Mid-Holocene paleoclimate of NW Taiwan inferred from d18O, d13C and Sr/Ca ratio of coral Porites skeleton
碩士 === 國立臺灣師範大學 === 地球科學系 === 100 === A drilling core (TY-05) was choosen from NW Taiwan and anaylzed the stable carbon and oxygen isotope composition and Sr/Ca ratio of the coral Porites inside. And analyzing the oxygen isotope composition of the seawater in the same study area, together this study...
| Main Authors: | , |
|---|---|
| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2011
|
| Online Access: | http://ndltd.ncl.edu.tw/handle/34090597951464013936 |