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<identifier>oai:HAL:hal-00413047v1</identifier>
<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Rock magnetic and paleointensity results from Mesozoic baked contacts of Armenia</title>
<creator>Shcherbakova, V. V.</creator>
<creator>Perrin, Mireille</creator>
<creator>Shcherbakov, V. P.</creator>
<creator>Pavlov, V. E.</creator>
<creator>Ayvaz'Yan, A.</creator>
<creator>Zhidkov, G. V.</creator>
<contributor>Borok Geophysical Observatory (BGO) ; Schmidt Institute of Physics of the Earth [Moscow] (IPE) ; Russian Academy of Sciences [Moscow] (RAS) - Russian Academy of Sciences [Moscow] (RAS)</contributor>
<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>
<contributor>Schmidt Institute of Physics of the Earth [Moscow] (IPE) ; Russian Academy of Sciences [Moscow] (RAS)</contributor>
<contributor>Yerevan State University, Departament of Geology ; Université du Québec</contributor>
<description>International audience</description>
<source>ISSN: 1343-8832</source>
<source>Earth Planets and Space</source>
<publisher>Springer/Terra Scientific Publishing Company</publisher>
<identifier>hal-00413047</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00413047</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00413047</source>
<source>Earth Planets and Space, Springer/Terra Scientific Publishing Company, 2009, 61 (1), pp.23-39</source>
<language>en</language>
<subject lang=en>Paleointensity</subject>
<subject lang=en>Armenia</subject>
<subject lang=en>Cretaceous</subject>
<subject lang=en>baked contacts</subject>
<subject lang=en>Thellier method</subject>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Samples were obtained from three baked contacts and one lava flow along the upper Turonian-lower Coniacian Tovuz section, two baked contacts along the upper Coniacian-lower Santonian Paravakar section in the northern part of Armenia, and three baked contacts along the Titonian-Valanginian Kafan section in southern Armenia. A total of 130 samples were studied. Updated mean paleomagnetic poles were calculated for the Upper Cretaceous Tovuz-Paravakar sections (65.6 degrees N, 162.2 degrees E, A(95) = 4.3, paleolatitude = 27.0 +/- 3.4 degrees) and the Upper Jurassic-Lower Cretaceous Kafan section (61.7 degrees N, 158.9 degrees E, A(95) = 4.8 degrees, paleolatitude = 24.7 +/- 3.8 degrees). Paleointensity determinations could be estimated from two of the upper Cretaceous and three of the Upper Jurassic-Lower Cretaceous baked contacts, corresponding to a 30% success rate. The mean virtual dipole moments obtained were low (1.7-5.5 x 10(22) A m(2)), which is in agreement with data published by Bol'shakov and Solodovnikov (1981a, 1983) for the same sections (3.0-4.4 x 10(22) A m(2)). Our results support the hypothesis of the Mesozoic Dipole Low, even though the overall data arc widely dispersed.</description>
<date>2009</date>
</dc>
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