By D. Large (auth.), Prof. Dr. Günther H. Friedrich, Dr. Peter M. Herzig (eds.)
The geology and metallogeny of base steel sulfide deposits in Europe, Africa and Australia used to be the subject of the DMG-GDMB-SAG Joint assembly held in Aachen (FRG), September 16-19, 1985. Divided into components, the awarded papers conceal the outline and interpretation of sediment-hosted in addition to volcanic-sediment-hosted and volcanic-hosted copper-zinc-lead (gold-silver) deposits. the current compilation is an summary of present learn actions and effects on copper-zinc-lead deposits in classical mining districts contemplating geological, lithological, geochemical and tectonic parameters of ore formation. Even during periods of depressed steel costs, base steel sulfide deposits nonetheless stay essentially the most beautiful mineral exploration pursuits. This wide assessment presents important info to researchers and explorationists.
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Additional info for Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments: Proceedings of the DMG-GDMB-SGA-Meeting Aachen, 1985
In: Friedrich G H, Genkin AD, Naldrett Al, Ridge lD, Sillitoe RH, Vokes FM (eds) Geology and Metallogeny of Copper deposits. SGA Spec Publ 4:477-491 Majorowicz 1 (1982) The ambiguities in tectonic interpretation of geothermal field patterns in the platformic areas in Poland. Przegl Geol 2: 86-94 Majorowicz 1, Marek S, Znosko 1 (1984) Paleogeothermal gradients by vitrinite reflectance data and their relation to the present geothermal gradient patterns of the Polish Lowlands. Tectonophysics 103: 141-156 Rentzschl (1981) Mineralogical-geochemical prospection methods in the Central European Copper Belt.
3 u o a. III , x 0 E " , «u Ro41 Ro43 Ro 23 Ro18 Ro19 Ro 35 m 5 x o E 4 Ole e N 3 u o 2 a. III , ' x 0 E " lllu Ro 43 Ro24 Ro41 Ro 23 Ro18 Ro19 Ro 35 m ~1L. ,LJ- . IL,~ lQLI. - . ,. Ji Ro19 Ro35 t: Fig. 10. Spacing for some typical drill hole intersections in the Rote Faule. copper facies and lead-zinc facies. A-spacing vertical distance between copper and lead peak; B-spacing vertical distance between copper and zinc peak; C -spacing vertical distance between lead and zinc peak. all measured in meters Fig.
Sketch map showing the tecto-stratigraphic situation of Central European Variscan Basement. Cities: F FrankfurtlM; B Berlin; P Prague; WI WrocYaw; K Kiiln; triangle sample sites of felsic metavolcanics analyzed; points sample sites of mafic metavolcanics analyzed or lie in any spatial/temporal relation to convergent plate boundaries, seems unclear. Based on the geochemistry of mafic metavolcanics (Okrusch et al. 1985), and from the metallogenetic point of view there seems to be evidence that parts of the Mid German Crystalline Rise, which represents the northernmost part of the Saxothuringian zone, could be referred to an ensialic island arc oflate Proterozoic to early Paleozoic age.
Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments: Proceedings of the DMG-GDMB-SGA-Meeting Aachen, 1985 by D. Large (auth.), Prof. Dr. Günther H. Friedrich, Dr. Peter M. Herzig (eds.)