BiCoNi Formation

Last updated April 28, 2020

The BiCoNi Formation is a hydrothermal lode formation, in which bismuth, cobalt, nickel and uranium ores have coalesced. It occurs mainly in the Ore Mountains and is the youngest formation in the hydrothermal sequence (polymetalliferous (kb) formation, iron-barite (eba) formation, precious brownspar (eb) formation, fluorite-barite (fba) formation, BiCoNi formation). Due to its combination with uranium, it is occasionally also called the bismuth-cobalt-nickel-uranium formation.

Genesis

The BiCoNi Formation emerged during the contact metamorphic restructuring of sedimentary slate in the course of Variscan granite intrusions during the Subhercynian-Austrian (Austrisch) cycle about 100–80 million years ago.^[1] It is the product of an intracrustal, epithermal paragenesis. It runs in quartz lode types as the primary ores or cobalt and nickel, which usually occur together with arsenides, native bismuth and pitchblende.

Use

The BiCoNi Formation has been intensively mined since the Late Middle Ages for bismuth, later cobalt and nickel, and, since the late 19th century, also for uranium. In the second half of the 20th century it was intensively mined by SDAG Wismut.

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References

↑ U. Lipp, S. Flach, Landesamt für Umwelt, Landwirtschaft und Geologie (ed.), "Übersicht zum zeitlichen Ablauf der Mineralabscheidungen und der Bildung der Paragenesen", Wismut-, Kobalt-, Nickel- und Silbererze Im Nordteil des Schneeberger Lagerstättenbezirkes, Bergbau in Sachsen (in German), Band 10, p. 1, retrieved 2014-02-26, Beilage 1 Abbildung 90

Literature

Oscar Walter Oelsner (1958), Die erzgebirgischen Granite, ihre Vererzung und die Stellung der BiCoNi-Formation innerhalb dieser Vererzung, Geologie (in German), Jg. 7, Berlin, pp. 682–701
G. Leithold; et al. (1962), Kammer der Technik, Fachverband Bergbau (ed.), Taschenbuch Bergbau: Tiefbau (in German), III, Leipzig: Deutscher Verlag für Grundstoffindustrie, pp. 30–35
U. Lipp, S. Flach, Landesamt für Umwelt, Landwirtschaft und Geologie (ed.), Wismut-, Kobalt-, Nickel- und Silbererze im Nordteil des Schneeberger Lagerstättenbezirkes, Bergbau in Sachsen (in German), 10, retrieved 2014-02-26
Axel Hiller, Werner Schuppan (31 December 2007), Landesamt für Umwelt, Landwirtschaft und Geologie (ed.), Geologie und Uranbergbau im Revier Schlema-Alberoda, Bergbau in Sachsen (in German), 14 (1. ed.), retrieved 2014-02-26

External links

Marco Münch. "Die biconi-Formation" (PDF, 352kB). Die Uranerzlagerstätte Schlema-Alberoda (in German). pp. 8f. Retrieved 2014-02-26.
H.-D. Bauer, G. Stoyke (2005). "Die Arsenproblematik in Betrieben der ehemaligen SAG/SDAG Wismut" (PDF, 174kB). Kompass 5/6 2005 (in German). Retrieved 2014-02-26.

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[1] U. Lipp, S. Flach, Landesamt für Umwelt, Landwirtschaft und Geologie (ed.), "Übersicht zum zeitlichen Ablauf der Mineralabscheidungen und der Bildung der Paragenesen", Wismut-, Kobalt-, Nickel- und Silbererze Im Nordteil des Schneeberger Lagerstättenbezirkes, Bergbau in Sachsen (in German), Band 10, p. 1, retrieved 2014-02-26, Beilage 1 Abbildung 90