GEOSCAN Search Results: Fastlink


TitleSeismic properties of rocks from the Flin Flon volcanogenic massive sulfide camp
AuthorWhite, D J; Mwenifumbo, C J; Salisbury, M H
SourceTrout Lake VMS deposit, Flin Flon, Canada; by Pehrsson, S (ed.); Gibson, H (ed.); Economic geology and the bulletin of the Society of Economic Geologists vol. 111, issue 4, 2016 p. 913-931,
Alt SeriesEarth Sciences Sector, Contribution Series 20110054
PublisherSociety of Economic Geologists
Mediapaper; on-line; digital
File formatpdf; html
NTS63K/12; 63K/13
AreaFlin Flon; Cliff Lake; Ross Lake
Lat/Long WENS-101.9667 -101.8333 54.8000 54.7000
Subjectsgeophysics; economic geology; geophysical surveys; seismic reflection surveys; seismic profiles; seismic methods; mineral exploration; mineral deposits; volcanogenic deposits; sulphide deposits; core samples; geophysical logging; seismic waves; s waves; bedrock geology; lithology; sedimentary rocks; sandstones; igneous rocks; volcanic rocks; basalts; rhyolites; mafic rocks; intrusive rocks; metasedimentary rocks; metamorphism; shearing; foliation; mineralization; alteration; intrusions; structural features; faults, thrust; folds; synclines; fault zones; stratigraphic analyses; Flin Flon Volcanogenic Massive Sulphide Camp; Missi Group; Hidden Formation; Flin Flon Formation; Millrock Member; Blue Lagoon Member; volcanogenic massive sulphide deposits (VMS); hanging wall; footwall; Precambrian
Illustrationsgeological sketch maps; seismic images; tables; plots; geophysical logs; profiles; histograms; seismic profiles
ProgramTargeted Geoscience Initiative (TGI-4), Volcanogenic Massive Sulfide Ore Systems
Released2016 05 13
AbstractSeismic properties of rocks from the Flin Flon volcanogenic massive sulfide (VMS) camp were determined to evaluate the suitability of seismic reflection imaging for mineral exploration and have subsequently aided interpretation of 2-D and 3-D seismic data acquired in the camp. Seismic impedances of Flin Flon rocks were determined from laboratory measurements of compressional and shear wave velocity (Vp, Vs) and density for 61 core samples. Complementary in situ measurements of Vp and density provided by sonic and density logs acquired in nine drill holes allow calculation of synthetic seismic responses. Sandstones of the Missi Group show low reflectivity with sparse strong internal reflections resulting from intrusions or thrust-interleaved mafic rocks. Basaltic sequences are generally moderately reflective due to variability in their composition, alteration, and the effects of foliation and shearing. The mine horizon, which hosts the known orebodies, should be reflective, based on the impedance contrast of constituent rhyolite and mafic igneous rocks and the presence of sulfide mineralization. However, reflectivity of this horizon should be variable due to the significant alteration of the footwall basalt. Ore zones (solid sulfide) should range from moderately to very highly reflective, depending on their sulfide compositions. Vertical seismic profiles demonstrate that contacts between major stratigraphic units (e.g., Missi Group contact with Hidden Formation volcanic rocks or felsic igneous rocks within the basalts) should produce significant reflections, whereas some of the internal reflectivity predicted for the basaltic sequences will not be as prevalent.