Abstract
AbstractDiamond inclusions have been found in apatite from a specific type of orthogneiss of a volcanosedimentary sequence from the deepest tectonic complex (Nevado-Filabride) of the Alpine Betic-Rif belt (Spain). This unusual finding led us to make a detailed petrographical and geochemical study, with the aim of characterizing ultrahigh-pressure (UHP) apatite and comparing it with the younger and widespread magmatic and/or metamorphic generations. The UHP apatite is abundant in biotite-rich orthogneisses, whereas it is lacking in the most common biotite-poor orthogneisses, which instead contain abundant magmatic apatite. In addition to diamond, UHP apatite contains abundant biphased inclusions consisting of chlorides and hydrocarbons. The late alteration of fluid inclusions caused oligomerization of hydrocarbons and graphitization of diamond, leading to a characteristic irregular outer brownish zone. The UHP apatite shows bell-shaped rare earth element (REE) profiles, with weak Eu anomalies and Sr and Th...
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