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Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism: ODP Leg 110

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Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism: ODP Leg 110. / Hounslow, M. W.; Bootes, P. A.; Whyman, G.
In: Proceedings of the Ocean Drilling Program, Scientific Results, 1990, p. 379-391.

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

Harvard

Hounslow, MW, Bootes, PA & Whyman, G 1990, 'Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism: ODP Leg 110', Proceedings of the Ocean Drilling Program, Scientific Results, pp. 379-391. https://doi.org/10.2973/odp.proc.sr.110.155.1990

APA

Hounslow, M. W., Bootes, P. A., & Whyman, G. (1990). Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism: ODP Leg 110. Proceedings of the Ocean Drilling Program, Scientific Results, 379-391. https://doi.org/10.2973/odp.proc.sr.110.155.1990

Vancouver

Hounslow MW, Bootes PA, Whyman G. Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism: ODP Leg 110. Proceedings of the Ocean Drilling Program, Scientific Results. 1990;379-391. doi: 10.2973/odp.proc.sr.110.155.1990

Author

Hounslow, M. W. ; Bootes, P. A. ; Whyman, G. / Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism : ODP Leg 110. In: Proceedings of the Ocean Drilling Program, Scientific Results. 1990 ; pp. 379-391.

Bibtex

@article{19e952c60e6f424e80e2b504995c2c5b,
title = "Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism: ODP Leg 110",
abstract = "The depositional remanent magnetization of samples collected on ODP Leg 110 is partially overprinted by a magnetization acquired in the Brunhes and an enigmatic coring or sampling remanence. The overprint acquired in the Brunhes may be a result of deformation related to grain fabric modification or to diagenetic alteration of the remanence-carrying titanomagnetite, derived from volcanic ash. In some samples from Hole 671B the primary remanence is partially retained, leading to a polarity stratigraphy that correlates with part of the Pleistocene-Pliocene sequence. However, the polarity stratigraphy is of too poor a quality to enable any meaningful time constraints. In the section with steeply dipping bedding in Hole 671B the anisotropy of magnetic susceptibility can be used to correct the remanence inclination because of the unique relationship between geomagnetic north and the E-W compression direction at this site. ",
author = "Hounslow, {M. W.} and Bootes, {P. A.} and G. Whyman",
year = "1990",
doi = "10.2973/odp.proc.sr.110.155.1990",
language = "English",
pages = "379--391",
journal = "Proceedings of the Ocean Drilling Program, Scientific Results",

}

RIS

TY - JOUR

T1 - Remanent magnetization of sediments undergoing deformation in the Barbados accretionary prism

T2 - ODP Leg 110

AU - Hounslow, M. W.

AU - Bootes, P. A.

AU - Whyman, G.

PY - 1990

Y1 - 1990

N2 - The depositional remanent magnetization of samples collected on ODP Leg 110 is partially overprinted by a magnetization acquired in the Brunhes and an enigmatic coring or sampling remanence. The overprint acquired in the Brunhes may be a result of deformation related to grain fabric modification or to diagenetic alteration of the remanence-carrying titanomagnetite, derived from volcanic ash. In some samples from Hole 671B the primary remanence is partially retained, leading to a polarity stratigraphy that correlates with part of the Pleistocene-Pliocene sequence. However, the polarity stratigraphy is of too poor a quality to enable any meaningful time constraints. In the section with steeply dipping bedding in Hole 671B the anisotropy of magnetic susceptibility can be used to correct the remanence inclination because of the unique relationship between geomagnetic north and the E-W compression direction at this site. 

AB - The depositional remanent magnetization of samples collected on ODP Leg 110 is partially overprinted by a magnetization acquired in the Brunhes and an enigmatic coring or sampling remanence. The overprint acquired in the Brunhes may be a result of deformation related to grain fabric modification or to diagenetic alteration of the remanence-carrying titanomagnetite, derived from volcanic ash. In some samples from Hole 671B the primary remanence is partially retained, leading to a polarity stratigraphy that correlates with part of the Pleistocene-Pliocene sequence. However, the polarity stratigraphy is of too poor a quality to enable any meaningful time constraints. In the section with steeply dipping bedding in Hole 671B the anisotropy of magnetic susceptibility can be used to correct the remanence inclination because of the unique relationship between geomagnetic north and the E-W compression direction at this site. 

U2 - 10.2973/odp.proc.sr.110.155.1990

DO - 10.2973/odp.proc.sr.110.155.1990

M3 - Journal article

AN - SCOPUS:0025665803

SP - 379

EP - 391

JO - Proceedings of the Ocean Drilling Program, Scientific Results

JF - Proceedings of the Ocean Drilling Program, Scientific Results

ER -