@article{10272/8356,
year = {2007},
url = {http://hdl.handle.net/10272/8356},
abstract = {A paleointensity study has been carried out on samples from 13 volcanic sites belonging to four different
types of volcanism of late Miocene to Pliocene age from south-eastern Spain. Rock-magnetic experiments
including measurement of thermomagnetic curves and hysteresis parameters as well as ore microscopy
showed that the main carriers of remanence were low-Ti titanomagnetite and titanohematite. A PSD
domain structure was observed in most samples. 43 of 90 samples from only 7 sites provided successful
paleointensity determinations. 4 sites yield very low paleointensity values, but only in sites M4 and G15
anomalous paleomagnetic directions confirm an intermediate polarity. Lamproitic and calc-alkaline volcanics
proved to be more suitable for paleointensity determinations in this area},
title = {Estudio preliminar de la paleointensidad de rocas volcánicas del Mioceno superior y Plioceno del sudeste de la Península Ibérica},
title = {Preliminary paleointensity determinations on late Miocene and Pliocene volcanic rocks from south eastern Spain},
author = {Calvo Rathert, M. and Vegas, Néstor and Gogichaichvili, A.},
}