南黄海南部陆区全新世沉积研究

陈报章; 李从先; 业治铮

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南黄海南部陆区全新世沉积研究

陈报章, 李从先, 业治铮

文章导航 > 沉积学报 > 1994 > 12(2): 63-71

陈报章, 李从先, 业治铮. 南黄海南部陆区全新世沉积研究[J]. 沉积学报, 1994, 12(2): 63-71.

引用本文:

陈报章, 李从先, 业治铮. 南黄海南部陆区全新世沉积研究[J]. 沉积学报, 1994, 12(2): 63-71.

Chen Baozhang, Li Congxian, Ye Zhizheng. The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land[J]. Acta Sedimentologica Sinica, 1994, 12(2): 63-71.

Citation:

Chen Baozhang, Li Congxian, Ye Zhizheng. The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land[J]. Acta Sedimentologica Sinica, 1994, 12(2): 63-71.

陈报章, 李从先, 业治铮. 南黄海南部陆区全新世沉积研究[J]. 沉积学报, 1994, 12(2): 63-71.

引用本文:

陈报章, 李从先, 业治铮. 南黄海南部陆区全新世沉积研究[J]. 沉积学报, 1994, 12(2): 63-71.

Chen Baozhang, Li Congxian, Ye Zhizheng. The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land[J]. Acta Sedimentologica Sinica, 1994, 12(2): 63-71.

Citation:

Chen Baozhang, Li Congxian, Ye Zhizheng. The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land[J]. Acta Sedimentologica Sinica, 1994, 12(2): 63-71.

南黄海南部陆区全新世沉积研究

1 徐州师范学院区域开发研究所;
2 同济大学海洋地质研究所

详细信息

作者简介:
陈报章男 29岁硕士讲师沉积学及第四纪地质学土壤地理学

中图分类号: P736.21

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文章访问数: 567
HTML全文浏览量: 18
PDF下载量: 356
被引次数: 0

The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land

1 Regional Development Institute of Xuzhou Normal college, Xuzhou;
2 Department of Marine Geology of Tongji University, Shanghai

摘要

摘要: 研究区全新统不整合超覆于上更新亚统之上,自下而上由滨海相(局部含河口海湾相)?近岸浅海相(潮成沙体相)和潮滩相构成?全新统海侵层主要受控于晚更新世末SE→NW逐渐抬高的掀斜状古地形,表现出明显的水平相交,可归纳为四种层序类型?本文通过钻孔剖面分析对比,揭示了研究区垂向相序演替和水平相变的规律及其二者间的关系,恢复了全新世沉积演化过程?
- 全新统 /
- 海侵层 /
- 层序类型 /
- 水平相变 /
- 沉积演化
Abstract: The author discussed the Holocene sedimentary facies and its evolution,based mainly upon data of the eight drill-holes and also upon other several dozens of reference drill-holes, as well as the field investigation of the buried tidal sand bodies in the studied area for the first time. Characteristics of the sediments in the cores have been studied about their textures, structures,minerals and macrofossils. Radiometric dating ¹⁴C carried out for the important levels. It is non-marine facies of Pleistocene that underlay the sediment of Holocene with unconformity between them: The topography of the area at the end of Pleistocene inclined from northwest towards southeast which influenced the Holocene transgression obviously. The Holocene sedimentary sequence can be divided into the lower transgressive and the upper regressive one, consisting of beach facies(contains estuary-bay in sbme part of the area),near- shore neritic facies(tidal sand body facies)and tidal flat facies etc. It is obvious that facies change horizontally. In different environment appear different sedimentary sequences. The sequence can be classified into four types,which were discussed加detail in this paper. For all the four types,the best developed area is in the southeast part of the studied area, and the worst is in the northwest. The buried tidal sand bodies can be crassified into three types:Ⅰ)near-shore tidal sand bars;Ⅱ)tidal sand waves ;Ⅲnear-shore tidal sand ridges. They were formed and preserved successively along with the cycle of transgression and regression,and their distribution pattern was controlled by shift of the Changjiang river towards southeast during the Holocene.

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参考文献(15)

[1]	李成治，李本川，lssl，海洋与湖沼，(4):311~331.
[2]	周长振，孙家松，1981，海洋地质研究，(1):83~91.
[3]	杨长恕,1985，海洋地质与第四纪地质，(3):35~94,
[4]	杨子赓等，1985，海洋地质与第四纪地质，(4):23~32,
[5]	郑光房,1989，南黄海第四纪层型地层对比，科学出版社。
[6]	许世远等，1987，长江三角洲现代沉积研究，华东师范大学出版社，97~106,
[7]	赵松龄等，1991，海洋地质与第四纪地质，(3):105 ~112。
[8]	陈报章等,1991，海洋地质与第四纪地质，(2):37~96.
[9]	Reading, H. D. (0d)，1978, Blackwell Scientific Publication,p. 259~336.
[10]	Stride, A. H.，1982, Offshore tidal sands processes and deposits, Chapan and Hall Lid, London, New York, p.380~920.
[11]	Caston, V. N. D.，1972, Linear sand banks in the southern North Sea, Sedimentology, Vol. 18, No. 1，P.63~78.
[12]	Belderson, R. H.，Stride, A. H.，1966, Mar. Geol.，Vol. 4, No. 4，p. 237~257.
[13]	Kenyon, N. H.，1970, Mar. Geol.，Vol. 8, No. 1，p. 25~39.
[14]	Off, T.，1963,人m. Assoc. Pat. Geol. Bull, Vo1.47，No. 2, p. 329~337.
[15]	Swift, D. J. P.，1975, Mar. Geol.，Vol. 13, No. 2, p. 105~134.

