线状沙脊形成与维持机制的研究

doi:10.11867/j.issn.1001-8166.1998.01.0022

地球科学进展 ›› 1998, Vol. 13 ›› Issue (1): 22 -26. doi: 10.11867/j.issn.1001-8166.1998.01.0022

线状沙脊形成与维持机制的研究

朱玉荣

同济大学海洋地质与地球物理系上海 200092

收稿日期:1997-02-03 修回日期:1997-06-02 出版日期:1998-02-01
通讯作者: 朱玉荣
基金资助:
国家自然科学基金项目“苏北近代潮成砂体的沉积过程和陆海相互作用”( 项目编号: 49476380) 资助.

STUDIES ON MECHANISM OF FORMATION AND MAINTENANCE OF LINEAR SAND RIDGES

Zhu Yurong

Department of Marine Geology and Geophysics, Tongji University, Shanghai 200092

Received:1997-02-03 Revised:1997-06-02 Online:1998-02-01 Published:1998-02-01

下载PDF ( 710 )

线状沙脊广泛分布于世界潮控陆架，对于油气勘探、航运、海岸及海洋工程施工等均具有重要意义。在介绍国外较有影响的６种线状沙脊形成与维持机制的概念和理论模式的基础上，对我国辽东浅滩线状沙脊的形成机制作了探讨。

关键词: 陆架, 线状沙脊, 形成与维持机制

Linear sand ridges, occurring extensively on continental shelves, have been studied all over the world because of their great significance in exploration of oil and gas, shipping, and construction of coastal and marine engineering, et al. Introduces six kinds of mechanism of formation and maintenance of linear sand ridges which are well known abroad, and simply analyses the formation mechanism of those linear sand ridges in eastern Bohai Sea.

Key words: Continental shelf, Linear sand ridge, Mechanism of formation and maintenace.

中图分类号:

P737.1

[1] Off T. Rhythmic linear sand bodies caused by tidal currents. Bulletin of AAPG, 1963,47(2):324-341.
[2] Caston V N D, Stride A H. Tidals and movement between some linear sand banks in the North Sea off northeast Norfolk.Marine Geology,1970,9:M38-M42.
[3] Caston G F. Potential gain and loss of sand by some sand banks in the southern North Sea off northeast Norfolk. Marine Geology,1981,41:239-250.
[4] Swift D J P. Tidal sand ridges and shoal-retreat massifts. Marine Geology, 1975, 18:105-134.
[5] Swift D J P, Field M E. Evolution of a classic sand ridges field: Maryland sector,North American inner shelf. Sedimentology, 1981, 28:461-482.
[6] Amos G L, King E L. Bedforms of the Canadian Eastern seaboard: a comparison with global occurrences. Marine Geology, 1984, 57:167-208.
[7] Parker G, Lanfredi N W , Swift D J P. Seafloor response to flow in southern Hemisphere and ridge field: A rgentine Inner shelf. Sedimentary Geology, 1982, 33:195-216.
[8] Harris P T,Pattiaratchi C B,Cole A R,et al. Evolution of subtidal sandbanks in Moreton Bay,eastern Australia.Marine Geology, 1992, 103: 225-247.
[9] 刘振夏, 夏东兴. 潮流脊的初步研究. 海洋与湖沼, 1983, 14(3): 286-295.
[10] 夏东兴, 刘振夏. 潮流脊的形成机制和发育条件. 海洋学报, 1984, 6(3): 361-367.
[11] 汤毓祥, 姚兰芳, 刘振夏. 辽东浅滩海域潮流运动特征及其与潮流脊发育的关系. 黄渤海海洋, 1993, 11(4), 9-16.
[12] 汤毓祥, 刘振夏, 姚兰芳. 渤海M₂潮流及其与辽东浅滩潮流脊发育的关系. 海洋通报, 1994, 13(1): 25-29.
[13] 刘振夏, 夏东兴, 汤毓祥, 等. 渤海东部全新世潮流沉积体系. 中国科学(B辑), 1994,24(12):1331-1338.
[14] 刘振夏, 夏东兴. 潮流沙脊的水力学问题探讨. 黄渤海海洋, 1995, 13(4): 23-28.
[15] 刘振夏. 中国陆架潮流沉积研究新进展. 地球科学进展, 1996, 11(4): 414-416.
[16] Houbolt J J H C. Recent sediment in the southern bight of the North Sea. Geologie Mijnbouw, 1968, 47:245-273.
[17] Swift D J P, Duane D B, Mckinney T F. Ridge and swale topography of the middle Atlantic Bight, north America. Marine Geology, 1973, 15:227-247.
[18] McCave I N. Tidal currents at the North Hinder light ship, southern North Sea: Flow direct ions and tubulence in relation to maintenance of sand banks. Marine Geology, 1979, 31:101-117.
[19] Soulsby R L. Measurements of the Reynolds stress components close to a marine sandbanks. Marine Geology, 1981, 31:101-114.
[20] Howarth M J, Huthnance J M. Tidal and residual circulation around a Norfolk sandbank. Esturarine and Coastal Shelf Science, 1984, 19:105-117.
[21] Smith J D. Geomorphology of a sand ridge. Journal of Geology, 1969, 77: 39-55.
[22] Belderson R H, Johnson M A, Kenyon N H. Bedforms. In: Stride A H, ed. Offshore tidal sands: processes and deposits. London: Chapman and Hall, 1982. 27-57.
[23] Johns B. Physical oceanography of coastal and shelf seas . New York: Elsevier, 1983. 321-386.
[24] Huthnance J M. On one mechanism forming linear sandbanks. Estuarine and Coastal Shelf Science, 1982a, 14:79-99.
[25] Huthnance J M. On the formation of sandbanks of finite extent. Estuarine and Coastal Shelf Science, 1982b, 15:277-299.
[26] Pattiaratchi C B, Collins M B. Mechanisms for linear sandbank formation and maintenance in relation to dynamical oceanographic observations. Prog Oceanog, 1987,19:117-176.
[27] Collins M B, Shimwell S J, Gao S,et al.Water and sediment movement in the vicinity of linear sandbanks:the Norfolk Banks, Southern North Sea. Marine Geology, 1995, 123:125-142.
[28] 刘振夏, 汤毓祥, 王揆洋, 等. 渤海东部潮流动力地貌特征. 黄渤海海洋, 1996, 14(1): 7-20.
[29] 方国洪, 杨景飞. 渤海潮运动的一个二维数值模型. 海洋与湖沼, 1985, 16(5): 337-345.

