Autor: |
Kuo Fong Ma, Takashi Yanagidani, Setsuro Nakao, Ryo Fujio, Jim Mori, Hisao Ito, Yasuyuki Kano |
Rok vydání: |
2006 |
Předmět: |
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Zdroj: |
Geophysical Research Letters. 33 |
ISSN: |
0094-8276 |
Popis: |
[1] We have made observations of a heat signature that is associated with the frictional heat generated at the time of faulting for a large earthquake. Temperature measurements in a borehole that intersects the Chelungpu fault at a depth of about 1100 m, show a small increase near the fault even six years after the earthquake. The temperature signature has a symmetric shape with a width of about 40 m and is centered on the fault that slipped about 5 m during the 1999 Chi-Chi, Taiwan earthquake. The small amplitude of 0.06°C for the observed temperature anomaly indicates a very low level of friction that generated heat at the time of the earthquake. |
Databáze: |
OpenAIRE |
Externí odkaz: |
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