![Sample our Geography journals, sign in here to start your FREE access for 14 days]({"type":"image" , "src" : "/sda/5937/TOC-Subject-Sample-2021-Geography.jpg"})
Abstract
Scanning Electron Microscopy and Energy Dispersive Analysis are used to study minute-sized crystals of high-field-strength-element minerals in an evolved batch of fluorine-rich granite. The batch separated due to buoyancy from the bulk magma before fluid separation was reached. Fluorine acted as the main complexing agent in the magma, facilitating the transport of many elements. Enhanced concentrations of elements such as Nb, Y, rare earth elements, Th and possibly Be gave the granite an accessory mineral composition similar to that of NYF pegmatite. Biotite was chloritized and often no remaining biotite can be identified. Frequent are two minerals from the aeschynite—euxenite—polycrase group. One is blocky and formed together with chlorite. It was replaced by an acicular variety, which continued to crystallize into the late hydrothermal stage. Bastna¨site and synchysite are also common in the granite. Both started crystallizing together with chlorite, but only synchysite can be followed into the late hydrothermal stage. Hingganite and gadolinite occur as inclusions in fluorite and chlorite. Galgenbergite formed as fracture-fillings. Some other rare minerals have merely been identified as accidental inclusions, but their identification is less certain. They include brenkite, fluocerite, fergusonite and possibly håleniusite. Chemical heterogeneities in the minerals point to incomplete equilibration.
Acknowledgements
Funding for this research was originally obtained from the Natural Science Research Council of Sweden (NFR). Vetenskapsrådet (VR) granted the funding to be used during an extended time. Peter Stutz, University of Hamburg, made the thin sections. Comments on a draft of the manuscript by Prof. Roland Vinx, University of Hamburg are acknowledged. Thanks also go to Ulf Bertil Andersson and an anonymous reviewer for valuable comments.