Mineralogical and petrographic composition of the sediments as an indicator of environmental changes in the Franz Victoria Trough, the Barents Seaстатья
Аннотация:Sediments from a core in the Franz Victoria trough, the Barents Sea, are studied in termsof mineralogical and petrographic composition. The main constituents were ‘black shale,quartz, siltstone, sandstone, quartzite, argillite, and carbonates. The core was eventuallydivided into three layers representing three stages of late deglaciation: I. deglacial, II.transitional period, III. Holocene.