Add to ORKGDuring the DELP-1986 cruise, three components of the geomagnetic field and the total force intensity were measured with an STCM (Shipboard Three Component Magnetometer) and a proton precession magnetometer. STCM provides three component geomagnetic field intensities on board a research vessel, of which results can be used to identify the orientation of the magnetic lineament from only one single ship track. Our data give some additional information on the magnetic anomaly lineation patterns of the northwestern Pacific and the direction of lineation of the area surveyed by the present cruise is reexamined by the three component magnetic field data. The direction of geomagnetic anomaly lineation of this area is confirmed to run with a N70°E s...
Geomagnetic observation by a proton precession magnetometer has been resumed at a station in the cen...
Assuming uniformity of magnetization, the direction and intensity of magnetization of nine seamounts...
The three components and total intensity of the geomagnetic field were measured using STCM and a pro...
During the DELP-1986 cruise, three components of the geomagnetic field and the total force intensity...
Three components and total intensity of the geomagnetic field were measured by Shipboard Three Compo...
Three components and total intensity of the geomagnetic field were measured by Shipboard Three Compo...
The direction and magnitude of the magnetization of four seamounts in the Pacific near the Japanese ...
A total force geomagnetic survey was made in the northwestern Pacific during the US-Japan Scientific...
Geomagnetic total force was measured by a towed proton precession magnetometer in the north-western ...
Geomagnetic total force was measured by a towed proton precession magnetometer in the north-western ...
The magnetic local attraction and horizontal force in the coast of Tanegashima were investigated in ...
A magnetic and bathymetric survey in the eastern part of the Japan Basin resulted in low amplitude a...
The writers carried out simultaneous observations of three geomagnetic components at four stations s...
The magnetic local attraction and horizontal force in the coast of Tanegashima were investigated in ...
Assuming uniformity of magnetization, the direction and intensity of magnetization of nine seamounts...
Geomagnetic observation by a proton precession magnetometer has been resumed at a station in the cen...
Assuming uniformity of magnetization, the direction and intensity of magnetization of nine seamounts...
The three components and total intensity of the geomagnetic field were measured using STCM and a pro...
During the DELP-1986 cruise, three components of the geomagnetic field and the total force intensity...
Three components and total intensity of the geomagnetic field were measured by Shipboard Three Compo...
Three components and total intensity of the geomagnetic field were measured by Shipboard Three Compo...
The direction and magnitude of the magnetization of four seamounts in the Pacific near the Japanese ...
A total force geomagnetic survey was made in the northwestern Pacific during the US-Japan Scientific...
Geomagnetic total force was measured by a towed proton precession magnetometer in the north-western ...
Geomagnetic total force was measured by a towed proton precession magnetometer in the north-western ...
The magnetic local attraction and horizontal force in the coast of Tanegashima were investigated in ...
A magnetic and bathymetric survey in the eastern part of the Japan Basin resulted in low amplitude a...
The writers carried out simultaneous observations of three geomagnetic components at four stations s...
The magnetic local attraction and horizontal force in the coast of Tanegashima were investigated in ...
Assuming uniformity of magnetization, the direction and intensity of magnetization of nine seamounts...
Geomagnetic observation by a proton precession magnetometer has been resumed at a station in the cen...
Assuming uniformity of magnetization, the direction and intensity of magnetization of nine seamounts...
The three components and total intensity of the geomagnetic field were measured using STCM and a pro...