Geophysical methods for detecting shallow sulphide mineralization in the Halifax Formation, Nova Scotia: a reconnaissance study

Authors
Citation
K. Howells et D. Fox, Geophysical methods for detecting shallow sulphide mineralization in the Halifax Formation, Nova Scotia: a reconnaissance study, ATL GEOL, 34(3), 1998, pp. 211-227
Citations number
37
Categorie Soggetti
Earth Sciences
Journal title
ATLANTIC GEOLOGY
ISSN journal
08435561 → ACNP
Volume
34
Issue
3
Year of publication
1998
Pages
211 - 227
Database
ISI
SICI code
0843-5561(199811)34:3<211:GMFDSS>2.0.ZU;2-O
Abstract
Construction activities have exposed sulphide-bearing slates of the Halifax Formation in southern mainland Nova Scotia. Under atmospheric conditions t he sulphides break down and cause acid rock drainage (ARD) which adversely affects local ecosystems. These effects have been a major problem at the Ha lifax International Airport, causing fish kills and the expenditure of mill ions of dollars to ameliorate the ARD. A preferable alternative is to locat e areas of sulphide mineralization in the construction area prior to excava tion. Concentrated zones of sulphide mineralization can then be avoided, or treatment plans can be formulated in advance. Geophysical surveys provide possible means of detecting sulphides in slates of the Halifax Formation. To evaluate various geophysical methods, reconnaissance profiles were carri ed out in two areas near the Halifax International Airport utilizing ground conductivity, magnetic, VLF EM, spontaneous potential, and induced polariz ation measurements. The conductivity meter selected was specific to "constr uction depths" (i.e., its exploration depth limit is 6 m or less). Test pit s were dug on one line in each area to sample bedrock coincident with and b etween conductivity anomalies. Bedrock samples collected in each test pit w ere analyzed for total sulphur, total carbon, Fe2+, and Fe3+ contents. On the first grid, increased total sulphur content was measured in rock spe cimens from a test pit coincident with a large ground conductivity anomaly. In contrast, extremely small total sulphur content was measured in rock sp ecimens from a nearby hole which was deliberately situated where there is n o conductivity anomaly. Similar results were obtained from the second grid. Magnetic anomalies are coincident with all but one of the sampled conducti vity anomalies, indicative of the presence of pyrrhotite. Combined ground c onductivity, magnetic and VLF EM surveys appear to be a practicable method for detecting near-surface sulphide mineralization in the Halifax Formation , and such surveys should be included in the Nova Scotia Environment Act.