Journal article Open Access

Direct evidence of ancient shock metamorphism at the site of the 1908 Tunguska event

Vannucchi, Paola; Morgan, Jason P.; Della Lunga, Damiano; Andronicos, Christopher L.; Morgan, W. Jason

DataCite XML Export

<?xml version='1.0' encoding='utf-8'?>
<resource xmlns:xsi="" xmlns="" xsi:schemaLocation="">
  <identifier identifierType="URL"></identifier>
      <creatorName>Vannucchi, Paola</creatorName>
      <creatorName>Morgan, Jason P.</creatorName>
      <givenName>Jason P.</givenName>
      <creatorName>Della Lunga, Damiano</creatorName>
      <familyName>Della Lunga</familyName>
      <creatorName>Andronicos, Christopher L.</creatorName>
      <givenName>Christopher L.</givenName>
      <creatorName>Morgan, W. Jason</creatorName>
      <givenName>W. Jason</givenName>
    <title>Direct evidence of ancient shock metamorphism at the site of the 1908 Tunguska event</title>
    <date dateType="Issued">2015-01-01</date>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
    <alternateIdentifier alternateIdentifierType="url"></alternateIdentifier>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1016/j.epsl.2014.11.001</relatedIdentifier>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
    <description descriptionType="Abstract">Shock metamorphism is rarely found at the surface of the Earth. The most used structures to identify shock metamorphism are "true Planar Deformation Features" (PDFs) in quartz, now accepted as diagnostic indicators of a meteorite impact. Here we present several lines of evidence for shock metamorphism and PDFs developed in quartz occurring on samples centered on a circular geological structure on Mount Stojkovic (60°54′06″N; 101°55′40″E), which lies within southern surface exposures of the Siberian Traps. The shock event appears to have occurred during the eruption of the surface Siberian Traps basalts that cover this region. Curiously, Mount Stojkovic lies within ∼3 km of the tree fall epicenter of the 1908 Tunguska event. Based on current estimates of the Phanerozoic impact distribution, there is at most a 1 in ∼17 000 chance that the 1908 bolide would randomly fall on the site of a previous impact structure capable of creating shocked quartz. Just as improbable would be an airbust event, incapable of creating a small crater, that could have produced shock metamorphism. Our preferred least implausible hypothesis is that the shock-metamorphism here was associated with a terrestrial event, a hyperexplosive volcanic gas eruption called 'Verneshot'.</description>
Views 332
Downloads 393
Data volume 2.2 GB
Unique views 324
Unique downloads 359


Cite as