Geology of the recently discovered massive and stockwork sulphide mineralization at Semblana, Rosa Magra and Monte Branco, Neves–Corvo mine region, Iberian Pyrite Belt, Portugal
نویسندگان
چکیده
Abstract The recently discovered massive and stockwork sulphide mineralization of Semblana-Rosa Magra Monte Branco, situated ESE the Neves–Corvo volcanogenic (VMS) deposit in Iberian Pyrite Belt (IPB) is presented. Geological setting tectonic model discussed based on proxies such as palynostratigraphy U–Pb zircon geochronology. found within IPB Volcano-Sedimentary Complex (VSC) Lower sequence, which includes felsic volcanic rocks (rhyolites) with ages zircons 359.6 ± 1.6 Ma, black shales Neves Formation late Strunian age. Massive sulphides are enveloped by these shales, implying that volcanism, shale sedimentation essentially coeval. This circumstance considered highly prospective, it represents an important exploration vector to target VMS across IPB, areas where VSC sequence present. Upper siliciclastic sedimentary middle–late Visean age, shows no but a Tournaisian (350.9 2.3 Ma) volcanism disseminated was also identified. Nevertheless, stratigraphic palynological gaps were sediments, between sequences, reflecting probable erosion uplift mechanisms linked extensional tectonics. Semblana Branco deposits Rosa enclosed sheets dismembered fold-and-thrust complex, characteristic NE region. methodologies used allow geological comparison other mine regions Lousal–Caveira, Herrerias, Tharsis Aznalcollar.
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ژورنال
عنوان ژورنال: Geological Magazine
سال: 2021
ISSN: ['1469-5081', '0016-7568']
DOI: https://doi.org/10.1017/s0016756820001284