Innovative seismic imaging of volcanogenic massive sulfide deposits, Neves-Corvo, Portugal — Part 2: Surface array

Author:

Donoso George A.1ORCID,Malehmir Alireza1ORCID,Brodic Bojan1ORCID,Pacheco Nelson2,Carvalho João3,Araujo Vitor2

Affiliation:

1. Uppsala University, Department of Earth Sciences, Villavägen 16, Uppsala 75236, Sweden.(corresponding author); .

2. Somincor (Lundin Mining), Neves-Corvo Mine, Santa Bárbara de Padrões, Castro Verde 7780-409, Portugal..

3. LNEG, Estrada da Portela-Zambujal, Apartado 7586, 2610-999 Amadora, Portugal..

Abstract

Seismic methods are an affordable and effective way of studying the subsurface for mineral exploration. With the goal of testing new technologies for mineral exploration in highly challenging mining areas, in early 2019, an innovative seismic survey was conducted at the Neves-Corvo mine, south Portugal. We have focused on the data and results from the surface array data, whereas other work deals with the underground seismic data. The surface seismic survey consisted of two perpendicular 2D profiles positioned above the known world-class tier-1 Lombador deposit. Simultaneously, a survey inside the active underground mine took place, being unique because it included the testing of a prototype system that enabled accurate GPS-time (microsecond accuracy) synchronization inside the mine tunnels, approximately 650 m below the surface profiles. Due to the active mining operations, the surface data are noisy. To handle this, a carefully tailored processing algorithm was developed and applied to enhance reflections in the data, interpreted to originate from lithologic contacts and the Lombador deposit. The results and interpretations from 2D processing were validated taking advantage of the known deposit geometry using 3D exploding reflector modeling and pseudo-3D cross-dip analysis. These analyses suggest that there is an out-of-plane signature of the Lombador deposit on the surface data. Additionally, source points activated in the exploration tunnels and simultaneously recorded on the surface profiles allowed for the creation of a 2D velocity model that was used for migration and time-to-depth conversion, providing a reliable 2D seismic section of the subsurface under the surface profiles. We determine that limited surface coverage 2D surveys and a velocity model derived from the tunnel-to-surface seismic recordings allow for imaging of key subsurface geologic structures and delineating mineral deposits of economic interest.

Funder

European Union Horizon 2020

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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