The complete sediment series recovered with the gravity corer during METEOR cruise M 41/1 were subjected to laboratory geophysical studies. Shipboard measurements on the segmented cores routinely comprised three basic physical parameters: - compressional (p-) wave velocity vp, - electric resistivity Rs (as a measure of density and porosity), - magnetic volume susceptibility K. These properties are closely related to lithology and grain-size of the sediments and provide high-resolution core logs (spacing 1 cm for p-wave velocity, 3 cm for electric resistivity and magnetic volume susceptibility) available prior to all other detailed investigations. In addition, oriented samples for subsequent shore based rock and paleomagnetic studies were t...
Whole-core measurements of Wet Bulk Density (WBD), compressional (P)-wave velocity (Vp), and Magneti...
Sediment magnetic properties are determined by the speciation, concentration and grain‐size range of...
This project aims to study the plausibility of using geophysical method alone to study the physical ...
The complete sediment series recovered during METEOR Cruise M 41/3 with the gravity corer were subje...
The complete sediment series recovered during METEOR Cruise M38/ 1 with the gravity corer were subje...
A large fraction of the sediment series recovered during METEOR Cruise M 46/2 with the gravity corer...
The sediment series recovered during METEOR Cruise M 46/4 with the gravity corer were subject to lab...
During METEOR Cruise M 34/1 all recovered gravity cores were subject to laboratory geophysical studi...
During METEOR Cruise 34/3 the recovered gravity cores were subject to laboratory geophysical studies...
The sediment series recovered during R/V METEOR Cruise M46/3 with the gravity corer were subject to ...
During METEOR Cruise 29/2 all of the recovered gravity cores were subjected to laboratory geophysica...
During METEOR Cruise 34/2 the recovered gravity cores were subject to laboratory geophysical studies...
During METEOR Cruise 29/1 all of the recovered gravity cores were subjected to laboratory geophysica...
During METEOR Cruise 23/2 the recovered gravity cares were subject to laboratory geophysical studies...
During METEOR Cruise M23/1 the recovered gravity and piston cores were subject to laboratory geophys...
Whole-core measurements of Wet Bulk Density (WBD), compressional (P)-wave velocity (Vp), and Magneti...
Sediment magnetic properties are determined by the speciation, concentration and grain‐size range of...
This project aims to study the plausibility of using geophysical method alone to study the physical ...
The complete sediment series recovered during METEOR Cruise M 41/3 with the gravity corer were subje...
The complete sediment series recovered during METEOR Cruise M38/ 1 with the gravity corer were subje...
A large fraction of the sediment series recovered during METEOR Cruise M 46/2 with the gravity corer...
The sediment series recovered during METEOR Cruise M 46/4 with the gravity corer were subject to lab...
During METEOR Cruise M 34/1 all recovered gravity cores were subject to laboratory geophysical studi...
During METEOR Cruise 34/3 the recovered gravity cores were subject to laboratory geophysical studies...
The sediment series recovered during R/V METEOR Cruise M46/3 with the gravity corer were subject to ...
During METEOR Cruise 29/2 all of the recovered gravity cores were subjected to laboratory geophysica...
During METEOR Cruise 34/2 the recovered gravity cores were subject to laboratory geophysical studies...
During METEOR Cruise 29/1 all of the recovered gravity cores were subjected to laboratory geophysica...
During METEOR Cruise 23/2 the recovered gravity cares were subject to laboratory geophysical studies...
During METEOR Cruise M23/1 the recovered gravity and piston cores were subject to laboratory geophys...
Whole-core measurements of Wet Bulk Density (WBD), compressional (P)-wave velocity (Vp), and Magneti...
Sediment magnetic properties are determined by the speciation, concentration and grain‐size range of...
This project aims to study the plausibility of using geophysical method alone to study the physical ...