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<dc:title>Magnetic dating of the Holocene monogenetic Tkarsheti volcano in the Kazbeki region (Great Caucasus)</dc:title>
<dc:creator>Vashakidze, Goga</dc:creator>
<dc:creator>Goguitchaichvili, Avto</dc:creator>
<dc:creator>García Redondo, Natalia</dc:creator>
<dc:creator>Calvo Rathert, Manuel</dc:creator>
<dc:creator>Carrancho Alonso, Ángel</dc:creator>
<dc:creator>Cejudo, Ruben</dc:creator>
<dc:creator>Morales, Juan Ignacio .</dc:creator>
<dc:creator>Lebedev, Vladimir A.</dc:creator>
<dc:creator>Gabarashvili, Ketino</dc:creator>
<dc:subject>Great Caucasus</dc:subject>
<dc:subject>Monogenetic volcano</dc:subject>
<dc:subject>Kazbeki</dc:subject>
<dc:subject>Magnetic dating</dc:subject>
<dc:description>The radiocarbon technique is widely used to date Late Pleistocene and Holocene lava flows. The significant difference&#xd;
with palaeomagnetic methods is that the 14C dating is performed on the organic matter carbonized by the rock&#xd;
formation or the paleosols found within or below the lava flow. On the contrary, the archaeomagnetic dating allows&#xd;
to date the moment when the lava is cooling down below the Curie temperatures. In the present study, we use the&#xd;
paleomagnetic dating to constrain the age of the Tkarsheti monogenetic volcano located within the Kazbeki Volcanic&#xd;
Province (Great Caucasus). A series of rock-magnetic experiments including the measurement of hysteresis curves,&#xd;
isothermal remanence, back-field and continuous thermomagnetic curves were applied. These experiments indicated&#xd;
that Pseudo-Single-Domain Ti-poor titanomagnetite is responsible for remanence. A characteristic remanent magnetization&#xd;
was obtained for all twenty analyzed samples yielding a stable single magnetization component observed&#xd;
upon both thermal and alternating field treatments. Comparison of the mean directions obtained (Inc = 48.6º,&#xd;
Dec = 6.4º, A95&#xd;
= 4.0° and K = 67) with the SCHA.DIF.14k model yielded two main time intervals (4740–4650 or 4427–&#xd;
4188 BC) as the best age estimate of the Lesser Tkarsheti lava flow. These results suggest an earlier age (between&#xd;
approximately 200 and 700 years) for this monogenetic lava flow than expected from the estimated age provided by&#xd;
a former 14C dating obtained in 1973 on woody remains. This first attempt to use the archaeomagnetic technique in&#xd;
the Caucasus indicates that the SCHA.DIF.14k geomagnetic model may be successfully used for dating purposes in&#xd;
the region.</dc:description>
<dc:date>2021-11-04T13:13:15Z</dc:date>
<dc:date>2021-11-04T13:13:15Z</dc:date>
<dc:date>2019-12</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:identifier>1343-8832</dc:identifier>
<dc:identifier>http://hdl.handle.net/10259/6105</dc:identifier>
<dc:identifier>10.1186/s40623-019-1109-4</dc:identifier>
<dc:language>eng</dc:language>
<dc:relation>Earth, Planets and Space. 2019, V. 71, 133</dc:relation>
<dc:relation>https://doi.org/10.1186/s40623-019-1109-4</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/Junta de Castilla y León//BU066U16//Estudio arqueomagnéticos y de propiedades magnéticas en registros de fuegos antrópicos prehistóricos. Aplicaciones a la arqueología</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/Junta de Castilla y León//BU235P18//Análisis arqueomagnéticos en materiales arqueológicos quemados de edad holocena y pleistocena</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/CONACYT//252149/MX</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/UNAM//101717/MX</dc:relation>
<dc:rights>http://creativecommons.org/licenses/by/4.0/</dc:rights>
<dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
<dc:rights>Atribución 4.0 Internacional</dc:rights>
<dc:publisher>Springer</dc:publisher>
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