|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Scientific Communications |
Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, Glasgow G75 0QF, Scotland
Outokumpu Tara Mines Ltd, Knockumber, Navan, County Meath, Ireland

Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, Glasgow G75 0QF, Scotland
Corresponding author: e-mail,
a.boyce{at}suerc.gla.ac.uk
We report sulfur and lead isotope analyses of mine
concentrates from Navan, the largest zinc deposit in Ireland. These samples,
each representing up to a million tonnes of ore, show very limited isotopic
variation, with mean
34S
= 13.6
± 2 per
mil (n =
20), and galena concentrate mean 206Pb/204Pb = 18.19 ±
0.03 (n =
7). Calculations suggest >90 percent of the Navan sulfides were derived
through bacteriogenic reduction of Mississippian seawater sulfate, whereas
metals were acquired from a local, orogenic crustal source beneath the
orebody. Enhanced bacterial activity was fundamental to ore deposition at
Navan: no bacteria, no giant ore deposit.
This article has been cited by other articles:
![]() |
C. D. Barrie, A. J. Boyce, A. P. Boyle, P. J. Williams, K. Blake, J. J. Wilkinson, M. Lowther, P. McDermott, and D. J. Prior On the growth of colloform textures: a case study of sphalerite from the Galmoy ore body, Ireland Journal of the Geological Society, May 1, 2009; 166(3): 563 - 582. [Abstract] [Full Text] [PDF] |
||||
![]() |
G. D. Bradshaw, S. M. Rowins, J. M. Peter, and B. E. Taylor Genesis of the Wolverine Volcanic Sediment-Hosted Massive Sulfide Deposit, Finlayson Lake District, Yukon, Canada: Mineralogical, Mineral Chemical, Fluid Inclusion, and Sulfur Isotope Evidence Economic Geology, January 1, 2008; 103(1): 35 - 60. [Abstract] [Full Text] [PDF] |
||||
![]() |
J.J. Wilkinson, C.E. Everett, A.J. Boyce, S.A. Gleeson, and D.M. Rye Intracratonic crustal seawater circulation and the genesis of subseafloor zinc-lead mineralization in the Irish orefield Geology, October 1, 2005; 33(10): 805 - 808. [Abstract] [Full Text] [PDF] |
||||
![]() |
G. Southam and J. A. Saunders The Geomicrobiology of Ore Deposits Economic Geology, September 1, 2005; 100(6): 1067 - 1084. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. J. Russell, A. J. Hall, A. J. Boyce, and A. E. Fallick 100th Anniversary Special Paper: * > On Hydrothermal Convection Systems and the Emergence of Life Economic Geology, May 1, 2005; 100(3): 419 - 438. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. J. Wilkinson, D. J. Weiss, T. F. D. Mason, and B. J. Coles ZINC ISOTOPE VARIATION IN HYDROTHERMAL SYSTEMS: PRELIMINARY EVIDENCE FROM THE IRISH MIDLANDS ORE FIELD Economic Geology, May 1, 2005; 100(3): 583 - 590. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. W. Moreau, R. I. Webb, and J. F. Banfield Ultrastructure, aggregation-state, and crystal growth of biogenic nanocrystalline sphalerite and wurtzite American Mineralogist, July 1, 2004; 89(7): 950 - 960. [Abstract] [Full Text] [PDF] |
||||
![]() |
C. E. Everett, C. E. Everett, D. M. Rye, and R. M. Ellam Source or Sink? An Assessment of the Role of the Old Red Sandstone in the Genesis of the Irish Zn-Pb Deposits Economic Geology, January 1, 2003; 98(1): 31 - 50. [Abstract] [Full Text] [PDF] |
||||
![]() |
R. J. Blakeman, R. J. Blakeman, J. H. Ashton, A. J. Boyce, A. E. Fallick, and M. J. Russell Timing of Interplay between Hydrothermal and Surface Fluids in the Navan Zn + Pb Orebody, Ireland: Evidence from Metal Distribution Trends, Mineral Textures, and {delta}34S Analyses Economic Geology, January 1, 2002; 97(1): 73 - 91. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |