40Ar/ 39Ar ages and paleomagnetism of São Miguel lavas, Azores

• Published in: Earth and planetary science letters Vol. 160; no. 3; pp. 637 - 649
• Main Authors: Johnson, Catherine L., Wijbrans, Jan R., Constable, Catherine G., Gee, Jeff, Staudigel, Hubert, Tauxe, Lisa, Forjaz, Victor-H., Salgueiro, Mário
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-08-1998
• Subjects: absolute age; Ar-40/Ar-39; Azores; magnetic field; paleomagnetism; secular variations; absolute age; magnetic field; Ar-40/Ar-39; secular variations; Azores; paleomagnetism
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/S0012-821X(98)00117-4

We present new
40Ar/
39Ar ages and paleomagnetic data for São Miguel island, Azores. Paleomagnetic samples were obtained for 34 flows and one dike; successful mean paleomagnetic directions were obtained for 28 of these 35 sites.
40Ar/
39Ar age determinations on 12 flows from the Nordeste complex were attempted successfully: ages obtained are between 0.78 Ma and 0.88 Ma, in contrast to published K–Ar ages of 1 Ma to 4 Ma. Our radiometric ages are consistent with the reverse polarity paleomagnetic field directions, and indicate that the entire exposed part of the Nordeste complex is of a late Matuyama age. The duration of volcanism across São Miguel is significantly less than previously believed, which has important implications for regional melt generation processes, and temporal sampling of the geomagnetic field. Observed stable isotope and trace element trends across the island can be explained, at least in part, by communication between different magma source regions at depth. The
40Ar/
39Ar ages indicate that our normal polarity paleomagnetic data sample at least 0.1 Myr (0–0.1 Ma) and up to 0.78 Myr (0–0.78 Ma) of paleosecular variation and our reverse polarity data sample approximately 0.1 Myr (0.78–0.88 Ma) of paleosecular variation. Our results demonstrate that precise radiometric dating of numerous flows sampled is essential to accurate inferences of long-term geomagnetic field behavior. Negative inclination anomalies are observed for both the normal and reverse polarity time-averaged field. Within the data uncertainties, normal and reverse polarity field directions are antipodal, but the reverse polarity field shows a significant deviation from a geocentric axial dipole direction.