Lithology, heavy mineral associations, and chemical composition of bottom sediments studied in two gravity cores from Isfjord, Western Spitsbergen (Svalbard) accompanied by high-frequency seismic records, provide a new insight on provenance and glaciomarine sedimentation in the fjord from the last deglaciation through Holocene.
Supplement to: Levitan, Mikhail A; Levchenko, Oleg V; Murdmaa, Ivar O; Peresypkin, Valery I; Roshchina, IA; Tolmacheva, AV (2008): History of sedimentation in Isfjord (Western Spitsbergen). Translated from Litologiya i Poleznye Iskopaemye, 2008, 6, 578-600, Lithology and Mineral Resources, 43(6), 520-541, doi:10.1134/S0024490208060023