Advertisement

Springer Nature is making Coronavirus research free. View research | View latest news | Sign up for updates

Die Flußspat- und Bleiglanzvererzung in Karbonatgesteinen der Sierra de Baza, Südspanien

  • 36 Accesses

  • 1 Citations

Abstract

The triassic sediments of the Sierra de Baza contain deposits of galena and fluorspar, partly under exploitation. After a survey of stratigraphy and tectonics of the mineralised series follows a description of the occurring ore types including stratiform banded “Zebra ores” and homogeneous vein fillings. The banded ores, because of their structures and textures, are regarded as synsedimentary formations, while the vein ore is presumed to be a product of mobilisation of the primary mineralisation.

This is a preview of subscription content, log in to check access.

Literatur

  1. Fallot, P., Sabaris, S. L.: Observations sur le trias bétique et ses algues calcaires, Mem. y. Comps Inst. Geol. Prov. Barcelona 11, 23–60 (1954)

  2. Folk, R. L.: Classification of carbonate rocks. A Symposium, published by the American Association of Petroleum Geologists, p. 62–84. Oklahoma, USA 1962

  3. Jansen, H.: De Geologie van die Sierra de Baza en van den angrenzenden Gebieden der Sierra Nevada de Los Filabrides (Zuid-Spanje), Academisch Proefschrift Thesis. Amsterdam: Verlag van Campen 1939

Download references

Author information

Additional information

Mitteilung aus dem Institut für Lagerstättenforschung der Technischen Universität Berlin.

Rights and permissions

Reprints and Permissions

About this article

Cite this article

Akin, H. Die Flußspat- und Bleiglanzvererzung in Karbonatgesteinen der Sierra de Baza, Südspanien. Mineral. Deposita 9, 61–68 (1974). https://doi.org/10.1007/BF00203278

Download citation