Results 61 to 70 of about 699 (206)
Can relative paleointensities be determined from the normalized magnetization of the wind‐blown loess of China? [PDF]
Although the wind‐blown loess and interbedded paleosol sequence in the Loess Plateau of China has been extensively studied and regarded as one of the most complete terrestrial records of both the geomagnetic field and climatic changes during the Quaternary, little attention has been paid to it as a source of relative paleointensity.
Pan, Y.X. +4 more
openaire +1 more source
Abstract The late Eocene to early Oligocene is an intriguing Paleogene period in which the Earth climate state changed from Warmhouse to Coolhouse. Accurate age models are essential for investigating these climate transitions. The southwestern Pacific International Ocean Discovery Program (IODP) Site U1553, with its almost complete succession of the ...
Yang Zhang +5 more
wiley +1 more source
The magnetization and relative paleointensity of experimentally deposited natural sediments [PDF]
University of Minnesota M.S. thesis. June 2017. Major: Earth Sciences. Advisors: Dario Bilardello, Joshua Feinberg. 1 computer file (PDF); vi, 83 pages.The magnetization of a sediment occurs when ferromagnetic detrital particles align with a ...
Molinek, Frank
core
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB8601-3
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB8601-
Bleil, Ulrich +3 more
core +1 more source
A Holocene Paleosecular Variation Record From the Northwestern Ross Sea, Antarctica
We present a mid‐to‐late Holocene record of relative paleosecular variation from the Ross Sea region of Antarctica. The 6,700‐year‐long record of inclination, declination, and relative paleointensity from a marine sediment core collected near Cape Adare ...
Olivia J. Truax +7 more
doaj +1 more source
We report paleomagnetic records of Matuyama–Brunhes geomagnetic polarity reversal and associated key tephra layers from the Early–Middle Pleistocene marine sedimentary succession in the Boso Peninsula. The outcrop is in Terasaki, Chiba, Japan and ~ 25 km
Hirokuni Oda +3 more
doaj +1 more source
Abstract Paleomagnetic and rock magnetic analyses were conducted on sediment cores from the northeastern Greenland Shelf and Young Sound along the western edge of Fram Strait. The paleomagnetic signal in all three sediment cores is characterized by a strong and stable single component magnetization carried by low coercivity ferrimagnetic single domain ...
Juliette Girard +7 more
wiley +1 more source
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB6007-2
(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB6007-
Bleil, Ulrich +3 more
core +1 more source
We obtain new 40Ar/39Ar ages for three lavas that record part of the Matuyama‐Brunhes geomagnetic field reversal process on Guadeloupe. These lavas record a reversed‐transitional‐reversed magnetostratigraphy and yield a weighted mean isochron age of 785 ...
M. C. Brown +3 more
doaj +1 more source
Abstract The Ediacaran–Cambrian (∼635–539 Ma) geomagnetic field is characterized by unusually high reversal rates and markedly weakened field strength. Estimates of these reversal frequencies can reveal key aspects of deep Earth dynamics and their potential influence on surface environments and early complex life.
J. W. L. Afonso +12 more
wiley +1 more source

