Deep water circulation changes in the northwestern Pacific during the past 180,000 years
碩士 === 國立臺灣大學 === 地質科學研究所 === 102 === At present the deep ocean carbon isotope minima (-0.2&;#8240;) is in the North Pacific, whereas during the Last Glacial Maximum (LGM) the minima (-0.9&;#8240;) was in the South Atlantic. Several previous studies pointed out that this shift was caused...
Main Authors: | Yun-Jung Chen, 陳韻嫆 |
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Other Authors: | 魏國彥 |
Format: | Others |
Language: | zh-TW |
Published: |
2013
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Online Access: | http://ndltd.ncl.edu.tw/handle/67435795701897459258 |
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