期刊文献+

华南与中南半岛三角洲发育特征之比较 被引量:2

The South China and Indochina Peninsula Deltas——A Comparison
下载PDF
导出
摘要 韩江、珠江、红河、湄公河、湄南河三角洲同处东亚季风热带。河流丰水少沙,径流强劲, 洪枯流量比值大,洪泛平原和湿地发育,有珊瑚礁和红树林堆积,平原推进速率较大,出海口门多,这些都是热带三角洲的特色。各三角洲的构造基础都是断陷盆地,由于断陷的幅度和时代不相同,故而第四系的厚度和年龄差异很大。受全球海平面变化的影响,末次冰期以来,各三角洲经历了相似的沉积过程,发育 3期三角洲。所处位置 (湾内或湾外)、滨外陆架坡度、海洋动力等条件,使各三角洲的地貌类型、地面高程、平原推进速率、水下三角洲、水动力类型等有较大的差异。 The five deltas of South China and Indochina Peninsula are all deposited in downfaulted basins. The downfault structure is mainly shown by the red weathering crust on the basement of the Quaternary,island hills on plain,islands off estuary,seismic activity and others.The thickness of Quaternary of Chao Phraya Delta is over 650m but that of Zhujiang Delta is only 63m, showing the different amplitude of downfaulting. The deposits of Early and Middle Pleistocene can be found in the three deltas of Indochina Peninsula but the kown oldest datings are only 52 138 a B P and 45 120 a B P in Hanjiang and Zhujiang Delta,respectively. Since middle stage of the Latest Glacial Period the five deltas have undergone three times of deltaic deposition and two times of discontinuity occurred.The maximum of Holocene transgression is mostly dated at 6 500-5 000 a B P.The advance rate of plain during the past hundred years is 63-120m/a in Zhujiang Delta but that of Chao Phraya Delta is only 4.0m/a. The similarity of the deltas can be enumerated as follows:abundant water and less silt content,composite deposits of several rivers,braided stream,several river mouths,smaller channel curvature,extensive flood plain and wetland,south-westward extending of delta plain,and sedimentary of mangrove. The deltas have following differentiation.The areas of the deltas are quite different.The altitude of plain is larger in the delta inside of estuary.The submerged delta developed in the delta with smaller shelf gradient.The hydrodynamics of the deltas can be recognized as follows:runoff-tidal type of Zhujiang Delta and Chao Phraya Delta,runoff-wave type of Hanjiang Delta and Red River Delta,and runoff-tidal-wave type of Mekong Delta.
出处 《地理科学》 CSCD 北大核心 2005年第1期56-62,共7页 Scientia Geographica Sinica
基金 国家自然科学基金资助项目(40371015)。
关键词 三角洲 华南 中南半岛 delta South China Indochina Peninsula
  • 相关文献

参考文献17

  • 1黄镇国,张伟强,陈俊鸿.中国红土与自然地带变迁[J].地理学报,1999,54(3):193-203. 被引量:27
  • 2黄镇国,张伟强,蔡福祥,徐起浩.华南末次冰期盛期最低海面问题[J].地理学报,1995,50(5):385-393. 被引量:17
  • 3陈欣树,包砺彦,陈俊仁,赵希涛.珠江口外陆架晚第四纪最低海面的发现[J].热带海洋,1990,9(4):73-77. 被引量:32
  • 4陈伟光,张虎男,张福来.珠江三角洲地区新构造运动年代学的研究[J].地震地质,1991,13(3):213-220. 被引量:17
  • 5黄镇国,张伟强,蔡福祥.珠江水下三角洲[J].地理学报,1995,50(3):206-214. 被引量:14
  • 6黄镇国 李平日 张仲英.珠江三角洲[M].广州:科学普及出版社,1982..
  • 7Nguyen K L. The seismotectonics of the Indochina Peninsula[ J ].Journal of Southeast Asian Earth Sciences,1991,6(2) :55 -61.
  • 8Mathers S. Zaiasiewicz J. Holocene sedimentary architecture of the Red River Delta, Vietnam [ J ]. Journal of Coastal Research,1999,15(2) :314-325.
  • 9Van Lap Nguyen,Thi Kim Oanh Ta,Masaaki Tateishi. Late Holocene depositional environments and coastal evolution of the Mekong River Delta, Southern Vietnam [ J ]. Journal of Asian Earth Sciences,2000,18(4) :427 -439.
  • 10Thiramonkol N. G, eomorphology of the lower central plain,Thailand [A]. In: Chulalongkom University. Proceedings of 3 rd Meeting of Working Group on Geomorphology of River and Coastal Plains [ C ]. Bangkok: Department of Geology, Chulalongkorn University, 1984. 103 - 117.

二级参考文献103

共引文献107

同被引文献41

引证文献2

二级引证文献15

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部