Variation of the Lake Khanka level in the late Holocene, primorye
New data on the evolution of Lake Khanka and the formation of onshore bars at its western coast in the late Holocene are discussed in the paper. The late Subatlantic age of the bars and climatic conditions of their formation have been established. In the middle Holocene (SA II), the climate was warm...
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Veröffentlicht in: | Russian journal of Pacific geology 2008-06, Vol.2 (3), p.272-276 |
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