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    कार्ल्सवर्ग पर्वतश्रेणी के तलछट की विशेषता

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    Vaigyanik_42_39.pdf (4.611Mb)
    Date
    2010
    Author
    Valsangkar, A.B.
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    Abstract
    The sediment coverage in the Carlsberg Ridge is similar in appearance to those in the Mid-Atlantic Ridge. The Carlsberg Ridge sediments show that their sources are continental, biogenic and diagenetic. The sedimentation rate determined by Th232 decay is 3 cm/ ka. The sediments are dominant in CaCO3 % and illite mineral, and low Cu, Fe and Mn %. They do not show enrichment of Fe, Mn and magnetic susceptibility.
    URI
    http://drs.nio.org/drs/handle/2264/5138
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