Appalachian Mississippi valley-type deposits: paleoaquifers and brine provinces

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Artículo de libro Serie Society of Economic Geologists. Special Publication, n.4.Editor: Littleton, Colorado: Society of Economic Geologists, 1997Descripción: pp. 29-57 ilus., tbls.Tema(s): INCLUSIONES FLUIDAS

Tipo de ítem	Ubicación actual	Signatura	Estado	Fecha de vencimiento	Código de barras
Artículo de libro	Biblioteca INGEMMET	553.44/S21\|2 (Navegar estantería)	Disponible		2563
Libro	Biblioteca INGEMMET	553.44/S21 (Navegar estantería)	Disponible		4660

Previo								Siguiente
Previo	553.44/S21\|17 Geochemical characteristics of the Fankou Pb-Zn deposit, northern Guangdong, south China	553.44/S21\|18 Geology, geochemistry, and genesis of the Silesia-Cracow zinc-lead district, southern Poland	553.44/S21\|19 Geology of the Admiral Bay carbonate-hosted zinc-lead deposit, Canning basin, Western Australia	553.44/S21\|2 Appalachian Mississippi valley-type deposits: paleoaquifers and brine provinces	553.44/S21\|20 Geology of the Polaris Zn-Pb deposit and surrounding area, Canadian Arctic archipelago	553.44/S21\|21 Influence of carbonate minerals on contemporary oxidation processes in tailings of Pb-Zn ore recovery	553.44/S21\|22 Internal sediments as a key to understanding the hydrothermal karst origin of the upper Silesian Zn-Pb ore deposits	Siguiente

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Previo								Siguiente
Previo	553.44/S21\|17 Geochemical characteristics of the Fankou Pb-Zn deposit, northern Guangdong, south China	553.44/S21\|18 Geology, geochemistry, and genesis of the Silesia-Cracow zinc-lead district, southern Poland	553.44/S21\|19 Geology of the Admiral Bay carbonate-hosted zinc-lead deposit, Canning basin, Western Australia	553.44/S21\|2 Appalachian Mississippi valley-type deposits: paleoaquifers and brine provinces	553.44/S21\|20 Geology of the Polaris Zn-Pb deposit and surrounding area, Canadian Arctic archipelago	553.44/S21\|21 Influence of carbonate minerals on contemporary oxidation processes in tailings of Pb-Zn ore recovery	553.44/S21\|22 Internal sediments as a key to understanding the hydrothermal karst origin of the upper Silesian Zn-Pb ore deposits	Siguiente

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