辽宁本溪庙洞降水、滴水和现生碳酸钙的 δ 18 O变化特征及其古气候意义
Cited by 0
Related Papers
The East Asian winter monsoon over the last 15,000 years: its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon
|Quaternary Science Reviews|2011|225
Applications of stalagmite laminae to paleoclimate reconstructions: Comparison with dendrochronology/climatology
|Quaternary Science Reviews|2006|142
Loess record of the aerodynamic environment in the east Asia monsoon area since 60,000 years before present
|Journal of Geophysical Research Atmospheres|2005|118
Temporal and spatial variations in the discharge and dissolved organic carbon of drip waters in Beijing Shihua Cave, China
|Hydrological Processes|2008|62