Titlebook: Sea-Level Rise and Coastal Subsidence: Causes, Consequences, and Strategies; John D. Milliman,Bilal U. Haq Book 1996 Springer Science+Busi

Pander

生锈

古代

Subsidence of the Ganges—Brahmaputra Delta of Bangladesh and Associated Drainage, Sedimentation and ing as a result of isostatic adjustment of the crust due to rise of the Himalayas and dewatering of the Proto-Bengal Fan sediments which is now buried under thick Mio-Pliocene-Pleistocene deltaic sediments. Well-log data from northwest of Dhaka indicates that at least a part of the basin is subsidin

archaeology

Tectonic, Eustatic and Isostatic Changes along the Indian Coastm Australia and Antarctica, rifting and drifting between India and Madagascar along the west coast, and collision of the plate with the Asian continent. Following these tectonic events, eustastic changes have played a major role in modifying the east and west coasts of India. Another factor responsi

束缚

Effect of Sea-Level Rise and Human Activity on the Yangtze Delta, Chinahe world. The low-lying delta includes a considerable amount of reclaimed lands with elevations less than 2 m above mean sea level. Natural rates of subsidence throughout the delta appear to be less than 5 mm/year, but locally rates have exceeded 100 mm/year where groundwater pumping has been excess

SKIFF

Angioplasty

和平

极肥胖

Subsidence, Sea-Level Rise, and Wetland Loss in the Lower Mississippi River Deltaana. Sites of deltaic sedimentation have shifted, sea level has risen and fallen by more than 100 m, and sequences of preserved deltas have been vertically stacked in the geologic record. This paper summarizes, in the form of a case history, recent changes in the modern Mississippi River Delta with

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