2003
DOI: 10.4217/opr.2003.25.4.529
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Classification of Deep-sen Sediment by Geotechnical Properties from the KODOS Area in the C-C Zone of the Northeast Equatorial Pacific

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Cited by 11 publications
(2 citation statements)
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“…The most straightforward explanation for these observations is that sediment particles within the pores and cracks of nodules are released to form part of the fines. Abyssal sediments in the KODOS area as well as other nodule exploration areas in the CCZ have average grain size of about 3-30 μm [31][32][33][34][35]. Thus, it is reasonable to expect that sediment particles encapsulated in the nodules are mostly silts and clays as well.…”
Section: Causes Of Compositional Variationmentioning
confidence: 99%
“…The most straightforward explanation for these observations is that sediment particles within the pores and cracks of nodules are released to form part of the fines. Abyssal sediments in the KODOS area as well as other nodule exploration areas in the CCZ have average grain size of about 3-30 μm [31][32][33][34][35]. Thus, it is reasonable to expect that sediment particles encapsulated in the nodules are mostly silts and clays as well.…”
Section: Causes Of Compositional Variationmentioning
confidence: 99%
“…. 이러한 이유 는 우리나라의 북쪽과 남쪽광구는 망간단괴의 형태 및 크기와 같은 분포특성, 퇴적물의 구성 성분, 지질공학 적인 특성 등이 다르기 때문이다 (Chi et al, 2003;MOMAF, 2007; 산출된 부존률을 직접 비교하여 보정상수를 산출하였다. (KORDI, 1993(KORDI, , 1994과 점유율 및 단괴 축의 길이를 이용하여 부존률을 보정하는 방 법으로 구분할 수 있다 (Handa and Tsurusaki, 1981;Sharma, 1989aSharma, , 1989bSharma and Kodagari, 1990).…”
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