Sedimentology and ore genesis / Седиментология и рудообразование (осадочное рудообразование)

Historically, the relation between sedimentology and the field of ore genesis has been a function of prevailing patterns of thought. Table I offers a brief schematic summary of the trend of thought patterns since Albertus Magnus.
Whenever the trend was to search for causes from within, the interest in the wall rock and its genesis was great. When causes from without appealed more to the scientists, the rocks enclosing ore deposits, and especially the sediments received little attention.
The present generation inherited largely the latter type of thinking; so much so, as a matter of fact, that sedimentary petrology was treated as a step child in petrology courses. An “economic geologist” was not required to have a serious interest in “soft rock petrology”. The ore in “soft rocks” was a priori believed to have come from “hard rocks” at unknown depths, and the magic word which solved all the problems was “replacement”. <...>

Early diagenetic pyrite in fine-grained sediments and the genesis of sulphide ores

Apropos du rdle metallogenique de la prkipitation et de I’adsorption skdimentaires

Facies differentiation and controlling factors for the depositional lead-zinc concentration in the Wange osyncline of the eastern Alps

Lead-zinc deposits in the Calcareous Alsp as an example of submarine-hydrothermal formation of mineral deposits

L’application des courbes pr6visionnelles a la recherche4 des gisements stratiformes de plomb

Diagenetic behaviour of sulphides

Supergene sulfides and sulfates in the supergene zones of sulfide ore deposits

ohlensauerlinge als eine Eisenquelle der sedimentaren Eisenerz

Уtude sMimentologique du minerai de fer oolithique de Lorraine

Facies problems of boehmitic and diasporitic