Early Neoproterozoic magmatism and Caledonian metamorphism recorded by the Mårma Terrane, Seve Nappe Complex, northern Swedish Caledonides
journal contributionposted on 2023-06-01, 11:34 authored by Riccardo Callegari, Karolina Kośmińska, Christopher J. Barnes, Iwona Klonowska, Abigail K. Barker, Sabine Rousku, Erika Nääs, Ellen Kooijman, Patrik Witt-Nilsson, Jarosław Majka
Figure S1. Geothermobarometry results for sample KB17-14b. Ellipses, both violet and light blue, indicate the garnet-biotite thermometer (GB) of Holdaway (2000) and the garnet-biotite-muscovite-plagioclase barometer (GBMP) of Wu (2015) for garnet core + biotite and muscovite inclusion in garnet + plagioclase core and garnet rim + biotite and muscovite in the matrix + plagioclase rim respectively. The green colored bar represents the calculation for the Ti-in-biotite thermometer of Wu and Chen (2015). The red- and yellow-colored bars represent the calculation for the Zr-in-rutile thermometer of Kohn (2020) for rutile inclusions in garnet and rutile in the matrix respectively.