minerals Article New Mineral with Modular Structure Derived from Hatrurite from the Pyrometamorphic Rocks of the Hatrurim Complex: Ariegilatite, BaCa12(SiO4)4(PO4)2F2O, from Negev Desert, Israel Evgeny V. Galuskin 1,*, Biljana Krüger 2 ID , Irina O. Galuskina 1, Hannes Krüger 2 ID , Yevgeny Vapnik 3, Justyna A. Wojdyla 4 and Mikhail Murashko 5 1 Faculty of Earth Sciences, Department of Geochemistry, Mineralogy and Petrography, University of Silesia, B˛edzi´nska60, 41-200 Sosnowiec, Poland;
[email protected] 2 Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria;
[email protected] (B.K.);
[email protected] (H.K.) 3 Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, P.O. Box 653, Beer-Sheva 84105, Israel;
[email protected] 4 Swiss Light Source, Paul Scherrer Institute, 5232 Villigen, Switzerland;
[email protected] 5 Saint Petersburg State University, Faculty of Geology, 7-9 Universitetskaya nab., St. Petersburg 199034, Russia;
[email protected] * Correspondence:
[email protected]; Tel.: +48-32-3689365 Received: 19 February 2018; Accepted: 5 March 2018; Published: 8 March 2018 3 Abstract: Ariegilatite, BaCa12(SiO4)4(PO4)2F2O(R3m, a = 7.1551(6) Å, c = 41.303(3) Å, V = 1831.2(3) Å , Z = 3), is a new member of the nabimusaite group exhibiting a modular intercalated antiperovskite structure derived from hatrurite. It was found in a few outcrops of pyrometamorphic rocks of the Hatrurim Complex located in the territories of Israel, Palestine and Jordan. The holotype specimen is an altered spurrite marble from the Negev Desert near Arad city, Israel.