The mount black lead-zinc deposit, a probable Mississippi valley-type sulphide occurrence at cooleman plains, southern New South Wales
Title:
The mount black lead-zinc deposit, a probable Mississippi valley-type sulphide occurrence at cooleman plains, southern New South Wales
Author:
Ashley, P. M. Creelman, R. A.
Appeared in:
Australian journal of earth sciences
Paging:
Volume 22 (1975) nr. 4 pages 423-433
Year:
1975
Contents:
The Mount Black lead-zinc deposit at Cooleman Plains, southern New South Wales, occurs in the uppermost part of the moderately folded, weakly metamorphosed, Upper Silurian Cooleman Limestone. A joint-controlled collapse-breccia zone interpreted as a palaeokarst structure has been partly replaced by quartz, sphalerite, galena, and a little chalcopyrite, pyrite, marcasite, tetrahedrite, arseno-pyrite, and mackinawite. These minerals show evidence of having encrusted and replaced limestone fragments in the breccia. Oxidic Zn, Pb, Cu, and Fe minerals have formed by the near-surface oxidation of the sulphides. Petrographic and field evidence indicates that the quartz and sulphides were deposited mainly by encrustation and precipitation from saline solutions (possibly diagenetically expelled connate brines) in cavities, probably at low temperature at shallow depth. The deposit has many similarities to Mississippi Valley-type lead-zinc deposits.
Journal description