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Kuprin P. N. Ferronsky V. I. Popovchak V. P. Shlykov V. G. Zolotaya L. A. Kalisheva M. V. 《Water Resources》2003,30(2):136-153
Qualitative changes in the Caspian Sea water regime for the last 20–25 kyr are analyzed based on studying the particle-size distribution, the composition of clay minerals, the mineral composition of the coarse clastic fraction, and the magnetic susceptibility of deep-sea bottom sediments. 相似文献
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