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      <header>
        <identifier>doi:10.1594/pangaea.712634</identifier>
        <datestamp>2024-07-21T10:12:33Z</datestamp>
        <setSpec>PANGAEA</setSpec>
        <setSpec>PANGAEA.REPOSITORY</setSpec>
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      <metadata>
        <oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:title>Iridium contents and microprobe analyses of DSDP Leg 77 samples</dc:title>
          <dc:creator>Alvarez, Walter</dc:creator>
          <dc:creator>Smit, Jan</dc:creator>
          <dc:creator>Lowrie, William</dc:creator>
          <dc:creator>Asaro, Frank</dc:creator>
          <dc:creator>Margolis, Stanley V</dc:creator>
          <dc:creator>Claeys, Philippe</dc:creator>
          <dc:creator>Kastner, Miriam</dc:creator>
          <dc:creator>Hildebrand, Alan R</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>1992</dc:date>
          <dc:date>Issued: 1992</dc:date>
          <dc:relation>doi:10.1130/0091-7613(1992)020&lt;0697:pidatc&gt;2.3.co;2</dc:relation>
          <dc:subject>Drilling/drill rig</dc:subject>
          <dc:subject>Leg77</dc:subject>
          <dc:subject>Glomar Challenger</dc:subject>
          <dc:subject>Deep Sea Drilling Project (DSDP)</dc:subject>
          <dc:description>Restudy of Deep Sea Drilling Project Sites 536 and 540 in the southeast Gulf of Mexico gives evidence for a giant wave at Cretaceous-Tertiary boundary time. Five units are recognized: (1) Cenomanian limestone underlies a hiatus in which the five highest Cretaceous stages are missing, possibly because of catastrophic K-T erosion. (2) Pebbly mudstone, 45 m thick, represents a submarine landslide possibly of K-T age. (3) Current-bedded sandstone, more than 2.5 m thick, contains anomalous iridium, tektite glass, and shocked quartz; it is interpreted as ejecta from a nearby impact crater, reworked on the deep-sea floor by the resulting tsunami. (4) A 50-cm interval of calcareous mudstone containing small Cretaceous planktic foraminifera and the Ir peak is interpreted as the silt-size fraction of the Cretaceous material suspended by the impact-generated wave. (5) Calcareous mudstone with basal Tertiary forams and the uppermost tail of the Ir anomaly overlies the disturbed interval, dating the impact and wave event as K-T boundary age. Like Beloc in Haiti and Mimbral in Mexico, Sites 536 and 540 are consistent with a large K-T age impact at the nearby Chicxulub crater.</dc:description>
          <dc:description>Supplement to: Alvarez, Walter; Smit, Jan; Lowrie, William; Asaro, Frank; Margolis, Stanley V; Claeys, Philippe; Kastner, Miriam; Hildebrand, Alan R (1992): Proximal impact deposits at the Cretaceous-Tertiary boundary in the Gulf of Mexico: A restudy of DSDP Leg 77 Sites 536 and 540. Geology, 20(8), 697-700</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Collection</dc:type>
          <dc:type>Supplementary Publication Series of Datasets</dc:type>
          <dc:format>application/zip</dc:format>
          <dc:rights>Creative Commons Attribution 3.0 Unported</dc:rights>
          <dc:rights>https://creativecommons.org/licenses/by/3.0/legalcode</dc:rights>
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