|
English
|
正體中文
|
简体中文
|
全文筆數/總筆數 : 80990/80990 (100%)
造訪人次 : 42118891
線上人數 : 1204
|
|
|
資料載入中.....
|
請使用永久網址來引用或連結此文件:
http://ir.lib.ncu.edu.tw/handle/987654321/50530
|
題名: | An extraordinary episode of Yellowstone caldera uplift, 2004-2010, from GPS and InSAR observations |
作者: | Chang,WL;Smith,RB;Farrell,J;Puskas,CM |
貢獻者: | 地球科學系 |
關鍵詞: | DEFORMATION;SUBSIDENCE;MIGRATION;INTRUSION;BENEATH |
日期: | 2010 |
上傳時間: | 2012-03-27 17:36:16 (UTC+8) |
出版者: | 國立中央大學 |
摘要: | Geodetic measurements of Yellowstone ground deformation from 2006 to June 2010 reveal deceleration of the recent uplift of the Yellowstone caldera following an unprecedented period of uplift that began in 2004. In 2006-2008 uplift rates decreased from 7 to 5 cm/yr and 4 to 2 cm/yr in the northern and southwest caldera, respectively, and in 2009 rates further reduced to 2 cm/yr and 0.5 cm/yr in the same areas. Elastic-dislocation modeling of the deformation data robustly indicates an expanding sill at similar to 7-10 km depth near the top of a seismically imaged, crystallizing magma reservoir, with a 60% decrease in the volumetric expansion rate between 2006 and 2009. Reduction of hydrothermal-volcanic recharge from beneath the northeast caldera and seismic moment release of the 2008 and 2010 large earthquake swarms are plausible mechanisms for decelerating the caldera uplift and may have influenced the change in recent caldera motion from uplift to subsidence. Citation: Chang, W.-L., R. B. Smith, J. Farrell, and C. M. Puskas (2010), An extraordinary episode of Yellowstone caldera uplift, 2004-2010, from GPS and InSAR observations, Geophys. Res. Lett., 37, L23302, doi:10.1029/2010GL045451. |
關聯: | GEOPHYSICAL RESEARCH LETTERS |
顯示於類別: | [地球科學學系] 期刊論文
|
文件中的檔案:
檔案 |
描述 |
大小 | 格式 | 瀏覽次數 |
index.html | | 0Kb | HTML | 699 | 檢視/開啟 |
|
在NCUIR中所有的資料項目都受到原著作權保護.
|
::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::