Large rivers : geomorphology and management

Large rivers : geomorphology and management
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发表时间:
2007
期刊:
The Annals of thoracic surgery
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通讯作者:
Avijit Gupta
Avijit Gupta
中科院分区:
其他
文献类型:
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作者:
Avijit Gupta

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. 吉尔伯特,G.K.(1885)湖岸的地形特征。我们青烟。测量员5、安。报告,69 - 123。吉尔伯特,G.K.(1890)《博纳维尔湖》。我们青烟。测量员Monogr。1。good, s.l., Jr .和Kuehl, S.A.(1998)孟加拉盆地洪泛平原过程和恒河-布拉马普特拉河沉积物的储存:基于Cs和Pb地质年代学的沉积研究。沉积物。青烟。科学通报,21(2),239-258。[刘志刚,Jr .,和Kuehl, S.A. .(1999)恒河-布拉马普特拉河水系全新世和现代沉积物收支:高水位向洪泛平原、陆架和深海沉积中心扩散的证据。]地质,27,559-562。[刘建平,刘建平,刘建平,等。(2000)大沉积物供应、活动构造运动和地壳运动对边缘层序发育的意义:恒河-雅鲁藏布江三角洲晚第四纪地层与演化。]沉积物。青烟。中文信息学报,133,227-248。刘建军,刘建军,刘建军,等(2006)全新世早期季风对恒河—布拉马普特拉河沉积物的影响。地质,28,1083-1086。古尔德,H.R.(1970)密西西比三角洲综合体。见:三角洲沉积:现代和古代(J.P.摩根主编)。SEPM规范。否。15,第3-30页。Harris, p.t., Baker, e.k., Cole, A.R.和Short, S.A.(1993)巴布亚湾受潮汐支配的飞河三角洲沉积的初步研究。续《货架法规》,13,441 - 472。Harris, p.t., Pattiaratchi, c.b., Keene, j.b., Dalrymple, r.w., Gardner, j.v., Baker, e.k., Cole, a.r., Mitchell, D, Gibbs, P.和Schroeder, W.W.(1996)巴布亚新几内亚湾前陆盆地晚第四纪三角洲和碳酸盐沉积:对海平面变化的响应。j .沉积物。Res. 66, 801-819。Harris, p.t., Heap, a.d., Bryce, s.m., Porter-Smith, R., Ryan, D.A.和Heggie, D.T.(2003)基于波浪、潮汐和河流动力的定量分析的澳大利亚碎屑海岸沉积环境分类。j .沉积物。Res., 72, 858-870。(2002)南宋洪三角洲的海岸变化。j . Geogr。, 111, 124-132(日文,附英文摘要)。Hayes, M.O.(1979)堰洲岛形态作为潮汐和波浪状态的函数。见:从圣劳伦斯湾到墨西哥湾的堰洲群岛(S.P.莱瑟曼主编)。学术出版社,纽约,第1-27页。(2003)大型河流三角洲的形态与沉积,地理学报。, 112, 337-359(日文,英文摘要)。郝康,齐藤英,赵强,程昌,王平,佐藤英,李超(2001a)长江三角洲全新世沉积相及沉积速率。地貌学,41,233-248。Hori, K., Saito, Y., Zhao, Q., Cheng, C., Wang, P., Sato, Y., Li, C. (2001b)末次海侵时期潮控古长江河口沉积相。3月青烟。, 177, 331-351。[堀康,齐藤永,赵强,王平(2002)长江三角洲的结构与演变。]沉积物。青烟。中文信息学报,14,249-264。Hori, K., Tanabe, S., Saito, Y., Haruyama, S., Nguyen, V.和Kitamura, A.(2004)三角洲形成与全新世海平面变化:来自越南红河三角洲的例子。沉积物。青烟。中文信息学报,164,237-249。霍维乌斯,N.(1998)大河泥沙供给的控制。见:陆相岩石中尤斯塔西、气候和构造运动的相对作用(K.W. Shanley和P.J. McCabe主编)。SEPM规范。否。59,第3-16页。
. Gilbert, G.K. (1885) The topographic features of lake shores. US Geol. Surv., 5th Ann. Rept, 69–123. Gilbert, G.K. (1890) Lake Bonneville. US Geol. Surv. Monogr. 1. Goodbred, S.L., Jr and Kuehl, S.A. (1998) Floodplain processes in the Bengal Basin and the storage of Ganges-Brahmaputra river sediment: an accretion study using Cs and Pb geochronology. Sediment. Geol., 121, 239–258. Goodbred, S.L., Jr and Kuehl, S.A. (1999) Holocene and modern sediment budgets for the Ganges-Brahmaputra River system: evidence for highstand dispersal to fl ood-plain, shelf, and deepsea depocenters. Geology, 27, 559–562. Goodbred, S.L., Jr and Kuehl, S.A. (2000a) The signifi cance of large sediment supply, active tectonism, and