georefid:2001-002890georefid:2001-002879SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2973/odp.proc.sr.166.129.20002000-01-01publicationgeorefid:2001-002890doi:10.2973/odp.proc.sr.166.129.2000McNeill, Donald F.Rosenstiel School of Marine and Atmospheric Science, Comparative Sedimentology Laboratory, Miami, FL, United StatesauthorKislak, Jason I.Ocean Drilling Program, United StatesauthorTexas A & M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Swart, Peter K., Eberli, Gregor P., Malone, Mitchell J., Anselmetti, Flavio S., Arai, Kohsaku, Bernet, Karin H., Betzler, Christian, Christensen, Beth A., De Carlo, Eric Heinen, Dejardin, Pascale M., Emmanuel, Laurent, Frank, Tracy D., Haddad, Geoffrey A., Isern, Alexandra R., Katz, Miriam E., Kenter, Jeroen A. M., Kramer, Philip A., Kroon, Dick, McKenzie, Judith A., McNeill, Donald F., Montgomery, Paul, Nagihara, Seiichi, Pirmez, Carlos, Reijmer, John J. G., Sato, Tokiyuki, Schovsbo, Niels H., Williams, Trevor, Wright, James D., Lowe, Ginny (editor), Proceedings of the Ocean Drilling Program, scientific results, Bahamas Transect; covering Leg 166 of the cruises of the drilling vessel JOIDES Resolution, San Juan, Puerto Rico, to Balboa Harbor, Panama, sites 1003-1009, 17 February-10 April 1996166123-127Paleomagnetic analyses from discrete samples of carbonate sediment from Hole 1006A were completed to assess the nature of magnetic remanence and to evaluate the use of directional data for a magnetic reversal stratigraphy. Magnetic remanence in these carbonates was moderate to weak but was stable enough to reliably identify polarity in 26.7% of the samples. The remaining 73.3% samples were judged either too weak or unstable, or else they exhibited a very steep inclination interpreted to be the result of some type of drilling overprint. Thus, magnetic polarity data from Hole 1006A should be used with caution. The nature of magnetic remanence and some reconnaissance acquisition tests suggest that single-domain magnetite (with some possible alteration to maghemite) is the dominant source of the remanent magnetization.completedStratigraphyalternating field demagnetizationAtlantic Oceancarbonate sedimentsCaribbean SeaCenozoicdemagnetizationisothermal remanent magnetizationLeg 166magnetic susceptibilitymagnetizationmagnetostratigraphymarine sedimentsmineral compositionnatural remanent magnetizationNorth AtlanticOcean Drilling ProgramODP Site 1006paleomagnetismremanent magnetizationreversalssedimentsurn:org.iodp:exp:166urnlargerWorkCitationcampaignurn:org.iodp:exp:166:site:1006urnlargerWorkCitationstudyurn:org.iodp:exp:166urnlargerWorkCitationcampaignEnglishgeoscientificInformation-79.2733-79.273324.235924.2359Data reportapplication/pdfunknownSEDIS Publication Catalogue

ana.macario@awi.de

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