Nilsson, Andreas et al. (2013): Magnetostratigraphic importance of secondary chemical remanent magnetizations carried by greigite (Fe (sub 3) S (sub 4) ) in Miocene sediments, New Jersey shelf (IODP Expedition 313)

Leg/Site/Hole:
IODP 313
Identifier:
2013-041374
georefid

10.1130/GES00854.1
doi

Creator:
Nilsson, Andreas
University of Liverpool, School of Environmental Sciences, Liverpool, United Kingdom
author

Lee, Youn Soo
Korea Institute of Geosicence and Mineral Resources, South Korea
author

Snowball, Ian
Uppsala University, Sweden
author

Hill, Mimi
author

Identification:
Magnetostratigraphic importance of secondary chemical remanent magnetizations carried by greigite (Fe (sub 3) S (sub 4) ) in Miocene sediments, New Jersey shelf (IODP Expedition 313)
2013
Geosphere
Geological Society of America, Boulder, CO, United States
9
3
510-520
Paleomagnetic and mineral magnetic analyses were carried out on Miocene clays from upper unit II at Sites M0027 and M0028 recovered during Integrated Ocean Drilling Program Expedition 313 on the New Jersey shallow shelf. A zone of mixed polarity in the lower section of Hole M0028A and dual overlapping magnetization components in upper Hole M0027A indicate that the sediments may have been chemically remagnetized during one or several events. Mineral magnetic investigations reveal that the magnetization is carried by the ferrimagnetic iron-sulfide greigite (Fe (sub 3) S (sub 4) ), possibly with traces of titanomagnetite. We find that several changes in polarity coincide with variations in magnetic mineral grain size and/or concentration. We interpret these variations as different stages of greigite growth, which were triggered by changes in pore-water chemistry and/or upward migration of methane.
English
Serial
Coverage:Geographic coordinates:
North:39.3803
West:-73.3718East: -73.2950
South:39.3357

Stratigraphy; anisotropy; Atlantic Ocean; Cenozoic; chemical remanent magnetization; continental shelf; cores; Expedition 313; greigite; Integrated Ocean Drilling Program; IODP Site M0027; IODP Site M0028; isothermal remanent magnetization; magnetic minerals; magnetic properties; magnetic susceptibility; magnetization; magnetostratigraphy; marine sediments; Miocene; Neogene; New Jersey; North Atlantic; Northwest Atlantic; paleomagnetism; remanent magnetization; sediments; sulfides; Tertiary; United States;

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