Abstract
It is suggested that these deposits were emplaced during early diagenesis by an influx of dissolved Cu into initially pyritic basal units of grey-bed host rocks, possibly from underlying coarse-grained red beds or pene-exhalative solutions which 'exhale' into the red beds.-R.E.S.
Cite
CITATION STYLE
APA
Brown, A. C., & Chartrand, F. M. (1986). Diagenetic features at White Pine (Michigan), Redstone (N.W. Territories, Canada) and Kamoto (Zaire). Sequence of mineralization in sediment-hosted copper deposits (Part 1). Geology and Metallogeny of Copper Deposits, 390–397. https://doi.org/10.1007/978-3-642-70902-9_28
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