Regional studies of dolomites and their included fluids: recognizing multiple chemically distinct fluids during the complex diagenetic history of Lower Carboniferous (Mississippian) rocks of the Irish Zn-Pb ore field

Author:

Johnson Aaron W.,Shelton Kevin L.,Gregg Jay M.,Somerville Ian D.,Wright Wayne R.,Nagy Zsolt R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference91 articles.

1. Ashton JH, Downing DT, Finlay S (1986) The geology of the Navan Zn-Pb orebody. In: Andrew CJ, Crowe RWA, Finley WM et al (eds) Geology and genesis of mineral deposits in Ireland. Irish Association for Economic Geology, Dublin, pp 243–280

2. Banks DA, Russell MJ (1992) Fluid mixing during ore deposition at the Tynagh base-metal deposit, Ireland. Eur J Mineral 4:921–931

3. Banks DA, Davies GR, Yardley BWD et al (1991) The chemistry of brines from an alpine thrust system in the central Pyrenees: an application of fluid inclusion analysis to the study of fluid behaviour in orogenesis. Geochim Cosmochim Acta 55:1021–1030

4. Banks DA, Boyce AJ, Samson IM (2002) Constraints on the origins of fluids forming Irish Zn-Pb-Ba deposits: evidence from the chemistry of fluid inclusions. Econ Geol 97:471–480

5. Becker SP, Nagy ZR, Johnson AW et al (2002) Relationship of evaporites to brine migration and carbonate hosted Zn-Pb mineralization in the Lower Carboniferous of southeastern Ireland. Geol. Soc Am Abs Prog 34:386

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