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http://www.wdcb.ru/WDCB/IPY/Arctic_vlc.ru.html http://www.wdcb.ru/WDCB/IPY/Arctic_vlc.ru.html http://oai.dtic.mil/oai/oai?verb=getRecord&metadataPrefix=html&identifier=AD0687303 http://oai.dtic.mil/oai/oai?verb=getRecord&metadataPrefix=html&identifier=AD0687303 http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V72-48B5DTD-KB&_user=10&_coverDate=12%2F31%2F1969&_rdoc=1&_fmt=high&_orig=search&_origin=search&_sort=d&_docanchor=&view=c&_searchStrId=1483380019&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=d13aabce0e6957c65da90764a767b693&searchtype=a A short description is presented of the topography, sediments and magnetic anomaly pattern of the Gakkel (Mid-Arctic) Ridge which together with the adjoining abyssal Nansen and Amundsen basins forms the Eurasian Basin of typical oceanic nature in the Arctic Ocean. The Eurasian Basin is characterized by a linear, symmetric pattern of magnetic anomalies with prominent axial anomaly typical of the world mid-oceanic ridge system. A number of fracture zones have been deduced from the magnetic data and a preliminary estimate of the average rate of spreading of about 1.1 cm/year for the last 8√10 million years in the Eurasian Basin is obtained. Some evidence indicating the possible continental extension of the rift zone of the Gakkel Ridge into the Moma Trough is presented Volcano опхкюоребнлнпяйне нйнмвюмхе упеарю цюййекъ http://www.evgengusev.narod.ru/laptev.html http://shrrr.gorod.tomsk.ru/index-1271591642.php |
