-
(Figure 10b, 11) Benthic electromagnetic profile of GeoB130106 on the northwe...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 10a, 11, 12) Benthic electromagnetic profile of GeoB130124 on the nor...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 9b) Correlation of EM and sediment core susceptibility
This dataset has no description
-
(Figure 9a) Correlation of EM and sediment core porosity
EM Porosity is derived from Archie's law with constants m = 1.6 and a = 1. -
(Figure 7b) Apparent susceptibility profiles by various available sensor size...
Assumption: magnetite dissolution sets in at depths of 0.2-0.8 m and is completed 0.2 m deeper. -
(Figure 7a) Simulations of apparent susceptibility and conductivity profiles ...
This dataset has no description
-
(Figure 6b) Horizontal footprint diameter (90% of the total signal) and half-...
This dataset has no description
-
(Figure 6a) Lateral response of GEM-3 sensor (96 cm coil) for susceptibility ...
This dataset has no description
-
(Figure 5c) In-phase and quadrature responses of GEM-3 sensor at various oper...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 5b) Vertical sensor characteristics of GEM-3 (96 cm coil) for quadrat...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 4a) Relative contribution of the magnetic response to total in-phase ...
This dataset has no description
-
(Figure 3) Modeled GEM-3 susceptibility and conductivity response under decre...
This model result assumes that the sensor emerges from an infinite seawater half-space (kappa w = -9 x 10**-6 and Sigma w = 3 S/m; susceptibility in SI-units). -
Permanent Magnetotelluric Reference Station Wittstock, Germany
Magnetotellurics (MT) is a passive geophysical method which uses natural variations of electromagnetic fields generated by global lightning discharges and ionospheric current...