eustasy on margin sequence development: Late Quaternary stratigraphy and evolution of the Ganges-Brahmaputra delta. Sediment. Geol., 133, 227–248. Goodbred, S.L., Jr and Kuehl, S.A. (2000b) Enormous GangesBrahmaputra sediment discharge during the strengthened early Holocene monsoon. Geology, 28, 1083–1086. Gould, H.R. (1970) The Mississippi delta complex. In: Deltaic Sedimentation: Modern and Ancient (J.P. Morgan, Ed.). SEPM Spec. Publ. no. 15, pp. 3–30. Harris, P.T., Baker, E.K., Cole, A.R. and Short, S.A. (1993) A preliminary study of sedimentation in the tidally dominated Fly River Delta, Gulf of Papua. Cont. Shelf Res., 13, 441– 472. Harris, P.T., Pattiaratchi, C.B., Keene, J.B., Dalrymple, R.W., Gardner, J.V., Baker, E.K., Cole, A.R., Mitchell, D., Gibbs, P. and Schroeder, W.W. (1996) Late Quaternary deltaic and carbonate sedimentation in the Gulf of Papua foreland basin: response to sea-level change. J. Sediment. Res., 66, 801–819. Harris, P.T., Heap, A.D., Bryce, S.M., Porter-Smith, R., Ryan, D.A. and Heggie, D.T. (2003) Classifi cation of Australian clastic coastal depositional environments based upon a quantitative analysis of wave, tidal, and river power. J. Sediment. Res., 72, 858–870. Haruyama, S. and Phai, V.V. (2002) Coastal change in the Southern Song Hong Delta. J. Geogr., 111, 124–132 (in Japanese with English abstract). Hayes, M.O. (1979) Barrier island morphology as a function of tidal and wave regime. In: Barrier Islands from the Gulf of St Lawrence to the Gulf of Mexico (S.P. Leatherman, Ed.). Academic Press, New York, pp. 1–27. Hori, K. and Saito, Y. (2003) Morphology and sediments of large river deltas, J. Geogr., 112, 337–359 (in Japanese with English abstract). Hori, K., Saito, Y., Zhao, Q., Cheng, C., Wang, P., Sato, Y. and Li, C. (2001a) Sedimentary facies and Holocene progradation rates of the Changjiang (Yangtze) delta, China. Geomorphology, 41, 233–248. Hori, K., Saito, Y., Zhao, Q., Cheng, C., Wang, P., Sato, Y. and Li, C. (2001b) Sedimentary facies of the tide-dominated paleoChangjiang (Yangtze) estuary during the last transgression. Mar. Geol., 177, 331–351. Hori, K., Saito, Y., Zhao, Q. and Wang, P. (2002) Architecture and evolution of the tide-dominated Changjiang (Yangtze) River delta, China. Sediment. Geol., 146, 249–264. Hori, K., Tanabe, S., Saito, Y., Haruyama, S., Nguyen, V. and Kitamura, A. (2004) Delta initiation and Holocene sea-level change: example from the Song Hong (Red River) delta, Vietnam. Sediment. Geol., 164, 237–249. Hovius, N. (1998) Controls on sediment supply by large rivers. In: Relative Role of Eustasy, Climate, and Tectonism in Continental Rocks (K.W. Shanley and P.J. McCabe, Eds.). SEPM Spec. Publ. no. 59, pp. 3–16.