Sedimentation rates in Funka Bay, HokkaidÔ

EijiMatsumoto; ShigekoTogashi

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Sedimentation rates in Funka Bay, HokkaidÔ

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Undisturbed sediment cores were collected by a modified gravity corer from Funka Bay. The sedimentation rate is determined by both210Pb and pumice chronological methods. The sedimentation rates by210Pb method are concordant with those by pumice methods. The derived rate varies from 0.06 to 0.22 g cm−2y−1, and an average is 0.09 g cm

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《日本海洋学会誌》 |2005年第6期|261-267|共页
作者
EijiMatsumoto; ShigekoTogashi;
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作者单位

Geological Survey of Japan;

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收录信息美国《科学引文索引》(SCI);
原文格式 PDF
正文语种英语
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Sedimentation rates in Funka Bay, HokkaidÔ

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