2007
DOI: 10.1016/j.margeo.2007.04.002
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Paleocurrent directions from paleomagnetic reorientation of magnetic fabrics in deep-sea sediments at the Antarctic Peninsula Pacific margin (ODP Sites 1095, 1101)

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Cited by 85 publications
(52 citation statements)
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“…On our profile, the diagram of maximum susceptibility axis direction was focused toward 310 • (Figure 5F), indicating that the weathered material mainly came from this direction (Parés et al, 2007). Materials transported by the Pear River are main candidates.…”
Section: Chemical Weathering Intensity and Terrigenous Fluxmentioning
confidence: 77%
“…On our profile, the diagram of maximum susceptibility axis direction was focused toward 310 • (Figure 5F), indicating that the weathered material mainly came from this direction (Parés et al, 2007). Materials transported by the Pear River are main candidates.…”
Section: Chemical Weathering Intensity and Terrigenous Fluxmentioning
confidence: 77%
“…Although paleocurrents may also produce a relatively well-defined magnetic lineation (e.g., Rees and Woodall, 1975;Parés et al, 2007) Furthermore, sites CJ05, CJ06, and CJ07 lie along the crest of a ~E-W trending, westward plunging syncline (Fig. 3).…”
Section: Late Cretaceous-late Eocene Tectonic Regime In the Magallanementioning
confidence: 99%
“…Paleomagnetic core reorientation has been successfully used for a number of years (e.g., Fuller, 1969;Kodama, 1984;Shibuya et al, 1991;Parés et al, 2007). The procedure is based on determining the direction of stable remanent magnetization (either viscous remanent magnetization or primary magnetization) with respect to a common reference line that is marked lengthwise along the core.…”
Section: Paleomagnetic Reorientation Of Coresmentioning
confidence: 99%