Deep massive sulphide exploration using 2D and 3D geoelectrical and induced polarization data in Skellefte mining district, northern Sweden. (23rd March 2016)

• Record Type: Journal Article
• Authors: Tavakoli, Saman; Bauer, Tobias E.; Rasmussen, Thorkild M.; Weihed, Pär; Elming, Sten‐Åke
• Is Part Of: Geophysical prospecting. Volume 64:Number 6(2016)
• Page Start: 1602
• Page End: 1619
• Publication Date: 2016-03-23
• Subjects: Skellefte District -- Induced polarization -- Volcanogenic massive sulphide -- Resistivity imaging -- Petrophysical data; Prospecting -- Geophysical methods -- Periodicals; 622.15
• DOI: 10.1111/1365-2478.12363
• Languages: English
• ISSNs: 0016-8025

Abstract

ABSTRACT: Geoelectrical and induced polarization data from measurements along three profiles and from one 3D survey are acquired and processed in the central Skellefte District, northern Sweden. The data were collected during two field campaigns in 2009 and 2010 in order to delineate the structures related to volcanogenic massive sulphide deposits and to model lithological contacts down to a maximum depth of 1.5 km. The 2009 data were inverted previously, and their joint interpretation with potential field data indicated several anomalous zones. The 2010 data not only provide additional information from greater depths compared with the 2009 data but also cover a larger surface area. Several high‐chargeability low‐resistivity zones, interpreted as possible massive sulphide mineralization and associated hydrothermal alteration, are revealed. The 3D survey data provide a detailed high‐resolution image of the top ∼450 m of the upper crust around the Maurliden East, North, and Central deposits. Several anomalies are interpreted as new potential prospects in the Maurliden area, which are mainly concentrated in the central conductive zone. In addition, the contact relationship between the major geological units, e.g., the contact between the Skellefte Group and the Jörn Intrusive Complex, is better understood with the help of 2010 deep‐resistivity/chargeability data. The bottommost part of the Vargfors basin is imaged using the 2010 geoelectrical and induced polarization data down to ∼1‐km depth.