<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>An attempt to constrain the age, duration, and eruptive history of the Karoo flood basalt : Naude's Nek section (South Africa)</dc:title>
  <dc:creator>Moulin, M.</dc:creator>
  <dc:creator>Fluteau, F.</dc:creator>
  <dc:creator>Courtillot, V.</dc:creator>
  <dc:creator>Marsh, J.</dc:creator>
  <dc:creator>Delpech, G.</dc:creator>
  <dc:creator>Quidelleur, X.</dc:creator>
  <dc:creator>/G&#xE9;rard, Martine</dc:creator>
  <dc:creator>Jay, A. E.</dc:creator>
  <dc:description>We have carried out paleomagnetic sampling of a similar to 750 m sequence of the Karoo large igneous province (Naude's Nek Pass, South Africa). K-Ar dating (Cassignol-Gillot) has been performed on four samples from the 650 m upper unit (mean age 179.2 +/- 1.8 Ma) and a sample from the lower unit (184.8 +/- 2.6 Ma). A succession of two phases of volcanism is suggested. The lower 25 flows (115 m thick) have recorded a reversed polarity; the next 23 flows (135 m thick) are transitional and contribute a detailed record of the "Van Zijl" (1962) Jurassic reversal. The upper 38 flows (500 m thick) have normal polarity. Directional groups (DGs) of lava flows with quasi-identical remanence directions indicate eruption durations too short to have recorded geomagnetic secular variation and hence are interpreted as single eruptive events. Altogether, 19 DGs and 10 sheet lobes yield a sequence of 29 distinct directions. This could correspond to a total eruptive activity shorter than 3000 years, less than one per mil of the total duration over which the section was emplaced. We obtain a new paleomagnetic pole for South Africa at similar to 180 Ma (lambda = 75.2 degrees N, phi = 276.4 degrees E, A(95) = 5.8 degrees, N = 19), which is consistent with earlier reports.</dc:description>
  <dc:date>2011</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010053729</dc:identifier>
  <dc:identifier>fdi:010053729</dc:identifier>
  <dc:identifier>Moulin M., Fluteau F., Courtillot V., Marsh J., Delpech G., Quidelleur X., G&#xE9;rard Martine, Jay A. E.. An attempt to constrain the age, duration, and eruptive history of the Karoo flood basalt : Naude's Nek section (South Africa). 2011, 116, B07403</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
