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Reflection seismic imaging to unravel subsurface geological structures of the Zinkgruvan mining area, central Sweden

Gil de la Iglesia, Alba (författare)
Uppsala universitet,Geofysik
Malehmir, Alireza, 1977- (författare)
Uppsala universitet,Geofysik,Uppsala Univ, Dept Earth Sci, Uppsala, Sweden.
Buske, Stefan (författare)
Tech Univ Bergakad Freiberg, Inst Geophys & Geoinformat, Freiberg, Germany.
visa fler...
Alcalde, Juan (författare)
Geosci Barcelona Geo3Bcn CSIC, Barcelona, Spain.
Ayarza, Puy (författare)
Univ Salamanca, Dept Geol, Salamanca, Spain.
Martinez, Yesenia (författare)
Geosci Barcelona Geo3Bcn CSIC, Barcelona, Spain.
Lindskog, Louise (författare)
Zinkgruvan Min AB, Zinkgruvan, Sweden.
Spicer, Bill (författare)
Lundin Min Corp, Toronto, ON, Canada.
Carbonell, Ramon (författare)
Geosci Barcelona Geo3Bcn CSIC, Barcelona, Spain.
Orlowsky, Dirk (författare)
DMT GmbH & Co, Essen, Germany.
Carriedo, Jorge (författare)
Lundin Min Corp, Toronto, ON, Canada.
Hagerud, Anja (författare)
Zinkgruvan Min AB, Zinkgruvan, Sweden.
visa färre...
 (creator_code:org_t)
Elsevier, 2021
2021
Engelska.
Ingår i: Ore Geology Reviews. - : Elsevier. - 0169-1368 .- 1872-7360. ; 137
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Zinkgruvan mining area is located on the south-eastern part of the Bergslagen district, one of the three major mineral producing regions in Sweden. In this study, we present the results from three (P1, P2 and P8) reflection seismic profiles each approximately 3000 m-long crossing the Zinkgruvan Zn-Pb-Ag-(Cu) mining area. P1 was acquired using cabled geophones with 10 m receiver and source interval and crossed major geological features. The other two profiles (P2 and P8) were acquired by wireless recorders with 20 m receiver and 10 m source interval and ran perpendicular to P1. Through a special data processing workflow adapted to this dataset, good quality seismic sections were obtained along these profiles, although a high noise level due to high voltage electric power lines was present. The interpretations were constrained by (1) seismic P-wave velocity and density data from a series of downhole logging measurements, (2) 3D forward reflection traveltime modelling in both pre- and post-stack domains, and (3) other geophysical and geological observations available from the site. Despite the notably complex geology, the processed seismic sections clearly reveal a series of horizontal to gently dipping reflections associated with known geological formations. Results indicate that most structures and lithological contacts dip or plunge to the northeast, including the targeted Zinkgruvan Formation. The results from this seismic survey are encouraging regarding the potential of the seismic method for base-metal exploration in Sweden and in particular in the Bergslagen district. It shows the high resolving power of the reflection seismic methods for imaging complex geological structures in a cost-effective and environmentally-friendly way.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)

Nyckelord

Reflection seismic
Mineral exploration
Modeling
Zinkgruvan

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

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