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- W2368488984 abstract "Base on the constructed AMS14C calendar age,the components of n-alkanes and grain size of Quaternary sediments in bore ZK25 are used to elucidate the changes of sedimentary environment and palaeoclimate since Late Pleistocene.The results indicate that Late Pleistocene and Holocene environment experiences four stages in Dongxihu district between Yangtze River and Hanjiang River.In the stage I of Early Pleistocene,there were alluvial deposits in the ZK25 core,replaced by lake deposits with alluvial deposits.In the Late Pleistocene,climate was arid and was ended by an obvious cold/dry event.In stage Ⅱ,precipitation increased in the early period of Holocene and thick alluvium was deposited.In stage Ⅲ,it was still warm but changed from arid to wet during the middle period of Holocene and deposition environment was changed to low-level lake.In stage Ⅱ,temperature decreased and showed a cool period in Late Holocene with a trend from dry to wet." @default.
- W2368488984 created "2016-06-24" @default.
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- W2368488984 date "2011-01-01" @default.
- W2368488984 modified "2023-09-26" @default.
- W2368488984 title "Sedimentary Environment and Palaeoclimate Changes Reflected by Quaternary Sediments of the Bore ZK25 in Dongxihu District of Wuhan City" @default.
- W2368488984 hasPublicationYear "2011" @default.
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