The petrogenesis of highly fractionated gem-bearing pegmatites of Malawi: evidence from mica and tourmaline chemistry and finite step trace element modelling
Author:
Funder
CIMERA
Glencore
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics,Economic Geology
Link
https://link.springer.com/content/pdf/10.1007/s00126-023-01236-1.pdf
Reference76 articles.
1. Adam J, Green T (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
2. Andreoli MAG (1984) Petrochemistry, tectonic evolution and metasomatic mineralisations of Mozambique belt granulites from S Malawi and Tete (Mozambique). Precambrian Res 25:161–186. https://doi.org/10.1016/0301-9268(84)90031-7
3. Ashwal LD, Armstrong RA, Roberts RJ et al (2007) Geochronology of zircon megacrysts from nepheline-bearing gneisses as constraints on tectonic setting: Implications for resetting of the U-Pb and Lu-Hf isotopic systems. Contrib Mineral Petrol 153:389–403. https://doi.org/10.1007/s00410-006-0153-9
4. Ashworth L, Kinnaird JA, Nex PAM et al (2020) Origin of rare-element-mineralized Damara Belt pegmatites: A geochemical and light stable isotope study. Lithos 372–373:105655. https://doi.org/10.1016/J.LITHOS.2020.105655
5. Bea F, Pereira MD, Corretgé LG, Fershtater GB (1994) Differentiation of strongly peraluminous, perphosphorus granites: the Pedrobernardo pluton, central Spain. Geochim Cosmochim Acta 58:2609–2627
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1. Correction to: The petrogenesis of highly fractionated gem‑bearing pegmatites of Malawi: evidence from mica and tourmaline chemistry and finite step trace element modelling;Mineralium Deposita;2023-12-19
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