Anoxic sediments of the Kveithola Trough, Barents Sea (Arctic region), micropaleontological and sedimentological evidences.
Abstract The glacially influenced Kveithola Trough is an abrupt narrow sedimentary system located in the NW Barents Sea. Along with the larger Storfjorden glacial system, it hosted, during the last glaciation, ice streams draining ice from the southern Svalbard in the north and Bear Island in the so...
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Format: | Text |
Language: | Italian |
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Pisa University
2017
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Online Access: | http://etd.adm.unipi.it/theses/available/etd-09192017-154942/ |