The development of pass-through superconducting rock magnetometers (SRM) has greatly
promoted collection of paleomagnetic data from continuous long-core samples. The output of pass-through
measurement is smoothed and distorted due to convolution of magnetization with the magnetometer
sensor response. Although several studies could restore high-resolution paleomagnetic signal through
deconvolution of pass-through...
The development of pass-through superconducting rock magnetometers (SRM) has greatly
promoted collection of paleomagnetic data from continuous long-core samples. The output of pass-through
measurement is smoothed and distorted due to convolution of magnetization with the magnetometer
sensor response. Although several studies could restore high-resolution paleomagnetic signal through
deconvolution of pass-through...
Paleomagnetic analysis and radiocarbon dating of an expanded Holocene deep-sea sediment sequence
recovered by Integrated Ocean Drilling Program (IODP) Expedition 303 from Labrador Sea Site U1305
(Lat.: 57°28.5 N, Long.: 48°31.8 W, water depth 3459 m) provides insights into mechanisms that drive
both paleomagnetic secular variation (PSV) and magnetization acquisition...
Paleomagnetic analysis and radiocarbon dating of an expanded Holocene deep-sea sediment sequence
recovered by Integrated Ocean Drilling Program (IODP) Expedition 303 from Labrador Sea Site U1305
(Lat.: 57°28.5 N, Long.: 48°31.8 W, water depth 3459 m) provides insights into mechanisms that drive
both paleomagnetic secular variation (PSV) and magnetization acquisition...
The development of pass-through superconducting rock magnetometers (SRM) has greatly
promoted collection of paleomagnetic data from continuous long-core samples. The output of pass-through
measurement is smoothed and distorted due to convolution of magnetization with the magnetometer
sensor response. Although several studies could restore high-resolution paleomagnetic signal through
deconvolution of pass-through...
Paleomagnetic analysis and radiocarbon dating of an expanded Holocene deep-sea sediment sequence
recovered by Integrated Ocean Drilling Program (IODP) Expedition 303 from Labrador Sea Site U1305
(Lat.: 57°28.5 N, Long.: 48°31.8 W, water depth 3459 m) provides insights into mechanisms that drive
both paleomagnetic secular variation (PSV) and magnetization acquisition...
