这在青藏高原东缘环境演化过程中,说明青藏高原第四纪冰期序列所反映的气候波动周期长、幅度大,并与高原隆升同步发生。
What happened in the environmental evolution in the eastern Tibet Plateau shows that climate change, which reflected by quaternary moraine series, has long cycle and great breadth.
分析末次冰期以来东海沉积物来源,对揭示古海洋、古气候变化和环境演化都有重要意义。
The studies to exhibit the sedimentary source in the East China Sea during the last glacial age are of great significance to reveal paleo-ocean, paleo-climate change and environmental evolution.
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