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<field name="value">Calvo Rathert, Manuel</field>
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<field name="confidence">500</field>
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<field name="value">Morales Contreras, Juan J.</field>
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<field name="confidence">500</field>
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<field name="value">Carrancho Alonso, Ángel</field>
<field name="authority">104</field>
<field name="confidence">500</field>
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<field name="value">Goguitchaichvili, Avto</field>
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<field name="value">2017-09-06T11:19:41Z</field>
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<field name="value">2017-09-06T11:19:41Z</field>
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<field name="value">2016-09</field>
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<field name="value">1525-2027</field>
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<field name="value">10.1002/2016GC006396</field>
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<field name="value">Sixteen Miocene, Pleistocene, and historic lava flows have been sampled in Lanzarote (Canary&#xd;
Islands) for paleointensity analysis with both the Coe and multispecimen methods. Besides obtaining new&#xd;
data, the main goal of the study was the comparison of paleointensity results determined with two different&#xd;
techniques. Characteristic Remanent Magnetization (ChRM) directions were obtained in 15 flows, and&#xd;
12 were chosen for paleointensity determination. In Thellier-type experiments, a selection of reliable&#xd;
paleointensity determinations (43 of 78 studied samples) was performed using sets of criteria of different&#xd;
stringency, trying to relate the quality of results to the strictness of the chosen criteria. Uncorrected and&#xd;
fraction and domain-state corrected multispecimen paleointensity results were obtained in all flows. Results&#xd;
with the Coe method on historical flows either agree with the expected values or show moderately lower&#xd;
ones, but multispecimen determinations display a large deviation from the expected result in one case. No&#xd;
relation can be detected between correct or anomalous results and paleointensity determination quality or&#xd;
rock-magnetic properties. However, results on historical flows suggest that agreement between both&#xd;
methods could be a good indicator of correct determinations. Comparison of results obtained with both&#xd;
methods on seven Pleistocene flows yields an excellent agreement in four and disagreements in three&#xd;
cases. Pleistocene determinations were only accepted if either results from both methods agreed or a result&#xd;
was based on a sufficiently large number (n>4) of individual Thellier-type determinations. In most&#xd;
Pleistocene flows, a VADM around 5 31022 Am2 was observed, although two flows displayed higher values&#xd;
around 931022 Am2.</field>
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<field name="value">project&#xd;
CGL2012-32149 (Ministerio de&#xd;
Econom ıa y Competitividad, Spain),&#xd;
project 320/2011 (Ministerio de Medio&#xd;
Ambiente y Medio Rural y Marino,&#xd;
Spain) and the European Regional&#xd;
Development Fund (ERDF).</field>
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<field name="value">eng</field>
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<field name="value">American Geophysical Union (AGU)</field>
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<field name="value">Geochemistry, Geophysics, Geosystems. 2016, V. 17, n. 9, p. 3638–3654</field>
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<field name="value">http://dx.doi.org/10.1002/2016GC006396</field>
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<field name="value">Magnetism</field>
<field name="value">Paleontology</field>
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<element name="es">
<field name="value">Magnetismo</field>
<field name="value">Paleontología</field>
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<field name="value">A comparison of Thellier-type and multispecimen paleointensity determinations on Pleistocene and historical lava flows from Lanzarote (Canary Islands, Spain)</field>
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<field name="value">2016 AGU</field>
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