24. ORIGIN OF AUTHIGENIC CARBONATES IN EOCENE TO QUATERNARY SEDIMENTS FROM THE ARCTIC OCEAN AND NORWEGIAN-GREENLAND SEA1
Authigenic carbonates occur in thin layers, nodules, and burrows in fine-grained siliciclastic sediments of middle Eocene to Quaternary age that were recovered from the Arctic Ocean and Norwegian-Greenland Sea during Leg 151. At Site 913 (East Greenland Margin), concentrically zoned microspherules a...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.492.8070 http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_24.pdf |