17 results on '"Palencia-Ortas, A."'
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2. Rapid Intensity Decrease During the Second Half of the First Millennium BCE in Central Asia and Global Implications
3. Inclination flattening effect in highly anisotropic archaeological structures from Iberia. Influence on archaeomagnetic dating
4. Refining geomagnetic field intensity changes in Europe between 200 CE and 1800 CE. New data from the Mediterranean region
5. Rapid intensity variations during the second half of the first millennium BCE in Central Asia and global implications.
6. Geomagnetic field intensity changes in the Central Mediterranean between 1500 BCE and 150 CE: Implications for the Levantine Iron Age Anomaly evolution
7. Further progress in the study of epsilon iron oxide in archaeological baked clays
8. Two archaeomagnetic intensity maxima and rapid directional variation rates during the Early Iron Age observed at Iberian coordinates. Implications on the evolution of the Levantine Iron Age Anomaly
9. Revisiting the chronology of the Early Iron Age in the north-eastern Iberian Peninsula
10. Updated Iberian Archeomagnetic Catalogue: New Full Vector Paleosecular Variation Curve for the Last Three Millennia
11. New archaeomagnetic directions from Portugal and evolution of the geomagnetic field in Iberia from Late Bronze Age to Roman Times
12. A new 200 Ma paleomagnetic pole for Africa, and paleo-secular variation scatter from Central Atlantic Magmatic Province (CAMP) intrusives in Morocco (Ighrem and Foum Zguid dykes)
13. The evolution of Iberia during the Jurassic from palaeomagnetic data
14. Palaeomagnetic and AMS study of the Tarfaya coastal basin, Morocco: an early Turonian palaeopole for the African plate
15. The base of the Toarcian (Early Jurassic) in the Almonacid de la Cuba section (Spain). Ammonite biostratigraphy, magnetostratigraphy and isotope stratigraphy
16. Magma flow, exsolution processes and rock metasomatism in the Great Messejana-Plasencia dyke (Iberian Peninsula)
17. Paleomagnetic study of the Messejana Plasencia dyke (Portugal and Spain): A lower Jurassic paleopole for the Iberian plate
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