A geochemical study of the shales of the Lower Cambrian Manganese Shale Group of the Harlech Dome, North Wales

Details A geochemical study of the shales of the Lower Cambrian Manganese Shale Group of the Harlech Dome, North Wales A geochemical study of the shales of the Lower Cambrian Manganese Shale Group of the Harlech Dome, North Wales

Nov 1959

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1959gecoa..17..186m&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 17, Issue 3-4, pp.186-200

Physics

2

Scientific paper

The shales of the Manganese Shale Group are featured geochemically by their relatively high manganese content, the predominance of ferrous over ferric iron, the sympathetic behaviour of cobalt, nickel, chromium, and vanadium with total iron, an inverse relationship of strontium and barium and a direct relationship of boron and barium. Evidence is presented to indicate that the source rocks of the Manganese Shales were acid gneisses.

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