Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 2. Tasmanian Cainozoic basalts and the origins of intraplate basaltic magmas-Reference-Cited by-同舟云学术

Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 2. Tasmanian Cainozoic basalts and the origins of intraplate basaltic magmas

Published:2010-08-21 Issue:6 Volume:161 Page:883-899
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Adam John,Green Trevor

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-010-0570-7.pdf

Reference95 articles.

1. Adam J (1990) The geochemistry and experimental petrology of sodic alkaline basalts from Oatlands, Tasmania. J Petrol 31:1201–1223

2. Adam J, Green TH (2006) Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. experimental results and the investigation of controls on partitioning behaviour. Contrib Mineral Petrol 152:1–17

3. Afonso JC, Zlotnik S, Fernàndez M (2008) Effects of compositional and rheological stratifications on small-scale convection under the oceans: implications for the thickness of ocean lithosphere and seafloor flattening. Geophys Res Lett 35:L20308. doi: 10.1029/2008GL035419

4. Albarède F (1995) Introduction to geochemical modelling. Cambridge, Cambridge University Press, p 543

5. Aldanmaz E, Köprübaşi N, Gürer ÖF, Kaymakçi N, Gourgaud A (2006) Geochemical constraints on the Cenozioc, OIB-type alkaline volcanic rocks of NW Turkey: implications for mantle sources and melting processes. Lithos 86:50–76

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