Frictional Properties of Hualien Hoping Granitic Gneiss, Taiwan, and Its Implication
碩士 === 國立中央大學 === 地球科學學系 === 105 === Fault-origin pseudotachylyte is a solidified melt produced by frictional heating during big earthquakes. It is well-known as a seismic indicator which can provide information on earthquake physics. A new locality of pseudotachylyte-bearing fault, hosted in the Ta...
| Main Authors: | , |
|---|---|
| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2017
|
| Online Access: | http://ndltd.ncl.edu.tw/handle/96174782671134842415 |