Characterization of geomagnetic field behaviour on timescales of centuries to millennia is necessary to understand the mechanisms that sustain the geodynamo and drive its evolution. As Holocene paleomagnetic and archeomagnetic data have become more abundant, strategies for regularized inversion of modern field data have been adapted to produce numerous time varying global field models. We evalu…

Tahun Terbit

2004

Edisi

Ed. 1 Cet. 1

ISBN/ISSN

979-3289-72-4

Deskripsi Fisik

ix, 330p., ; ill : 23 cm

No. Panggil

331.11 SON m