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Chemical remanent magnetization of the FeOOH, Fe2O3 system
Physics of the Earth and Planetary Interiors, 1968Abstract The Chemical Remanent Magnetization (CRM) produced by dehydrating the four isomers of ferric oxyhydroxide has been investigated using X-ray and thermoanalytical as well as thermomagnetic techniques. Synthetic powders were used set in a plaster of Paris matrix and the CRM acquired after heating in the Earth's field was measured using an ...
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Journal of Geophysical Research: Solid Earth, 1985
We have carried out a laboratory simulation of the chemical remanent magnetization (CRM) of titanomaghemites produced by seafloor oxidation of titanomagnetites carrying a primary thermoremanent magnetization (TRM). The starting material was well‐characterized synthetic monodomain titanomagnetite of composition Fe2.4Ti0.4Al0.2O4, dispersed in CaF2 and ...
Özden Özdemir, David J. Dunlop
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We have carried out a laboratory simulation of the chemical remanent magnetization (CRM) of titanomaghemites produced by seafloor oxidation of titanomagnetites carrying a primary thermoremanent magnetization (TRM). The starting material was well‐characterized synthetic monodomain titanomagnetite of composition Fe2.4Ti0.4Al0.2O4, dispersed in CaF2 and ...
Özden Özdemir, David J. Dunlop
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Izvestiya, Physics of the Solid Earth, 2017
© 2017, Pleiades Publishing, Ltd.The results of the experimental studies on creating chemical and partial thermal remanent magnetizations (or their combination), which are imparted at the initial stage of the laboratory process of the oxidation of primary magmatic titanomagnetites (Tmts) contained in the rock, are presented.
Gribov S., Dolotov A., Shcherbakov V.
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© 2017, Pleiades Publishing, Ltd.The results of the experimental studies on creating chemical and partial thermal remanent magnetizations (or their combination), which are imparted at the initial stage of the laboratory process of the oxidation of primary magmatic titanomagnetites (Tmts) contained in the rock, are presented.
Gribov S., Dolotov A., Shcherbakov V.
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Izvestiya, Physics of the Solid Earth, 2017
© 2017, Pleiades Publishing, Ltd. The results of the Thellier–Coe experiments on paleointensity determination on the samples which contain chemical remanent magnetization (CRM) created by thermal annealing of titanomagnetites are reported. The results of the experiments are compared with the theoretical notions. For this purpose, Monte Carlo simulation
Shcherbakov V., Sycheva N., Gribov S.
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© 2017, Pleiades Publishing, Ltd. The results of the Thellier–Coe experiments on paleointensity determination on the samples which contain chemical remanent magnetization (CRM) created by thermal annealing of titanomagnetites are reported. The results of the experiments are compared with the theoretical notions. For this purpose, Monte Carlo simulation
Shcherbakov V., Sycheva N., Gribov S.
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Physics of the Earth and Planetary Interiors, 1985
Abstract Oolitic hematite-bearing ironstones of the Silurian Red Mountain Formation of Alabama are shown to carry a single-component remanence stable enough to have survived major folding (of probable Permian age). Nevertheless, the remanence direction (ten sites yielding a paleopole at 38.0°N, 132.4°E with dm = 3.6°, dp = 1.9°), its reverse polarity
J.P. Hodych, R.R. Pätzold, K.L. Buchan
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Abstract Oolitic hematite-bearing ironstones of the Silurian Red Mountain Formation of Alabama are shown to carry a single-component remanence stable enough to have survived major folding (of probable Permian age). Nevertheless, the remanence direction (ten sites yielding a paleopole at 38.0°N, 132.4°E with dm = 3.6°, dp = 1.9°), its reverse polarity
J.P. Hodych, R.R. Pätzold, K.L. Buchan
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GEOPHYSICS, 1981
Redox chemical remanent magnetization (CRM) results from current flow associated with a redox potential cell. An active redox cell covered by later volcanics may continue in operation for a period of time, sufficiently long that the current flowing in the overlying volcanics will cause or assist in the remobilization of iron. The remobilization may be
Lloyal O. Bacon, Charles L. Elliot
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Redox chemical remanent magnetization (CRM) results from current flow associated with a redox potential cell. An active redox cell covered by later volcanics may continue in operation for a period of time, sufficiently long that the current flowing in the overlying volcanics will cause or assist in the remobilization of iron. The remobilization may be
Lloyal O. Bacon, Charles L. Elliot
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Journal of Geochemical Exploration, 2000
Abstract Paleomagnetic results from Jurassic sediment on Skye, Scotland, are consistent with the hypothesis that authigenic magnetite and an associated chemical remanent magnetization (CRM) can form during the conversion of smectite to illite. Sediment in north Skye, where smectite is abundant and the clays are unaltered, contain a weak and unstable ...
S.D Woods, R.D Elmore, M.H Engel
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Abstract Paleomagnetic results from Jurassic sediment on Skye, Scotland, are consistent with the hypothesis that authigenic magnetite and an associated chemical remanent magnetization (CRM) can form during the conversion of smectite to illite. Sediment in north Skye, where smectite is abundant and the clays are unaltered, contain a weak and unstable ...
S.D Woods, R.D Elmore, M.H Engel
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Integrative oncology: Addressing the global challenges of cancer prevention and treatment
Ca-A Cancer Journal for Clinicians, 2022Jun J Mao,, Msce +2 more
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