A self-consistent top–down model for differentiation in bimodal suites: application to the Sonju Lake Intrusion–Finland granite system (MN)
Author:
Affiliation:
1. Department of Geology, University of Illinois Urbana Champaign, Champaign, IL, USA
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2016.1276866
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1. Implications of incremental emplacement of magma bodies for magma differentiation, thermal aureole dimensions and plutonism–volcanism relationships
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3. Inter-mineral Fe isotope variations in mantle-derived rocks and implications for the Fe geochemical cycle
4. Comment on “Heavy iron isotope composition of granites determined by high resolution MC-ICP-MS”, by F. Poitrasson and R. Freydier [Chem. Geol. 222 132–147]
5. Stable isotope fractionation by thermal diffusion through partially molten wet and dry silicate rocks
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1. Reply to Müntener and Baumgartner comment on: ‘Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton’;Contributions to Mineralogy and Petrology;2019-05-31
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