Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
2008 Annual Meeting of Japan Association of Mineralogical Sciences
Session ID : S2-02
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S2: Water-rock interaction
Chemical reaction during an earthquake in the Taiwan Chelungpu fault
*Tetsuro HironoKoichiro FujimotoWataru TanikawaToshiaki MishimaTsuyoshi IshikawaMasaharu TanimizuResearch Group TCDP HoleB
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Abstract
The Taiwan Chelungpu-Fault Drilling Project was undertaken in 2002 to investigate the faulting mechanism of the 1999 Mw 7.6 Taiwan Chi-Chi earthquake. Hole B penetrated the Chelungpu fault, and core samples were recovered from between 948.42- and 1352.60-m depth. Three major zones, designated FZB1136 (fault zone at 1136-m depth in hole B), FZB1194, and FZB1243, were recognized in the core samples as active fault zones within the Chelungpu fault. Nondestructive continuous physical property measurements and various kind of the chemical analyses were conducted on all core samples. In this presentation, we introduce the main result from this project.
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© 2008 Japan Association of Mineralogical Sciences
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