Trace element transport rates in subduction zones: evidence from Th, Sr and Pb isotope data for Tonga-Kermadec arc lavas
- 1 August 1997
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 150 (3-4) , 291-302
- https://doi.org/10.1016/s0012-821x(97)00107-6
Abstract
No abstract availableThis publication has 39 references indexed in Scilit:
- The origin of Samoa: new evidence from Sr, Nd, and Pb isotopesPublished by Elsevier ,2002
- Lithospheric Contributions to Arc Magmatism: Isotope Variations Along Strike in Volcanoes of Honshu, JapanScience, 1996
- Cerium/lead and lead isotope ratios in arc magmas and the enrichment of lead in the continentsNature, 1994
- Thorium-Uranium Fractionation by Garnet: Evidence for a Deep Source and Rapid Rise of Oceanic BasaltsScience, 1993
- Trace element models for mantle melting: application to volcanic arc petrogenesisGeological Society, London, Special Publications, 1993
- Th, Pb, and Sr isotope variations in young island arc volcanics and oceanic sedimentsEarth and Planetary Science Letters, 1991
- Uranium and 10Be enrichments by fluids in Andean arc magmasNature, 1990
- The subducted component in island arc lavas: constraints from Be isotopes and B–Be systematicsNature, 1990
- Seismotectonics and present-day relative plate motions in the Tonga-Lau and Kermadec-Havre regionTectonophysics, 1989
- 10Be in island-arc volcanoes and implications for subductionNature, 1982