohai Gulf since Late Pleistocene. It is generally held that there werethree or four marine beds in this area as deposits resulting from the three marine tran-sgreisons. |
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