Magnetic susceptibility of sediment core LV76-21

The sediment magnetic susceptibility (MS) was measured onboard using a Satis Geo KM-7 kappameter at a resolution of 1 cm. Within 2 h after coring, the sediment core was split, and one half of core was used for the MS measurements. Values of the sediment MS are determined by concentration of terrigen...

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Bibliographic Details
Main Authors: Gorbarenko, Sergey A, Kirichenko, Ivan S, Psheneva, Olga, Bosin, Aleksandr A
Format: Dataset
Language:English
Published: PANGAEA
Subjects:
Akademik M.A. Lavrentyev
AMS 14C ages
Benthic and planktonic foraminifera
DEPTH
sediment/rock
Detroit Seamount
GC
Gravity corer
IRD
Kappameter
Satis Geo
KM-7
LV76
LV76-21
Magnetic susceptibility
productivity proxies
Planktonic foraminifera
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.954779
Description
Summary:The sediment magnetic susceptibility (MS) was measured onboard using a Satis Geo KM-7 kappameter at a resolution of 1 cm. Within 2 h after coring, the sediment core was split, and one half of core was used for the MS measurements. Values of the sediment MS are determined by concentration of terrigenous ferromagnetic material and of volcanogenic material as well.

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