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南黄海南部陆区全新世沉积研究

1 徐州师范学院区域开发研究所;

2 同济大学海洋地质研究所

作者简介:
陈报章男 29岁硕士讲师沉积学及第四纪地质学土壤地理学

刊出日期: 1994-06-10

中图分类号: P736.21

关键词:

全新统 /

海侵层 /

层序类型 /

水平相变 /

沉积演化

摘要: 研究区全新统不整合超覆于上更新亚统之上,自下而上由滨海相(局部含河口海湾相)?近岸浅海相(潮成沙体相)和潮滩相构成?全新统海侵层主要受控于晚更新世末SE→NW逐渐抬高的掀斜状古地形,表现出明显的水平相交,可归纳为四种层序类型?本文通过钻孔剖面分析对比,揭示了研究区垂向相序演替和水平相变的规律及其二者间的关系,恢复了全新世沉积演化过程?

English Abstract

The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land

1 Regional Development Institute of Xuzhou Normal college, Xuzhou;

2 Department of Marine Geology of Tongji University, Shanghai

Publish Date: 1994-06-10

Abstract: The author discussed the Holocene sedimentary facies and its evolution,based mainly upon data of the eight drill-holes and also upon other several dozens of reference drill-holes, as well as the field investigation of the buried tidal sand bodies in the studied area for the first time. Characteristics of the sediments in the cores have been studied about their textures, structures,minerals and macrofossils. Radiometric dating ¹⁴C carried out for the important levels. It is non-marine facies of Pleistocene that underlay the sediment of Holocene with unconformity between them: The topography of the area at the end of Pleistocene inclined from northwest towards southeast which influenced the Holocene transgression obviously. The Holocene sedimentary sequence can be divided into the lower transgressive and the upper regressive one, consisting of beach facies(contains estuary-bay in sbme part of the area),near- shore neritic facies(tidal sand body facies)and tidal flat facies etc. It is obvious that facies change horizontally. In different environment appear different sedimentary sequences. The sequence can be classified into four types,which were discussed加detail in this paper. For all the four types,the best developed area is in the southeast part of the studied area, and the worst is in the northwest. The buried tidal sand bodies can be crassified into three types:Ⅰ)near-shore tidal sand bars;Ⅱ)tidal sand waves ;Ⅲnear-shore tidal sand ridges. They were formed and preserved successively along with the cycle of transgression and regression,and their distribution pattern was controlled by shift of the Changjiang river towards southeast during the Holocene.

陈报章, 李从先, 业治铮. 南黄海南部陆区全新世沉积研究[J]. 沉积学报, 1994, 12(2): 63-71.

引用本文:

陈报章, 李从先, 业治铮. 南黄海南部陆区全新世沉积研究[J]. 沉积学报, 1994, 12(2): 63-71.

Chen Baozhang, Li Congxian, Ye Zhizheng. The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land[J]. Acta Sedimentologica Sinica, 1994, 12(2): 63-71.

Citation:

Chen Baozhang, Li Congxian, Ye Zhizheng. The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land[J]. Acta Sedimentologica Sinica, 1994, 12(2): 63-71.

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南黄海南部陆区全新世沉积研究

作者简介:
陈报章男 29岁硕士讲师沉积学及第四纪地质学土壤地理学

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The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land

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目录

南黄海南部陆区全新世沉积研究

1 徐州师范学院区域开发研究所;

2 同济大学海洋地质研究所

作者简介:
陈报章男 29岁硕士讲师沉积学及第四纪地质学土壤地理学

English Abstract

The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land

1 Regional Development Institute of Xuzhou Normal college, Xuzhou;

2 Department of Marine Geology of Tongji University, Shanghai

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南黄海南部陆区全新世沉积研究

作者简介: 陈报章 男 29岁 硕士讲师 沉积学及第四纪地质学 土壤地理学

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The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land

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出版历程

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南黄海南部陆区全新世沉积研究

1 徐州师范学院区域开发研究所; 2 同济大学海洋地质研究所

作者简介: 陈报章 男 29岁 硕士讲师 沉积学及第四纪地质学 土壤地理学

English Abstract

The Study on Holocene Sedimentation in the Southern South Hnanghai Sea Coastal Land

1 Regional Development Institute of Xuzhou Normal college, Xuzhou; 2 Department of Marine Geology of Tongji University, Shanghai

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
陈报章男 29岁硕士讲师沉积学及第四纪地质学土壤地理学

1 徐州师范学院区域开发研究所;

2 同济大学海洋地质研究所

作者简介:
陈报章男 29岁硕士讲师沉积学及第四纪地质学土壤地理学

1 Regional Development Institute of Xuzhou Normal college, Xuzhou;

2 Department of Marine Geology of Tongji University, Shanghai