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Contributions to Mineralogy and Petrology

, Volume 162, Issue 1, pp 61–81 | Cite as

Mass transfer and porosity evolution during low temperature water–rock interaction in gneisses of the simano nappe: Arvigo, Val Calanca, Swiss Alps

  • Tobias Weisenberger
  • Kurt Bucher
Original Paper

Abstract

Late Alpine fissures and fractures in amphibolite-facies basement gneisses at Arvigo (Val Calanca, Swiss Alps) show distinct cm-sized reaction selvages parallel to the fracture walls that composed of subgreenschist facies assemblages produced by the interaction of water present in the fracture porosity with the old high-grade gneiss assemblages. The process of selvage or reaction-vein formation occurred in the brittle deformation regime and at temperatures characteristic of, first the prehnite-pumpellyite facies and then later of the zeolite facies. The vein formation occurred during uplift and cooling at very late stages of the Alpine orogeny. The reaction veins are composed of a selvage of altered gneiss on both sides of the central fracture and a central zone with fissure minerals that have been growing in the open fracture pore space. The central zone of the Arvigo veins contains an early assemblage with epidote, prehnite and chlorite and a late succession sequence of various species of zeolite. The veins of the Arvigo quarry are convincing evidence that fracture fluids in gneiss and granite have the potential to precipitate Ca–zeolite. This is an important find because many fluids recovered from deep continental drill holes and from geothermal energy exploration are found to be oversaturated in respect to a number of Ca–zeolite species. Vein formation during late uplift and cooling of the Alps occurred at continuously decreasing T and at hydrostatic pressure: (1) coexisting prehnite/epidote records temperatures of 330–380°C, (2) chlorite formation at temperature of 333 ± 32°C and (3) formation of zeolites <250°C. In the selvages the prime reaction is the replacement of plagioclase by albite along a sharp reaction front that separates the selvage from unaltered gneiss. In addition to albitisation, chloritisation of biotite is the second important reaction in the alteration process. The reactions release components for the formation of Ca–Al silicates. The water–rock interaction is associated with a depletion of Al, Si, Ca, Fe and K in the altered wall rock. The overall reaction is associated with an increase in porosity of up to 14.2 ± 2.2% in the selvage zone (altered wall rock), caused by the volume decrease during albitisation and the removal of biotite. The propagation of the sharp reaction front through the gneiss matrix occurred via a dissolution-reprecipitation mechanism. Zeolite formation is tied to the plagioclase alteration reaction in the rock matrix, which releases components for zeolite formation to a CO2-poor aqueous liquid.

Keywords

Water–Rock Interaction Laumontite Prehnite Reaction Vein Albitisation Arvigo Swiss Alps 

Notes

Acknowledgments

We are grateful to Giovanni and Alfredo Polti for permission to do field work in the active quarry. Special thanks go to the technicians and staff of the Institute of Geosciences, Mineralogy—Geochemistry, University of Freiburg and particularly H. Müller-Sigmund for her useful advise during EMP analyses and her patience with us at the electron microprobe. A. Leemann from the Swiss Federal Laboratories for Materials Testing and Research for impregnation of rock samples. We thank J. Ferry, L. Machiels and an anonymous reviewer for their very detailed and constructive comments that have greatly improved our paper and J. Hoefs for his editorial efforts and the editorial handling of the paper. A special thanks deserved to the Friedrich Rinne foundation for the financial support.

Supplementary material

410_2010_583_MOESM1_ESM.doc (203 kb)
Electronic supplementary material 1: (DOC 203 kb)
410_2010_583_MOESM2_ESM.eps (7.8 mb)
Electronic supplementary material 2: X-ray images (TS 12.1) showing a relict plagioclase grain surrounded by albite, showing increased porosity around plagioclase. (a) Ca element map. Plagioclase shows Ca enrichment relative to the core. (b) K element map. (c) Na element map. Same colour codes are used as in figure 6 (EPS 7989 kb)
410_2010_583_MOESM3_ESM.doc (124 kb)
Electronic supplementary material 3: (DOC 124 kb)
410_2010_583_MOESM4_ESM.doc (93 kb)
Electronic supplementary material 4: (DOC 93 kb)
410_2010_583_MOESM5_ESM.doc (68 kb)
Electronic supplementary material 5: (DOC 67 kb)
410_2010_583_MOESM6_ESM.eps (4.6 mb)
Electronic supplementary material 6: X-ray images showing element distribution in a prehnite aggregate indicating a Fe ⇔ Al substitution during growth. (a) Fe element map showing an iron-enrichment in the core. (b) Al element map showing an Al-depletion in the core. The same colour code are used as in figure 6 (EPS 4755 kb)
410_2010_583_MOESM7_ESM.doc (59 kb)
Electronic supplementary material 7: (DOC 59 kb)
410_2010_583_MOESM8_ESM.doc (90 kb)
Electronic supplementary material 8: (DOC 89 kb)
410_2010_583_MOESM9_ESM.eps (428 kb)
Electronic supplementary material 9: (a) Extra-framework cation (Ca+Sr+Mg-Na-K) distribution of zeolites. (b) R2+ - R+ - Si compositional diagram of zeolites. Si/Al ratio increases in chronologic order. Dashed area marks the chemical composition of zeolites found in granites and gneisses in the Swiss Alps (Weisenberger and Bucher 2010) (EPS 428 kb)

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© Springer-Verlag 2010

Authors and Affiliations

  1. 1.Institute of GeosciencesAlbert-Ludwigs-Universität FreiburgFreiburgGermany
  2. 2.Bureau of Economic Geology, Jackson School of GeosciencesThe University of Texas at AustinAustinUSA

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