琉球嶼的海階及珊瑚定年研究
| dc.contributor.author | 石再添 | zh_tw |
| dc.contributor.author | 張瑞津 | zh_tw |
| dc.contributor.author | 許民陽 | zh_tw |
| dc.contributor.author | 沈淑敏 | zh_tw |
| dc.date.accessioned | 2014-10-27T15:40:21Z | |
| dc.date.available | 2014-10-27T15:40:21Z | |
| dc.date.issued | 1991-03-?? | zh_TW |
| dc.description.abstract | The Liu-chiu Y? is a raised coral reef island, located southwest offshore 14 km from Tung-kang, Pintung Hsien. Two structural depression lines striking NE-SW and E-W separate the island into four blocks. The Liu-Chiu Y? Limestone overlays the Liu-Chiu Y? Mudstone with a uncon-formity relationship. Three steps of marine terraces can be recognized: Pleistonce I, Pleistonce II and Holocene terrace. Based on coral reef dating, elevation of samples and sea level curve, the average uplift rate of west coast is estimated about 2 mm/yr during the period from 34 ka to 10 ka YBP whereas 0.4 mm/yr in east coast since Holocene. The uplift and deformation of marine terraces are influenced both by the tectonic stress coming southweast and downwarping near Kao-Ping Drowned Valley. | en_US |
| dc.identifier | 3783CDC3-9FCD-4AE3-70CC-B9F243F8B966 | zh_TW |
| dc.identifier.uri | http://rportal.lib.ntnu.edu.tw/handle/20.500.12235/23634 | |
| dc.language | 中文 | zh_TW |
| dc.publisher | 地理學系 | zh_tw |
| dc.publisher | Department of Geography, NTNU | en_US |
| dc.relation | (17)，85-97 | zh_TW |
| dc.relation.ispartof | 國立臺灣師範大學地理研究報告 | zh_tw |
| dc.subject.other | 定年 | zh_tw |
| dc.subject.other | 珊瑚 | zh_tw |
| dc.subject.other | 海階 | zh_tw |
| dc.subject.other | 琉球嶼 | zh_tw |
| dc.title | 琉球嶼的海階及珊瑚定年研究 | zh-tw |
| dc.title.alternative | The Marine Terraces and Coral Reef Dating in Liu-Chiu Yü, Taiwan | zh_tw |