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- W2352001344 abstract "The sedimentary sequences since 13 ka BP have been established in the Bala lake area, Kahu Co, northern Tibet, through a study of a lacustrine section. The climate since 13 ka BP may be divided into two dry-cold phases and two moist phases, of which the two moist phases and the dry-cold phase of the second cycle may be broadly correlated with the first and second new Hypsithermal phases and second new glacial phase in the northern hemisphere. This in the main reflects the general regularity of global climatic change since the last deglaciation. The response of the interior of the Qinghai-Tibet Plateau to the global climatic change is relatively sensitive." @default.
- W2352001344 created "2016-06-24" @default.
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- W2352001344 date "2007-01-01" @default.
- W2352001344 modified "2023-09-23" @default.
- W2352001344 title "Lake deposits and environmental evolution of the Bala lake area,Kahu Co,northwestern Gêrzê, Tibet,China,since 13 kaBP" @default.
- W2352001344 hasPublicationYear "2007" @default.
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