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Ferrimagnetic Cr and Mn spinels in sediments: Residual magnetic minerals after diagenetic dissolution

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Ferrimagnetic Cr and Mn spinels in sediments: Residual magnetic minerals after diagenetic dissolution. / Hounslow, MW.
In: Geophysical Research Letters, Vol. 23, No. 20, 01.10.1996, p. 2823-2826.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Hounslow, MW 1996, 'Ferrimagnetic Cr and Mn spinels in sediments: Residual magnetic minerals after diagenetic dissolution', Geophysical Research Letters, vol. 23, no. 20, pp. 2823-2826. https://doi.org/10.1029/96GL01327

APA

Hounslow, MW. (1996). Ferrimagnetic Cr and Mn spinels in sediments: Residual magnetic minerals after diagenetic dissolution. Geophysical Research Letters, 23(20), 2823-2826. https://doi.org/10.1029/96GL01327

Vancouver

Hounslow MW. Ferrimagnetic Cr and Mn spinels in sediments: Residual magnetic minerals after diagenetic dissolution. Geophysical Research Letters. 1996 Oct 1;23(20):2823-2826. doi: 10.1029/96GL01327

Author

Hounslow, MW. / Ferrimagnetic Cr and Mn spinels in sediments : Residual magnetic minerals after diagenetic dissolution. In: Geophysical Research Letters. 1996 ; Vol. 23, No. 20. pp. 2823-2826.

Bibtex

@article{05a44aa164784b10b29786e99ecfb88e,
title = "Ferrimagnetic Cr and Mn spinels in sediments: Residual magnetic minerals after diagenetic dissolution",
abstract = "Ferrimagnetic Cr-Fe and Mn-Fe spinels are the dominant remanence carrying phases in the late Triassic Lunde Formation. These have largely been identified by magnetic mineral extraction from the sediments, combined with microscopy. The extensive removal of most of the originally deposited magnetic Fe-Ti oxides during diagenesis has left the Cr-Fe and Mn-Fe spinels as a mineral residue which is resistant to dissolution. The rock magnetic signature of these minerals is not sufficiently known, to be able to identify these minerals on the basis of their magnetic properties alone.",
author = "MW Hounslow",
year = "1996",
month = oct,
day = "1",
doi = "10.1029/96GL01327",
language = "English",
volume = "23",
pages = "2823--2826",
journal = "Geophysical Research Letters",
issn = "0094-8276",
publisher = "John Wiley & Sons, Ltd",
number = "20",

}

RIS

TY - JOUR

T1 - Ferrimagnetic Cr and Mn spinels in sediments

T2 - Residual magnetic minerals after diagenetic dissolution

AU - Hounslow, MW

PY - 1996/10/1

Y1 - 1996/10/1

N2 - Ferrimagnetic Cr-Fe and Mn-Fe spinels are the dominant remanence carrying phases in the late Triassic Lunde Formation. These have largely been identified by magnetic mineral extraction from the sediments, combined with microscopy. The extensive removal of most of the originally deposited magnetic Fe-Ti oxides during diagenesis has left the Cr-Fe and Mn-Fe spinels as a mineral residue which is resistant to dissolution. The rock magnetic signature of these minerals is not sufficiently known, to be able to identify these minerals on the basis of their magnetic properties alone.

AB - Ferrimagnetic Cr-Fe and Mn-Fe spinels are the dominant remanence carrying phases in the late Triassic Lunde Formation. These have largely been identified by magnetic mineral extraction from the sediments, combined with microscopy. The extensive removal of most of the originally deposited magnetic Fe-Ti oxides during diagenesis has left the Cr-Fe and Mn-Fe spinels as a mineral residue which is resistant to dissolution. The rock magnetic signature of these minerals is not sufficiently known, to be able to identify these minerals on the basis of their magnetic properties alone.

U2 - 10.1029/96GL01327

DO - 10.1029/96GL01327

M3 - Journal article

VL - 23

SP - 2823

EP - 2826

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

IS - 20

ER -