We present new Ar-40/Ar-39 ages and paleomagnetic data for Sao Miguel
island, Azores. Paleomagnetic samples were obtained for 34 flows and o
ne dike; successful mean paleomagnetic directions were obtained for 28
of these 35 sites. Ar-40/Ar-39 age determinations on 12 flows from th
e Nordeste complex were attempted successfully: ages obtained are betw
een 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 p
aleomagnetic field directions, and indicate that the entire exposed pa
rt of the Nordeste complex is of a late Matuyama age. The duration of
volcanism across Sao Miguel is significantly less than previously beli
eved, which has important implications for regional melt generation pr
ocesses, and temporal sampling of the geomagnetic field. Observed stab
le isotope and trace element trends across the island can be explained
, at least in part, by communication between different magma source re
gions at depth. The Ar-40/Ar-39 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 dat
a sample approximately 0.1 Myr (0.78-0.88 Ma) of paleosecular variatio
n. Our results demonstrate that precise radiometric dating of numerous
flows sampled is essential to accurate inferences of long-term geomag
netic field behavior. Negative inclination anomalies are observed for
both the normal and reverse polarity time-averaged field. Within the d
ata uncertainties, normal and reverse polarity field directions are an
tipodal, but the reverse polarity field shows a significant deviation
from a geocentric axial dipole direction. (C) 1998 Elsevier Science B.
V. All rights reserved.