Results 81 to 90 of about 4,180 (226)
Abstract Self‐reversed magnetization, acquired antiparallel to the external field, can complicate the interpretation of paleomagnetic directional records, particularly in altered greigite‐bearing sediments with anomalous magnetizations. The underlying physical process for this self‐reversal remains poorly constrained.
Shichu Chen, Liao Chang, Wyn Williams
wiley +1 more source
(Table 1) Paleomagnetism at DSDP Hole 83-504B
(Table 1) Paleomagnetism at DSDP Hole 83 ...
Hajimu Kinoshita (6973205) +5 more
core +1 more source
Resolving the Internal Magnetic Domain Structure of Cloudy Zone Tetrataenite
Abstract Recent advances in magnetic imaging can directly capture the internal magnetization of natural and synthetic materials at resolutions <10 nm. This capability opens new possibilities to determine the magnetic domain state of ferromagnetic minerals that are fundamental for recording and retaining paleomagnetic records.
Elias N. Mansbach +5 more
wiley +1 more source
Paleomagnetic data enables the global reconstruction of the geomagnetic field, allowing the investigation of significant events like polarity reversals and excursions.
Ahmed Nasser Mahgoub +4 more
doaj +1 more source
Dating en matching in de Aardwetenschappen
In zijn oratie laat Wout Krijgsman vooral zien hoe je met een multi-disciplinaire aanpak de geologische geschiedenis het beste kunt dateren en hoe je met een internationale onderzoeksgroep een breder inzicht kunt verkrijgen in de grootschalige ...
Krijgsman, W., Paleomagnetism
core
Reconciling Paleomagnetism and Pangea. [PDF]
Although an array of geological and geophysical data support the conventional (Wegenerian) paleogeographic model of Pangea in the Late Triassic-Early Jurassic, its configuration in pre-Late Triassic time has remained controversial for the last half ...
Domeier, Mathew M.
core
The Steens Basalt, now considered part of the Columbia River Basalt Group (CRBG), contains the earliest eruptions of this magmatic episode. Lava flows of the Steens Basalt cover about 50,000 km2 of the Oregon Plateau in sections up to 1000 m thick.
Nicholas A. Jarboe +4 more
doaj +1 more source
Slow True Polar Wander Around Varying Equatorial Axes Since 320 Ma
True polar wander (TPW), the rotation of the solid Earth relative to the spin axis, is driven by changes in the Earth's moment of inertia induced by mantle convection and may have influenced past climate and life. Long‐term TPW is typically inferred from
Bram Vaes, Douwe J. J. vanHinsbergen
doaj +1 more source
Acquisition of chemical remanent magnetization during experimental ferrihydrite-hematite conversion in Earth-like magnetic field-implications for paleomagnetic studies of red beds [PDF]
Hematite-bearing red beds are renowned for their chemical remanent magnetization (CRM). If the CRM was acquired substantially later than the sediment was formed, this severely compromises paleomagnetic records.
Jiang, Zhaoxia +8 more
core +1 more source
Paleomagnetism of western equatorial Pacific sediment cores [PDF]
Stable, detrital paleomagnetism measured in samples from 78 deep-sea sediment cores from the western equatorial Pacific provides the basis for a regional comparison of sediment magnetic characteristics and determination of area-wide patterns of Pliocene ...
Hammond, Stephen Randolph.
core

