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Geology and Geochemistry of Carbonate-hosted Lead-zinc Deposits of the Kootenay Arc (82F/east Half).

Authors
Sabin-AE
Source
Paper 1988-1 in Geo Fieldwork British Col Min of Energy Mines & Pet Res 1988 :531-534
Link
NIOSHTIC No.
10006248
Abstract
Carbonate-hosted, lead-zinc deposits of the kootenay arc have been grouped as either transgressive or concordant types, based on field characteristics. Lead isotope analyses suggest that each ore deposit type contains a unique grouping of lead ratios that do not adequately conform to the bluebell or shale lead growth curves. Detailed ore and gangue mineral petrology, lithogeochemistry, ore geochemistry, lead isotopy, and field evidence will be gathered and then used to qualitatively and quantitatively compare and contrast among these carbonate-hosted deposits.
Publication Date
19880101
Document Type
OP;
Fiscal Year
1988
Identifying No.
OP 144-88
NIOSH Division
WO;
Source Name
Paper 1988-1 in Geo. Fieldwork British Col. Min. of Energy, Mines & Pet. Res. 1988, PP. 531-534
Page last reviewed: April 12, 2019
Content source: National Institute for Occupational Safety and Health Education and Information Division