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Tracing seawater evaporation and evaporite dissolution in the Zambian Copperbelt: evidence from crush-leach analysis of fluid inclusions and stable isotopes

Tracing seawater evaporation and evaporite dissolution in the Zambian Copperbelt: evidence from crush-leach analysis of fluid inclusions and stable isotopes
Tracing seawater evaporation and evaporite dissolution in the Zambian Copperbelt: evidence from crush-leach analysis of fluid inclusions and stable isotopes
Fluids in the Zambian Copperbelt have been investigated by sampling different generations of vein material from numerous deposits across the classic mining district and currently explored Western Domes region. Veins were segregated into pre kinematic, pre-syn kinematic and post kinematic groups based on their relationship to host rock fabrics. Crush-leach halogen data indicates the presence of two main fluid types, one with Cl/Br < seawater, indicative of a fluid derived from residual evaporated seawater which dominate the pre and pre-syn kinematic samples, and one with Cl/Br > seawater, characteristic of a fluid containing a component derived from dissolved evaporites which dominated the post-kinematic vein generation. Halogen data suggests fluids were ultimately derived from strong evaporation of seawater beyond the carnalite saturation point. Cation data suggests significant water-rock interaction consistent with hydrothermal alteration assemblages. delta Cl-37 of fluid leachate is close to 0 for all samples, suggesting an ultimate seawater source of chlorine. delta O-18(fluid) is variable between similar to -3 and +11, probably reflecting different amounts of water-rock equilibration and different residence times. Isotopically light delta C-13 and delta D signatures reflect oxidation of organic matter. Vein material with delta C-13 similar to Neoproterozoic carbonates reflects buffering by host rock carbonate sequences.
Zambia, Copperbelt, fluids, halogens, stable isotopes, thermochemical sulfate reduction, mineralization, fractionation, deposits, origin, quartz, brines, basin
978-91-7403-207-9
659-662
Uppsala University
Roberts, S.
f095c7ab-a37b-4064-8a41-ae4820832856
Nowecki, J.
0e3552f2-8ffb-4252-8064-87a2ce57e624
Gleeson, S.
93178ca5-c840-4491-8951-9ef3ecd08b2d
Boyce, A.
5ce4f091-5fa3-4841-bef7-6b6b2b032b5d
Jonsson, E.
Roberts, S.
f095c7ab-a37b-4064-8a41-ae4820832856
Nowecki, J.
0e3552f2-8ffb-4252-8064-87a2ce57e624
Gleeson, S.
93178ca5-c840-4491-8951-9ef3ecd08b2d
Boyce, A.
5ce4f091-5fa3-4841-bef7-6b6b2b032b5d
Jonsson, E.

Roberts, S., Nowecki, J., Gleeson, S. and Boyce, A. (2013) Tracing seawater evaporation and evaporite dissolution in the Zambian Copperbelt: evidence from crush-leach analysis of fluid inclusions and stable isotopes. In, Jonsson, E. (ed.) Mineral Deposit Research for High-Tech World, Vols. 1-4. 12th Biennial SGA Meeting on Mineral Deposit Research for a High-Tech World (11/04/13 - 14/08/13) Uppsala, SE. Uppsala University, pp. 659-662.

Record type: Book Section

Abstract

Fluids in the Zambian Copperbelt have been investigated by sampling different generations of vein material from numerous deposits across the classic mining district and currently explored Western Domes region. Veins were segregated into pre kinematic, pre-syn kinematic and post kinematic groups based on their relationship to host rock fabrics. Crush-leach halogen data indicates the presence of two main fluid types, one with Cl/Br < seawater, indicative of a fluid derived from residual evaporated seawater which dominate the pre and pre-syn kinematic samples, and one with Cl/Br > seawater, characteristic of a fluid containing a component derived from dissolved evaporites which dominated the post-kinematic vein generation. Halogen data suggests fluids were ultimately derived from strong evaporation of seawater beyond the carnalite saturation point. Cation data suggests significant water-rock interaction consistent with hydrothermal alteration assemblages. delta Cl-37 of fluid leachate is close to 0 for all samples, suggesting an ultimate seawater source of chlorine. delta O-18(fluid) is variable between similar to -3 and +11, probably reflecting different amounts of water-rock equilibration and different residence times. Isotopically light delta C-13 and delta D signatures reflect oxidation of organic matter. Vein material with delta C-13 similar to Neoproterozoic carbonates reflects buffering by host rock carbonate sequences.

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More information

Published date: 2013
Venue - Dates: 12th Biennial SGA Meeting on Mineral Deposit Research for a High-Tech World, Uppsala, Sweden, 2013-04-11 - 2013-08-14
Keywords: Zambia, Copperbelt, fluids, halogens, stable isotopes, thermochemical sulfate reduction, mineralization, fractionation, deposits, origin, quartz, brines, basin
Organisations: Geochemistry

Identifiers

Local EPrints ID: 367876
URI: http://eprints.soton.ac.uk/id/eprint/367876
ISBN: 978-91-7403-207-9
PURE UUID: 19991e0f-b8c9-4ffd-92f1-7533e60f52b1
ORCID for S. Roberts: ORCID iD orcid.org/0000-0003-4755-6703

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Date deposited: 08 Aug 2014 12:54
Last modified: 19 Mar 2022 02:33

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Contributors

Author: S. Roberts ORCID iD
Author: J. Nowecki
Author: S. Gleeson
Author: A. Boyce
Editor: E. Jonsson

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