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3D Constrained Gravity Inversion and TEM, Seismic Reflection and Drill-Hole Analysis for New Target Generation in the Neves–Corvo VMS Mine Region, Iberian Pyrite Belt

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Abstract

Located in the Iberian pyrite belt, the Neves–Corvo mine is a world-class massive sulfide deposit and the largest operating mine in Portugal with underground mining down to 1000 m depth focused on massive and stockwork Cu, Zn, Pb rich ores. Gravimetric data have had a leading role in the discovery of the seven known deposits, together with time-domain electromagnetic (TEM) ground data. In this work, we present the results of a 3D constrained gravity inversion carried out with legacy ground gravity data. The 3D gravity inversions were carried out using an updated density database containing approximately 142,000 measurements. A recently constructed 3D geological model based on reprocessed 2D seismic reflection, 3D seismic, TEM and updated geology from detailed surface mapping and drill-hole data, was used to constrain the inversions. The results show multiple high-density anomalies that may indicate the presence of mineralization at depth. These anomalies were therefore cross-checked with holes previously drilled. Approximately 97% of more than 1000 available surface drill-holes located on or at a distance of less than 200 m from the high-density anomalies intersected mineralization. However, gravity anomalies have been drilled in the past and particularly dense black shales or rhyolitic/gabbroic rocks have been intersected. To increase the success of future drilling, gravimetric anomalies have been correlated spatially with high-conductivity TEM zones and strong-amplitude seismic reflections, because igneous rocks usually present weak-to-moderate conductivity and a massive column of black shales presents a seismic signature quite different from that of mineralization. We concluded that some of these locations represent high-quality targets to consider following up with drilling and further exploration.

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Figure 1

adapted from Oliveira et al., 2016; Matos et al., 2020). (c) Simplified stratigraphy of the Neves–Corvo mine region, after Oliveira et al. (2013), Mendes et al. (2020) and Pereira et al. (2021). Legend: MT = Mértola Fm. (MT1, MT2 and MT3); r = Brancanes Fm.; g = Godinho Fm.; bv = “Borra de vinho” Fm.; s = Grandaços Fm.; Va = Felsic volcanic rocks; Vb = Mafic volcanic rocks; MS = Massive Sulfides; ST = Stockwork; n = Neves Fm.; Co = Corvo Fm.; PQ = Phyllite Quartzite Gr.; ca = limestones; d = dolerites; J = Jaspers

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Availability of Data and Material

Gravimetric data are commercially available at LNEG; density database is available upon request.

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Acknowledgments

The authors are grateful to Somincor/Lundin Mining Corporation for providing drill-hole, geological and EM data used in this work, and LNEG for the land gravity and geological data. The authors thank the EU for funding projects EXPLORA/Alentejo2020 (Op ALT20-03-0145-FEDER-000025), and Smart Exploration (Agreement No. 775971) under H2020 research and innovation program. We are also grateful to EMIT and Emerson for providing academic licenses of Maxwell and GoCad software, respectively, and Naphtali from Seequent for support to Oasis Montaj and VOXI licenses. This work is also dedicated to all SFM/IGM/LNEG field work teams that permitted the production of hundreds of gravity maps in detailed 1/5 000 and 1/25 000 scales, coordinated by José Marcos Bengala, Manuel Nolasco Silva, Vitor Alvoeiro and Luís Torres. We are also indebted to Ian Fergusson and four anonymous reviewers who greatly contributed to improve the quality of this work.

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Correspondence to João Carvalho.

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Appendix

Appendix

See Figure 10.

Figure 10
figure 10

Results for the third run of the gravimetric inversion (d > 3.5 g/cm3) overlaid by the analytical signal of the residual Bouguer anomaly map shown in Figure 2b. Geological contours of Figure 1b are also superimposed

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Marques, F., Dias, P., Carvalho, J. et al. 3D Constrained Gravity Inversion and TEM, Seismic Reflection and Drill-Hole Analysis for New Target Generation in the Neves–Corvo VMS Mine Region, Iberian Pyrite Belt. Nat Resour Res 31, 2321–2346 (2022). https://doi.org/10.1007/s11053-022-10081-4

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