Abstract
The localisation and the metallogenesis of both hypogene sulphide and supergene non-sulphide mineralisation at the Skorpion Mine in southernmost Namibia have been — at least partly — structurally controlled. The hypogene Late Proterozoic hybrid VHMS/SHMS Zn-(Cu-Pb-Ba) ores of this district have formed in an environment, regionally controlled by the intersection of a 1st-order basin margin fault with a major transform/transfer fault. Bi-modal volcanism, anomalously high heat flow and hydrothermal activity have been the other regionally significant controls for the hypogene ore formation.
The supergene ores have formed from meteoric oxidation of base metal sulphides, channelled by factures of a late-stage brittle fault system. This anastomosing, steeply dipping fault array with a dextral oblique-slip reverse sense of movement has apparently formed in a (local?) transpressional crustal regime. The fault system opened abundant dilatational joints and fractures, providing improved permeability and an enlarged reactive rock surface of the host rocks. Meteoric waters have been able to percolate and convect along the fault system and to oxidise the hypogene ores to more than 700 m depth.
The fault system has been reactivated in neotectonic and even Recent times, as documented by faults truncating and off-setting the overburden. Other fault systems on land and offshore southwestern Africa show similar NNW-SSE strikes and might document the genetic connection of these (generally extensional) fault systems with the Skorpion Fault.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Borg G, Armstrong R (2002) Isotopic SHRIMP age dating of zircons from igneous basement and rhyolitic cover rocks at Skorpion, Southern Namibia. 11th IAGOD/Geocongress 2002, Extended abstract volume on CD-ROM. Geol. Surv. Namibia
Borg G, Kämner K, Buxton M, Armstrong R, Schalk Wvd (2003) Geology of the Skorpion non-sulphide deposit, southern Namibia. Economic Geology, 98:749–771
Borg G, Klein E, Kämner K., Botha R, Harney D (2004) Lithology, structure, and deep weathering characteristics of the supergene Skorpion zinc ore body. Geoscience Africa 2004, Abstract Volume 1, University of the Witwatersrand, Johannesburg, South Africa, 71–72.
Botha WJ, Alchin DJ (2002) Interpretation of the airborne DIGHEM geophysical survey data north of Rosh Pinah. In: 11th Quadrennial IAGOD Symposium and Geocongress 2002 (Ed. by L. Robb and R. Montjoie), CD-ROM, Geological Society of Namibia, Windhoek.
Frimmel HE (2000) The Pan African Gariep Belt in southwestern Namibia and western South Africa. Communications Geological Survey of Namibia, 12:197–209
Viola G, Andreoli M, Ben-Avraham Z, Stengel I, Reshef M (2004) Offshore mudvolcanoes and onland faulting in southwestern Africa. Earth Planetary Science Letters, 66:953–967
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 2005 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
Borg, G., Kämner, K., Klein, E. (2005). Structural control on the localisation and deep oxidation of the Skorpion supergene zinc deposit, Namibia. In: Mineral Deposit Research: Meeting the Global Challenge. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-27946-6_224
Download citation
DOI: https://doi.org/10.1007/3-540-27946-6_224
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-27945-7
Online ISBN: 978-3-540-27946-4
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)