Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/46246
Title: The Mono Lake excursion recorded in phonolitic lavas from Tenerife (Canary Islands): Paleomagnetic analyses and coupled K/Ar and Ar/Ar dating
Authors: Kissel, C.
Guillou, H.
Laj, C.
Carracedo, J. C. 
Nomade, S.
Perez-Torrado, F. 
Wandres, C.
UNESCO Clasification: 250621 Vulcanología
Keywords: Mono Lake excursion
Paleomagnetism
Dating
Time scale
Issue Date: 2011
Publisher: 0031-9201
Journal: Physics of the Earth and Planetary Interiors 
Abstract: We present a coupled paleomagnetic/dating investigation conducted on three different lava flows from the island of Tenerife (Canary Islands; Spain) erupted during the Mono Lake excursion (MLE). Paleomagnetic analyses consist in zero field demagnetizations (AF and/or thermal) and of Thellier and Thellier experiments using the PICRIT-03 set of criteria to select reliable intensity determinations. One of the flows is characterized by a direction largely deviated from the one expected from an axial geocentric dipole (GAD) field. Its paleointensity value is very low (7.8 μT). The two other sites are characterized by inclinations slightly shallower than the GAD value and by low intensity values (about 12 and 21 μT; present value: 38 μT). The three K/Ar ages combined with two 40Ar/39Ar ages range from 32.0 to 33.2 ka and they are not statistically distinguishable from one another. It therefore appears that these lavas have recorded the MLE (the only excursion in this time interval) confirming its brief duration (shorter than the minimum age uncertainties available). The mean age is younger but, within the uncertainties, consistent with the age of the 10Be peak and of the marine intensity low when reported in the most recent ice age model. These new results are the first ones with radiometric dating produced from the northern hemisphere. Combined with existing cosmogenic, marine and volcanic paleomagnetic data, these results are discussed in terms of dating, and geometry of the earth magnetic field during the excursion.
URI: http://hdl.handle.net/10553/46246
ISSN: 0031-9201
DOI: 10.1016/j.pepi.2011.04.014
Source: Physics of the Earth and Planetary Interiors [ISSN 0031-9201], v. 187, p. 232-244
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