Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 27 September 2018 doi:10.20944/preprints201809.0551.v1 Peer-reviewed version available at Minerals 2018, 8, 537; doi:10.3390/min8110537 Article Mineralogical and Geochemical Constraints on the Origin and Late-Stage Crystallization History of the Breivikbotn Silicocarbonatite, Seiland Igneous Province in Northern Norway: Prerequisites for Zeolite Deposits in Carbonatite Complexes Dmitry R. Zozulya 1,*, Kåre Kullerud 2,3, Erling K. Ravna 2, Yevgeny E. Savchenko 1, Ekaterina A. Selivanova 1 and Marina G. Timofeeva 1 1 Geological Institute, Kola Science Centre, 14 Fersman Str, 184209 Apatity, Russia 2 Department of Geology, University of Tromsø, N-9037 Tromsø, Norway 3 Norwegian Mining Museum, N-3616 Kongsberg, Norway * Correspondence:
[email protected]; Tel.: +7-81555-79742 Abstract: The present work reports new mineralogical and whole rock geochemical data from the Breivikbotn silicocarbonatite (Seiland igneous province, North Norway), allowing conclusions to be drawn concerning its origin and the role of late fluid alteration. The rock shows a rare mineral association: calcite + pyroxene + amphibole + zeolite group minerals + garnet + titanite, with apatite, allanite, magnetite and zircon as minor and accessory minerals, and it is classified as silicocarbonatite. Calcite, titanite and pyroxene (Di36-46 Acm22-37 Hd14-21) are primarily magmatic minerals. Amphibole of hastingsitic composition has formed after pyroxene at a late-magmatic stage. Zeolite group minerals (natrolite, gonnardite, Sr-rich thomsonite-(Ca)) were formed during hydrothermal alteration of primary nepheline by fluids/solutions with high Si-Al-Ca activities. Poikilitic garnet (Ti-bearing andradite) has inclusions of all primary minerals, amphibole and zeolites, and presumably crystallized metasomatically during a late metamorphic event (Caledonian orogeny).