4.6 Article

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

期刊

GEOPHYSICS
卷 86, 期 3, 页码 B181-B191

出版社

SOC EXPLORATION GEOPHYSICISTS
DOI: 10.1190/GEO2020-0336.1

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资金

  1. European Union's Horizon 2020 research and innovation program [775971]
  2. H2020 Societal Challenges Programme [775971] Funding Source: H2020 Societal Challenges Programme

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Seismic methods prove to be an affordable and effective way to study subsurface for mineral exploration. An innovative seismic survey was conducted at the Neves-Corvo mine in early 2019, utilizing surface array data and underground seismic data to examine the mining areas. Through careful processing of noisy surface data and analysis, key subsurface geological structures and economic mineral deposits were successfully imaged and delineated.
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.

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