<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" 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:contributor>A. Weislogel</dc:contributor>
  <dc:contributor>N.J. Drinkwater</dc:contributor>
  <dc:contributor>T. McHargue</dc:contributor>
  <dc:contributor>A. Tankard</dc:contributor>
  <dc:contributor>J. Wooden</dc:contributor>
  <dc:contributor>D. Hodgson</dc:contributor>
  <dc:contributor>S. Flint</dc:contributor>
  <dc:creator>A. Fildani</dc:creator>
  <dc:date>2009</dc:date>
  <dc:description>U-Pb ages determined using sensitive high-resolution ion microprobe-reverse geometry on 205 single-grain zircons from 16 ash beds within submarine fan deposits of the Ecca Group provide the first evidence of a marine Permian-Triassic (P-T) boundary in the Karoo Basin of South Africa. These U-Pb ages provide an objective basis for correlating the deep-marine sediments of the southwest Karoo Basin with fluvial-deltaic deposits in the central and eastern parts of the basin where the P-T boundary is recorded in a diverse macrofauna. Furthermore, these new zircon ages and their correlation imply asymmetric subsidence and variable sedimentation rates across the basin. ?? 2009 Geological Society of America.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/G25685A.1</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>U-Pb zircon ages from the southwestern Karoo Basin, South Africa - Implications for the Permian-Triassic boundary</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>