Certain terms of mining geology as defined and used

Schmitt, Harrison Ashley

doi:10.2113/gsecongeo.49.2.198

Economic Geology

1954

DOI: 10.2113/gsecongeo.49.2.198

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Certain terms of mining geology as defined and used

Harrison Ashley Schmitt¹

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Epigenetic Mineralization in Yorkshire

Dunham¹

1959

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Summary The lead-zinc-copper-fluorine-barium deposits of N.W. Yorkshire are discordant veins and associated replacements of epigenetic origin. A summary of previous ideas shows that the principle of stratigraphic control has been recognized from earliest times. The structural setting of the deposits on the Rigid Block and their relation to preferred horizons in the Viséan and Namurian rocks is described. After a review of current genetic hypotheses it is suggested that at the time of mineralization, an active circulation of deep groundwaters was augmented by juvenile waters from acidic magmatism in the crust or from still deeper levels. The possible roles of metamorphic and connate waters are considered.

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Epigenetic Mineralization in Yorkshire

Dunham¹

1959

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Certain terms of mining geology as defined and used

Cited by 1 publication

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Epigenetic Mineralization in Yorkshire

Epigenetic Mineralization in Yorkshire

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