Publisher: Elsevier

Related content
Volume 155, Number 1, 15 February 1998

< previous issue | all issues | next issue >

Favourites:Add to Favourites

Paleomagnetic confirmation of the Laurentian origin of the Argentine Precordillera
pp. 1-14(14)
Authors: Seselja, B.; Tepavcevic, A.; Rapalini, A.E.; Astini, R.A.

Favourites:Add to Favourites

Secular variation of Nd and Pb isotopes in ferromanganese crusts from the Atlantic, Indian and Pacific Oceans
pp. 15-28(14)
Authors: Xiaoyun, L.; Wang, D.; Wong, C.K.; O'Nions, R.K.; Frank, M.; von Blanckenburg, F.; Ling, H.

Favourites:Add to Favourites

Radiometrically determined sedimentary fluxes in the sub-polar North Atlantic during the last 140,000 years
pp. 29-43(15)
Authors: Savage, C.D.; Zhang, C.; McManus, J.F.; Anderson, R.F.; Broecker, W.S.; Fleisher, M.Q.; Higgins, S.M.

Favourites:Add to Favourites
Favourites:Add to Favourites

Oceanic plateau model for continental crustal growth in the Archaean: A case study from the Kostomuksha greenstone belt, NW Baltic Shield
pp. 57-74(18)
Authors: Raghunathan, T.T.; Shikare, M.M.; Waphare, B.N.; Puchtel, I.S.; Hofmann, A.W.; Mezger, K.; Jochum, K.P.; Shchipansky, A.A.; Samsonov, A.V.

Favourites:Add to Favourites

Regular vs. chaotic mantle mixing
pp. 75-86(12)
Authors: Zhang, F.; Lin, G.; Ferrachat, S.; Ricard, Y.

Favourites:Add to Favourites

The effect of convection planform on the toroidal-poloidal energy ratio
pp. 87-95(9)
Authors: El-Zahar, M.H.; Fateen, L.A.; Weinstein, S.A.

Favourites:Add to Favourites

Holocene sea-level change and ice-sheet history in the Vestfold Hills, East Antarctica - A high-resolution, high-precision model
pp. 131-145(15)
Authors: Beifang, C.; Sanming, Z.; Zwartz, D.; Bird, M.; Stone, J.; Lambeck, K.

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
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