minerals Article Apatite from NWA 10153 and NWA 10645—The Key to Deciphering Magmatic and Fluid Evolution History in Nakhlites Łukasz Birski 1,*, Ewa Słaby 1, Elias Chatzitheodoridis 2, Richard Wirth 3, Katarzyna Majzner 4, Gabriela A. Kozub-Budzy ´n 5, Jiˇrí Sláma 6, Katarzyna Liszewska 1, Izabela Kocjan 7 and Anna Zagórska 7 1 Institute of Geological Sciences, Polish Academy of Sciences, Research Centre in Warsaw, Twarda 51/55, 00-818 Warsaw, Poland;
[email protected] (E.S.);
[email protected] (K.L.) 2 Department of Geological Sciences, School of Mining and Metallurgical Engineering, National Technical University of Athens, 9 Heroon Polytechneiou, 15780 Zografou, Athens, Greece;
[email protected] 3 Helmholtz-Zentrum Potsdam Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany;
[email protected] 4 Faculty of Chemistry, Jagiellonian University, Raman Imaging Group, Gronostajowa 2, 30-387 Cracow, Poland;
[email protected] 5 Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Mickiewicza 30, 30-059 Cracow, Poland;
[email protected] 6 Institute of Geology Academy of Sciences of the Czech Republic Rozvojová 269, 165 00 Prague Czech Republic;
[email protected] 7 Institute of Geological Sciences, Polish Academy of Sciences, Research Centre in Cracow, Senacka 1, 31-002 Cracow, Poland;
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[email protected] (A.Z.) * Correspondence:
[email protected] Received: 10 September 2019; Accepted: 7 November 2019; Published: 10 November 2019 Abstract: Apatites from Martian nakhlites NWA 10153 and NWA 10645 were used to obtain insight into their crystallization environment and the subsequent postcrystallization evolution path.