Cover photo: A euhedral, oscillatory zoned, primary monazite has been altered at the rims and along cracks to an allanite-apatite-xenotime assemblage. The host mineral is feldspar. Granite, Strzegom Massif. Workshop on accessory minerals, University of Warsaw, September 2014 Editors of Volume Bogusław BAGIŃSKI, Oliwia GRAFKA Witold MATYSZCZAK, Ray MACDONALD Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw Al. Żwirki i Wigury 93, 02-089 Warszawa
[email protected] Language correction: Ray MACDONALD Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw Al. Żwirki i Wigury 93, 02-089 Warszawa
[email protected] 1 Organizing committee: Bogusław BAGIŃSKI Ray MACDONALD Michał RUSZKOWSKI Financial support: Workshop on accessory minerals was financially supported by the Polish Ministry of Science and Higher Education subvention and research grant No N N307634040, Faculty of Geology University of Warsaw and PIG-PIB. 2 Workshop on accessory minerals, University of Warsaw, September 2014 Preface The progress made over the past two decades in our understanding of accessory minerals containing HFSE has been remarkable. Even when “fresh-minted”, minerals such as monazite, xenotime, allanite and zircon are compositionally and structurally complex. The complexity increases many times during low-temperature alteration processes, such as interaction with hydrothermal fluids and weathering. Progress has, of course, been expedited by the introduction of a range of exciting new technologies, especially in structure determinations. On re-reading the excellent 2002 review of accessory mineral research by Poitrasson et al., one is struck by how far the subject area has advanced in 12 years. We felt that this was an opportune time to bring together a group of Earth scientists with special expertise in accessory minerals to outline their current research interests, to share ideas and to consider productive future research directions.