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<datestamp>2018-01-11</datestamp>
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<title lang=en>Core complex mechanics: From the Gulf of Corinth to the Snake Range</title>
<creator>Chéry, Jean</creator>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0091-7613</source>
<source>EISSN: 0091-7613</source>
<source>Geology</source>
<publisher>Geological Society of America</publisher>
<identifier>hal-01419920</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01419920</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01419920</source>
<source>Geology, Geological Society of America, 2001, 29 (5), pp.439-442. 〈http://geology.gsapubs.org/content/29/5/439.full〉. 〈10.1130/0091-7613(2001)0292.0〉</source>
<identifier>DOI : 10.1130/0091-7613(2001)029<0439:CCMFTG>2.0</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1130/0091-7613(2001)029<0439:CCMFTG>2.0</relation>
<source>http://geology.gsapubs.org/content/29/5/439.full</source>
<language>en</language>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The activity of subhorizontal decollements mapped by geologists in extensional provinces is not explained by rock mechanics principles, which predict that only steep faults can slip. These exposed decollements are therefore suspected to be inactive; they may correspond to rotated, formerly active, high-angle faults. However, growing seismological evidence of earthquakes with low-angle fault-plane mechanisms has forced us to revisit this viewpoint. Using the example of the Gulf of Corinth in Greece, we propose a mechanical model that explains how a weak, high-angle fault may form a low-angle decollement at depth. This decollement is uplifted in a second stage of extension, which allows the exhumation of a metamorphic core complex such as the northern Snake Range, Nevada.</description>
<date>2001</date>
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