Fluid mixing from below in unconformity-related hydrothermal ore deposits

Paul D. Bons, Tobias Fusswinkel, Enrique Gomez Rivas, Gregor Markl, Thomas Wagner, Benjamin Walter

Research output: Contribution to journalArticle

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Abstract

Unconformity-related hydrothermal ore deposits typically form by mixing of hot, deep, rock-buffered basement brines and cooler fluids derived from the surface or overlying sediments. Current models invoking simultaneous downward and upward flow of the mixing fluids are inconsistent with fluid overpressure indicated by fracturing and brecciation, fast fluid flow suggested by thermal disequilibrium, and small-scale fluid composition variations indicated by fluid inclusion analyses. We propose a new model where fluids first descend, then evolve while residing in pores and later ascend. We use the hydrothermal ore deposits of the Schwarzwald district in southwest Germany as an example. Oldest fluids reach the greatest depths, where long residence times and elevated temperatures allow them to equilibrate with their host rock, to reach high salinity, and to scavenge metals. Youngest fluids can only penetrate to shallower depths and can (partially) retain their original signatures. When fluids are released from different levels of the crustal column, these fluids mix during rapid ascent in hydrofractures to form hydrothermal ore deposits. Mixing from below during ascent provides a viable hydromechanical mechanism to explain the common phenomenon of mixed shallow and deep fluids in the formation of hydrothermal ore deposits.
Original languageEnglish
Pages (from-to)1035-1038
Number of pages4
JournalGeology
Volume42
Issue number12
Early online date15 Oct 2014
DOIs
Publication statusPublished - 1 Dec 2014

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ore deposit
unconformity
fluid
fluid composition
overpressure
basement rock
disequilibrium
fluid inclusion
host rock
fluid flow
residence time
salinity
metal
sediment

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Bons, P. D., Fusswinkel, T., Gomez Rivas, E., Markl, G., Wagner, T., & Walter, B. (2014). Fluid mixing from below in unconformity-related hydrothermal ore deposits. Geology, 42(12), 1035-1038. https://doi.org/10.1130/G35708.1

Fluid mixing from below in unconformity-related hydrothermal ore deposits. / Bons, Paul D.; Fusswinkel, Tobias; Gomez Rivas, Enrique; Markl, Gregor; Wagner, Thomas; Walter, Benjamin.

In: Geology, Vol. 42, No. 12, 01.12.2014, p. 1035-1038.

Research output: Contribution to journalArticle

Bons, PD, Fusswinkel, T, Gomez Rivas, E, Markl, G, Wagner, T & Walter, B 2014, 'Fluid mixing from below in unconformity-related hydrothermal ore deposits', Geology, vol. 42, no. 12, pp. 1035-1038. https://doi.org/10.1130/G35708.1
Bons PD, Fusswinkel T, Gomez Rivas E, Markl G, Wagner T, Walter B. Fluid mixing from below in unconformity-related hydrothermal ore deposits. Geology. 2014 Dec 1;42(12):1035-1038. https://doi.org/10.1130/G35708.1
Bons, Paul D. ; Fusswinkel, Tobias ; Gomez Rivas, Enrique ; Markl, Gregor ; Wagner, Thomas ; Walter, Benjamin. / Fluid mixing from below in unconformity-related hydrothermal ore deposits. In: Geology. 2014 ; Vol. 42, No. 12. pp. 1035-1038.
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abstract = "Unconformity-related hydrothermal ore deposits typically form by mixing of hot, deep, rock-buffered basement brines and cooler fluids derived from the surface or overlying sediments. Current models invoking simultaneous downward and upward flow of the mixing fluids are inconsistent with fluid overpressure indicated by fracturing and brecciation, fast fluid flow suggested by thermal disequilibrium, and small-scale fluid composition variations indicated by fluid inclusion analyses. We propose a new model where fluids first descend, then evolve while residing in pores and later ascend. We use the hydrothermal ore deposits of the Schwarzwald district in southwest Germany as an example. Oldest fluids reach the greatest depths, where long residence times and elevated temperatures allow them to equilibrate with their host rock, to reach high salinity, and to scavenge metals. Youngest fluids can only penetrate to shallower depths and can (partially) retain their original signatures. When fluids are released from different levels of the crustal column, these fluids mix during rapid ascent in hydrofractures to form hydrothermal ore deposits. Mixing from below during ascent provides a viable hydromechanical mechanism to explain the common phenomenon of mixed shallow and deep fluids in the formation of hydrothermal ore deposits.",
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