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- W2384695219 abstract "there are five terraces along the coast of South China at the level of60—80m,35—45m.20—25m,8—12m and 3—5m.that means a series ofemergences in South China Coast during the Quarternary period.But there are also many evidences of submergence in South ChinaCoast,for example,some crusts of weathering,some marks of neolithic age,and some peat deposits have been found under the marine deposit,and riasof coastal type are common.the author considers that a transgression of early Pleistocene age mightexist,before the 60—80m terrace was built.Then the regression tookplace,and a series of terraces(60—80m,35—45m,20—25m,8—12m)were built,at the sealevel of correspondent heights.Afterward two transgre-ssions came again;one might occur in early Holocene,and 3—5m terracewas formed (The vibration in this epoch was about 50m);another might heat the end of neolithic age (its vibration was only on a small scale).After the neolithic age,South China Coast appears emergent up to therecent time.Only local region is submerged due to earthquake and others.The emergence and submergence in the South China coastal regionmay be the result of advance and retreat of glaciers,the warping on thecoastal region and the subsidence of the ocean bottom.It is very difficultto explain,if only one of the factors is considered.But for the Quarternary,the subsidence of the ocean bottom is of great importance." @default.
- W2384695219 created "2016-06-24" @default.
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- W2384695219 date "1974-01-01" @default.
- W2384695219 modified "2023-09-23" @default.
- W2384695219 title "ON SOME PROBLEMS ABOUT EMERGENCE AND SUBMERGENCE IN THE COASTAL REGION OF SOUTH CHINA SINCE QUARTERNARY PERIOD" @default.
- W2384695219 hasPublicationYear "1974" @default.
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