Publisher: Elsevier

Related content
Volume 130, Number 3, 29 April 2002

< previous issue | all issues | next issue >

Favourites:Add to Favourites

A theoretical analysis of the observed variability of the geomagnetic dipole field
pp. 143-157(15)
Authors: Hoyng, P.; Schmitt, D.; Ossendrijver, M.A.J.H.

Favourites:Add to Favourites
Favourites:Add to Favourites

An integrated paleomagnetic study of Rio Grande de Santiago volcanic succession (trans-Mexican volcanic belt): revisited
pp. 175-194(20)
Authors: Goguitchaichvili, A.; Alva-Valdivia, L.; Rosas-Elguera, J.; Urrutia-Fucugauchi, J.; Gonzalez, J.A.; Morales, J.; Sole, J.

Favourites:Add to Favourites

Probing mid-mantle heterogeneity using PKP coda waves
pp. 195-208(14)
Authors: Hedlin, M.A.H.; Shearer, P.M.

Favourites:Add to Favourites

Sources of anomalous transient electric signals (ATESs) in the ULF band in the Lamia region (central Greece): electrochemical mechanisms for their generation
pp. 209-233(25)
Authors: Pham V.-N.; Boyer, D.; Chouliaras, G.; Savvaidis, A.; Stavrakakis, G.; Le Mouel, J.

Favourites:Add to Favourites

Crustal thickness, discontinuity depth, and upper mantle structure beneath southern Africa: constraints from body wave conversions
pp. 235-251(17)
Authors: Stankiewicz, J.; Chevrot, S.; van der Hilst, R.D.; de Wit, M.J.

Favourites:Add to Favourites

QLg tomography in Colombia
pp. 253-270(18)
Authors: Ojeda, A.; Ottemoller, L.

Favourites:Add to Favourites

Self-diffusion in liquid Fe at high pressure
pp. 271-284(14)
Author: Dobson, D.P.

Favourites:Add to Favourites

Interpretation of charging on fracture or frictional slip surface of rocks
pp. 285-291(7)
Authors: Takeuchi, A.; Nagahama, H.

Favourites:Add to Favourites

Contents Volume
pp. 293-294(2)

Share Content

Access Key

Free Content
Free content
New Content
New content
Open Access Content
Open access content
Subscribed Content
Subscribed content
Free Trial Content
Free trial content
Cookie Policy
X
Cookie Policy
ingentaconnect website makes use of cookies so as to keep track of data that you have filled in. I am Happy with this Find out more