Low total and inorganic carbon contents within the Taiwan Chelungpu fault system
Low total and inorganic carbon contents within the Taiwan Chelungpu fault system
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DOI：
10.2343/geochemj.41.391
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发表时间：
2007-10
影响因子：
0.8
通讯作者：
M. Ikehara;T. Hirono;O. Tadai;M. Sakaguchi;H. Kikuta;T. Fukuchi;T. Mishima;N. Nakamura;K. Aoike;K. Fujimoto;Y. Hashimoto;T. Ishikawa;Hisao Itô;M. Kinoshita;Weiren Lin;K. Masuda;Takuo Matsubara;O. Matsubayashi;K. Mizoguchi;M. Murayama;K. Otsuki;H. Sone;M. Takahashi;W. Tanikawa;M. Tanimizu;W. Soh;Sheng-rong Song
中科院分区：
文献类型：
--
作者：
M. Ikehara;T. Hirono;O. Tadai;M. Sakaguchi;H. Kikuta;T. Fukuchi;T. Mishima;N. Nakamura;K. Aoike;K. Fujimoto;Y. Hashimoto;T. Ishikawa;Hisao Itô;M. Kinoshita;Weiren Lin;K. Masuda;Takuo Matsubara;O. Matsubayashi;K. Mizoguchi;M. Murayama;K. Otsuki;H. Sone;M. Takahashi;W. Tanikawa;M. Tanimizu;W. Soh;Sheng-rong Song
我们提供了从1999年集集地震时发生滑动的台湾车笼埔断层系统中采集的岩心样品的总碳和无机碳含量，并报告了FZB 1136中黑色泥带（B孔中1136 m深处的断层带）以及FZB 1194和FZB 1243中黑色物质盘中无机碳含量较低。
We presented the total and inorganic carbon contents of core samples recovered from the Taiwan Chelungpu fault system, which slipped at the 1999 Chi-Chi earthquake, and reported lower contents of inorganic carbon within the black gouge zone in FZB1136 (fault zone at depth 1136 m in Hole B) and in the black-material disks in FZB1194 and FZB1243.