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Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA

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Published

Standard

Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA. / Oldfield, Frank; Maher, Barbara; Donghue, J et al.
In: Journal of the Geological Society, Vol. 142, No. 6, 12.1985, p. 1035-1046.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Oldfield, F, Maher, B, Donghue, J & Pierce, J 1985, 'Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA', Journal of the Geological Society, vol. 142, no. 6, pp. 1035-1046. https://doi.org/10.1144/gsjgs.142.6.1035

APA

Vancouver

Oldfield F, Maher B, Donghue J, Pierce J. Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA. Journal of the Geological Society. 1985 Dec;142(6):1035-1046. doi: 10.1144/gsjgs.142.6.1035

Author

Oldfield, Frank ; Maher, Barbara ; Donghue, J et al. / Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA. In: Journal of the Geological Society. 1985 ; Vol. 142, No. 6. pp. 1035-1046.

Bibtex

@article{5c63c521027547bdbe26b4feb8970295,
title = "Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA",
abstract = "Characterization of both the source materials and the bottom sediments of an estuary by magnetic characters, on a particle size basis, allows the source of the bottom sediments to be determined and indicates a shift in sediment sources, corresponding to changing land-use patterns. The major source of the sediments in the lower part of cores from the middle of the estuary is eroding shorelines. Soil-derived particulates, from the uplands, dominate the upper part of the cores. This change in source occurred in the early part of the 19th century. The magnetic character of the most recent sediments suggests a progressive depletion, through time, of the upland soils in the finest fractions. ",
author = "Frank Oldfield and Barbara Maher and J Donghue and J Pierce",
year = "1985",
month = dec,
doi = "10.1144/gsjgs.142.6.1035",
language = "English",
volume = "142",
pages = "1035--1046",
journal = "Journal of the Geological Society",
issn = "0016-7649",
publisher = "Geological Society of London",
number = "6",

}

RIS

TY - JOUR

T1 - Particle-size related, mineral magnetic source sediment linkages in the Rhode River catchment, Maryland, USA

AU - Oldfield, Frank

AU - Maher, Barbara

AU - Donghue, J

AU - Pierce, J

PY - 1985/12

Y1 - 1985/12

N2 - Characterization of both the source materials and the bottom sediments of an estuary by magnetic characters, on a particle size basis, allows the source of the bottom sediments to be determined and indicates a shift in sediment sources, corresponding to changing land-use patterns. The major source of the sediments in the lower part of cores from the middle of the estuary is eroding shorelines. Soil-derived particulates, from the uplands, dominate the upper part of the cores. This change in source occurred in the early part of the 19th century. The magnetic character of the most recent sediments suggests a progressive depletion, through time, of the upland soils in the finest fractions.

AB - Characterization of both the source materials and the bottom sediments of an estuary by magnetic characters, on a particle size basis, allows the source of the bottom sediments to be determined and indicates a shift in sediment sources, corresponding to changing land-use patterns. The major source of the sediments in the lower part of cores from the middle of the estuary is eroding shorelines. Soil-derived particulates, from the uplands, dominate the upper part of the cores. This change in source occurred in the early part of the 19th century. The magnetic character of the most recent sediments suggests a progressive depletion, through time, of the upland soils in the finest fractions.

U2 - 10.1144/gsjgs.142.6.1035

DO - 10.1144/gsjgs.142.6.1035

M3 - Journal article

VL - 142

SP - 1035

EP - 1046

JO - Journal of the Geological Society

JF - Journal of the Geological Society

SN - 0016-7649

IS - 6

ER -