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...

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Bibliographic Details
Main Authors: Chien-Cheng Hung, 洪建程
Other Authors: Li-Wei Kuo
Format: Others
Language:zh-TW
Published: 2017
Online Access:http://ndltd.ncl.edu.tw/handle/96174782671134842415