Evidence of frictional melting from disk-shaped black material, discovered within the Taiwan Chelungpu fault system

Tetsuro Hirono*, Minoru Ikehara, Kenshiro Otsuki, Toshiaki Mishima, Masumi Sakaguchi, Wonn Soh, Masahiro Omori, Weiren Lin, En Chao Yeh, Wataru Tanikawa, Chien Ying Wang

*此作品的通信作者

研究成果: 雜誌貢獻期刊論文同行評審

74 引文 斯高帕斯(Scopus)

摘要

The Taiwan Chelungpu-fault Drilling Project penetrated three fault zones as the Chelungpu fault system, which slipped during the 1999 Chi-Chi earthquake, discovering disk-shaped black material (BM disk) within the middle and lower fault zones in Hole B. The microscopic features of the BM disks indicated that they were pseudotachylytes, and they showed high magnetic susceptibility, possibly the result of intense shearing or high temperature conditions. Inorganic carbon content of the BM disks was low, possibly because of thermal decomposition of carbonate minerals. The high temperatures might be related to frictional heating during the earthquake, implying that the BM disks were produced under intense shearing with frictional heating that reached melting temperature. Because the disks, which provide the only evidence of melting, pre-date the 1999 earthquake, we concluded that frictional melting did not occur during the earthquake.

原文英語
文章編號L19311
期刊Geophysical Research Letters
33
發行號19
DOIs
出版狀態已發佈 - 2006 10月
對外發佈

ASJC Scopus subject areas

  • 地球物理
  • 一般地球與行星科學

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