minerals Article The Panasqueira Rare Metal Granite Suites and Their Involvement in the Genesis of the World-Class Panasqueira W–Sn–Cu Vein Deposit: A Petrographic, Mineralogical, and Geochemical Study Christian Marignac 1 , Michel Cuney 1,* , Michel Cathelineau 1 , Andreï Lecomte 1, Eleonora Carocci 1 and Filipe Pinto 2 1 Université de Lorraine, CNRS, CREGU, GeoRessources, F-54000 Nancy, France;
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[email protected] Received: 20 May 2020; Accepted: 15 June 2020; Published: 23 June 2020 Abstract: Elucidation of time-space relationships between a given wolframite deposit and the associated granites, the nature of the latter, and their alterations, is a prerequisite to establishing a genetic model. In the case of the world-class Panasqueira deposit, the problem is complicated because the associated granites are concealed and until now poorly known. The study of samples from a recent drill hole and a new gallery allowed a new approach of the Panasqueira granite system. Detailed petrographic, mineralogical, and geochemical studies were conducted, involving bulk major and trace analyses, BSE and CL imaging, EPMA, and SEM-EDS analyses of minerals. The apical part of the Pansqueira pluton consisted of a layered sequence of separate granite pulses, strongly affected by polyphase alteration. The use of pertinent geochemical diagrams (major and trace elements) facilitated the discrimination of magmatic and alteration trends.