1、

Different ages in the last glacial epoch in Xishan Mountain, Beijing area, the pollen that loess contained, all regard herbs pollen as principle.

北京西山末次冰期不同时代黄土所含花粉,均以草本植物花粉为主。

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2、

The late glacial epoch in the area witnessed a cold-slightly dry or cool-slightly dry climate and repeated cold-warm climatic oscillations.

结果表明:该区晚冰期的气候特点为冷偏干或凉偏干,冷暖波动频繁。

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3、

It is showed by the study on stalagmite records that the last glacial epoch corresponds to YD and the Heinrich events recorded in North Atlantic sediment, and also corresponds to ice core from Greenland.

。研究表明,末次冰期相当于格陵兰冰芯记录、北大西洋沉积记录的YD、Heinrich事件等的气候跃变事件,几根石笋取得了非常一致的准确定位及定年。

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5、

The big glacial period in geological history and it's composition analysis

地质历史中的大冰期及其成因分析

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6、

On basic features of climate and environment in Quaternary glacial period in eastern China

中国东部第四纪冰期气候与环境的基本特征

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7、

Evolution of natural environment in China since the last glacial period and its position in the global change

末次冰期以来中国自然环境变迁及其与全球变化的关系

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8、

Climate Effect of Dust Aerosol in Southern Chinese Loess Plateau Since the Last Glacial Period

黄土高原南部末次冰期以来沙尘气溶胶的气候效应

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9、

A new note on Quaternary glacial period in the Lushan mountain, east China

庐山第四纪冰期研究的新认识

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10、

Evidence of fossil Ostracodes for environmental changes of Bohai Sea since late glacial period

渤海晚冰期以来环境变化的化石介形类证据

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