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Magnetite dissolution, diachronous greigite formation, and secondary magnetizations from pyrite oxidation: Unravelling complex magnetizations in Neogene marine sediments from New Zealand

Magnetite dissolution, diachronous greigite formation, and secondary magnetizations from pyrite oxidation: Unravelling complex magnetizations in Neogene marine sediments from New Zealand
Magnetite dissolution, diachronous greigite formation, and secondary magnetizations from pyrite oxidation: Unravelling complex magnetizations in Neogene marine sediments from New Zealand
Detailed rock magnetic and electron microscope analyses indicate that the magnetic signature of Neogene marine sediments from the east coast of New Zealand is dominated by the authigenic iron sulphide greigite. The greigite is present as a mixed population of stable single domain and superparamagnetic grains, which is consistent with authigenic growth from solution. This growth can result from pyritization reactions soon after deposition, which also leads to dissolution of most detrital magnetite; however, where constrained by field tests, our data suggest that remanence acquisition can occur > 1 Myr after deposition, and can vary in timing at the outcrop scale. Strong viscous overprints result from oxidation of the iron sulphides, probably during percolation of oxic ground water. This process can sometimes destroy any ancient remanent magnetization. This complex magnetic behaviour, particularly the presence of late-forming magnetizations carried by greigite, means that the remanence in New Zealand Cenozoic sediments, and in similar sediments elsewhere, cannot be assumed to be primary without confirmation by field tests. The reversals test should be employed with caution in such sediments, as patchy remagnetizations can lead to false polarity stratigraphies.
magnetite, dissolution, greigite, pyrite, hematite, remagnetization, new zealand
0012-821X
119-137
Rowan, C.J.
5d88ac64-c1d9-47c5-ba0a-ccf43eccc673
Roberts, A.P.
4497b436-ef02-428d-a46e-65a22094ba52
Rowan, C.J.
5d88ac64-c1d9-47c5-ba0a-ccf43eccc673
Roberts, A.P.
4497b436-ef02-428d-a46e-65a22094ba52

Rowan, C.J. and Roberts, A.P. (2006) Magnetite dissolution, diachronous greigite formation, and secondary magnetizations from pyrite oxidation: Unravelling complex magnetizations in Neogene marine sediments from New Zealand. Earth and Planetary Science Letters, 241 (1-2), 119-137. (doi:10.1016/j.epsl.2005.10.017).

Record type: Article

Abstract

Detailed rock magnetic and electron microscope analyses indicate that the magnetic signature of Neogene marine sediments from the east coast of New Zealand is dominated by the authigenic iron sulphide greigite. The greigite is present as a mixed population of stable single domain and superparamagnetic grains, which is consistent with authigenic growth from solution. This growth can result from pyritization reactions soon after deposition, which also leads to dissolution of most detrital magnetite; however, where constrained by field tests, our data suggest that remanence acquisition can occur > 1 Myr after deposition, and can vary in timing at the outcrop scale. Strong viscous overprints result from oxidation of the iron sulphides, probably during percolation of oxic ground water. This process can sometimes destroy any ancient remanent magnetization. This complex magnetic behaviour, particularly the presence of late-forming magnetizations carried by greigite, means that the remanence in New Zealand Cenozoic sediments, and in similar sediments elsewhere, cannot be assumed to be primary without confirmation by field tests. The reversals test should be employed with caution in such sediments, as patchy remagnetizations can lead to false polarity stratigraphies.

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More information

Published date: 15 January 2006
Keywords: magnetite, dissolution, greigite, pyrite, hematite, remagnetization, new zealand

Identifiers

Local EPrints ID: 24130
URI: http://eprints.soton.ac.uk/id/eprint/24130
ISSN: 0012-821X
PURE UUID: 7bb58788-fb33-446a-a6fa-46ea56e47919

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Date deposited: 22 Mar 2006
Last modified: 15 Mar 2024 06:53

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Contributors

Author: C.J. Rowan
Author: A.P. Roberts

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