[1]	胡利民,石学法,叶君,张钰莹. 北极东西伯利亚陆架沉积有机碳的源汇过程研究进展[J]. 地球科学进展, 2020, 35(10): 1073-1086.
[2]	孙湫词, 方银霞, 李家彪. 大陆架划界科学技术及其在海上丝路合作中的应用前景分析 ^*[J]. 地球科学进展, 2018, 33(12): 1215-1222.
[3]	李丽, 徐沁. 上新世以来巽他陆架海平面变化研究[J]. 地球科学进展, 2017, 32(11): 1126-1136.
[4]	贺娟. 氢氧同位素记录揭示的巽他陆架末次冰期以来古降水量变化[J]. 地球科学进展, 2017, 32(11): 1137-1146.
[5]	戴璐. 末次冰期时暴露的巽他大陆架可能被热带稀树草原覆盖吗?[J]. 地球科学进展, 2017, 32(11): 1147-1156.
[6]	贾国东. 冰期出露的巽他陆架:重要的陆地碳储库?[J]. 地球科学进展, 2017, 32(11): 1157-1162.
[7]	黄文星, 朱本铎, 刘丽强, 张金鹏. 海底地理实体命名对大陆架划界的影响——以日本为例[J]. 地球科学进展, 2016, 31(8): 811-819.
[8]	卢汐, 宋金明, 袁华茂, 李宁. 黑潮与毗邻陆架海域的碳交换[J]. 地球科学进展, 2015, 30(2): 214-225.
[9]	韦钦胜，王辉武，葛人峰，王保栋. 南黄海悬浮体的垂直分布特性及其指示意义[J]. 地球科学进展, 2013, 28(3): 374-390.
[10]	韦钦胜,吕新刚,王宗兴,王守强,臧家业. 黄海陆架锋特征及其生态效应的初步分析[J]. 地球科学进展, 2010, 25(4): 435-443.
[11]	何家雄,施小斌,夏斌,刘海龄,阎贫,姚永坚,张树林. 南海北部边缘盆地油气勘探现状与深水油气资源前景[J]. 地球科学进展, 2007, 22(3): 261-270.
[12]	吴德星,兰健. 中国东部陆架边缘海海洋物理环境演变及其环境效应[J]. 地球科学进展, 2006, 21(7): 667-672.
[13]	郭朴,方文东,于红兵. 近海陆架区内潮观测研究进展[J]. 地球科学进展, 2006, 21(6): 617-624.
[14]	王晓梅;孙湘君. 南海巽他陆架末次冰期以来的孢粉记录初步研究[J]. 地球科学进展, 2005, 20(8): 833-839.
[15]	范德江,杨作升,郭志刚. 中国陆架 ²¹⁰Pb测年应用现状与思考[J]. 地球科学进展, 2000, 15(3): 297-302.

阅读次数

全文

摘要