Geomagnetic Polarity Epochs and Pleistocene Geochronometry

@article{Cox1963GeomagneticPE,
  title={Geomagnetic Polarity Epochs and Pleistocene Geochronometry},
  author={Allan Cox and Richard R. Doell and G. Brent Dalrymple},
  journal={Nature},
  year={1963},
  volume={198},
  pages={1049-1051}
}
Retrospective on the plate tectonic revolution focusing on K/Ar dating, linear volcanic chains and the geomagnetic polarity time scale
Notions of migration of volcanism in the Hawaiian Islands were contemplated for decades, but no quantitative measurements were made until the early 1960s. Collections of volcanic rocks from theExpand
Quaternary time scales for the Pontocaspian domain : Interbasinal connectivity and faunal evolution
The Pontocaspian (Black Sea - Caspian Sea) region has a very dynamic history of basin development and biotic evolution. The region is the remnant of a once vast Paratethys Sea. It contains some ofExpand
Quaternary time scales for the Pontocaspian domain: Interbasinal connectivity and faunal evolution
The Pontocaspian (Black Sea Caspian Sea) region has a very dynamic history of basin development and biotic evolution. The region is the remnant of a once vast Paratethys Sea. It contains some of theExpand
Magnetic methods and the timing of geological processes
Abstract Magnetostratigraphy is best known as a technique that employs correlation among different stratigraphic sections using the magnetic directions that define geomagnetic polarity reversals asExpand
Quantitative Analysis of the Polarity Reversal Pattern of the Earth's Magnetic Field and Self-Reversing Dynamo Models
Craig, Patrick Shane M.S., Department of Earth and Environmental Sciences, Wright State University, 2013. Quantitative Analysis of the Polarity Reversal Pattern of the Earths Magnetic Field andExpand
Geochronology and the evolution of Australia in the Mesozoic
The Mesozoic geological history of the Australian continent saw the dispersal of Gondwana, of which Australia was part, and a change from progressive accretion of crust to the eastern one-third ofExpand
Modelling plate kinematics in the Scotia Sea
A new model of plate kinematics in the Scotia Sea region is presented in which continental crustal blocks and the signatures of seafloor spreading are defined semi-automatically using gravity andExpand
New 40Ar/39Ar age of the Bishop Tuff from multiple sites and sediment rate calibration for the Matuyama-Brunhes boundary
Precise dating of sanidine from proximal ash flow Bishop Tuff and air fall Bishop pumice and ash, California, can be used to derive an absolute age of the Matuyama Reversed-Brunhes Normal (M-B)Expand
An Automated System for Measuring In Situ K–Ar Ages
  • Jesús Solé
  • Materials Science
  • Geostandards and Geoanalytical Research
  • 2021
Review of the Early–Middle Pleistocene boundary and Marine Isotope Stage 19
  • M. Head
  • Progress in Earth and Planetary Science
  • 2021
The Global Boundary Stratotype Section and Point (GSSP) defining the base of the Chibanian Stage and Middle Pleistocene Subseries at the Chiba section, Japan, was ratified on January 17, 2020.Expand
...
1
2
3
4
5
...

References

SHOWING 1-7 OF 7 REFERENCES
Potassium-Argon Dates of Some Cenozoic Volcanic Rocks of the Sierra Nevada, California
A date of 19.9 m. y. (early Hemingfordian) from a welded rhyolite tuff at the top of the type section of the Valley Springs Formation, and one of 25.7 m. y. (early Arikareean) from the basal weldedExpand
Oxidation of Iron-Titanium Oxides in Igneous Rocks
Iron-titanium oxides in the compositional range magnetite-ulvospinel-ilmenite are likely to undergo oxidation during cooling in the presence of magmatic gases or air. The mineralogy and magneticExpand
Self-reversal of magnetization in a shale containing pyrrhotite
Abstract A series of experiments are described on self-reversal of magnetization in a rock containing pyrrhotite. This self-reversal was produced by heat-treatment at about 320°c. Two unusual effectsExpand
The magnetic properties of ilmenite-haematite crystals
  • C. M. Carmichael
  • Chemistry
  • Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences
  • 1961
The interpretation of both palaeomagnetic and geophysical prospecting data requires a better understanding of the magnetic properties of the iron oxide minerals found in rocks. The magneticExpand
Reverse Magnetization of Rocks and Its Connection with the Geomagnetic Field
From the present knowledge on the magnetism of rocks, palaeomagnetic study by means of the natural remanent magnetization of igneous rocks is reliable when and only when the natural remanentExpand