Asian monsoon variability during 124-206 ka inferred from oxygen isotope records of stalagmites from Yangkou Cave, Chongqing, China
碩士 === 國立臺灣大學 === 地質科學研究所 === 100 === Asian monsoon (AM) variation over past 380 kyrs has been reconstructed using stalagmite oxygen isotope records from caves in China, showing that AM intensity primarily follows Northern Hemisphere summer insolation on orbital timescales. However, those 100s-kyr r...
| Main Authors: | , |
|---|---|
| Other Authors: | |
| Format: | Others |
| Language: | en_US |
| Published: |
2012
|
| Online Access: | http://ndltd.ncl.edu.tw/handle/24728991599443751903 |