⁴⁰Ar/³⁹Ar dating of mesothermal, orogenic mineralization in a low-angle reverse shear zone in the Lower Palaeozoic of the Anglo-Brabant fold belt, Belgium

References

• Andre L., Deutsch S. and Michot J. Donnees geochronologiques concernant le developpement tectono-metamorphique du segment Caledonien Brabançon. Annales de la Societe géologique de Belgique, 104, 1981, 241–53.
   Google Scholar
• Andre L. and Deutsch S. Les porphyres de Quenast et de Lessines: geochronologie, geochimie isotopique et contribution au probleme de liage du socle precambrien du Massif du Brabant (Belgique). BulL Societe beige de Géologie, 93, 1984, 375–84.
   Google Scholar
• Annels A. E. and Roberts D. E. Turbidite-hosted gold mineral-ization at the Dolaucothi gold mines, Dyfed, Wales, United Kingdom. Econ. Geol., 84, 1989, 1293–314.
   Web of Science ®Google Scholar
• Arehart G. B. et al. 40Ar/39Ar, K/Ar and fission track geochrono-logy of sediment-hosted disseminated gold deposits at Post-Betze, Carlin Trend, northeastern Nevada. Econ. Geol., 88, 1993, 622–46.
   Web of Science ®Google Scholar
• Baksi A. K, Archibald D. A. and Farrar E. Intercalibration of 40Ar/39Ar dating standards. Chem. GeoL , 129, 1996, 307–24.
   Web of Science ®Google Scholar
• Bierlein F. P. and Crowe D. E. Phanerozoic orogenic lode gold deposits. Reviews in Econ. Geol., 13, 2000, 103–39.
   Google Scholar
• Blundell D. J., Freeman R. and Mueller S. A continent revealed, the European geotraverse (Cambridge: Cambridge University Press, 1992).
   Google Scholar
• Boven A. et al. 40Ar/39Ar study of plagioclases from the Rogaland anorthosite complex (southwest Norway): an attempt to understand argon ages in plutonic plagioclase. Chem. Geol., 176, 2001, 105–35.
   Web of Science ®Google Scholar
• Cocks L., McKerrow W. and Van Staal C. The margins of Avalonia. Geol. Mag., 134, 1997, 627–36.
   Web of Science ®Google Scholar
• Craw D., Windle S. J. and Angus P. V. Gold mineralization without quartz veins in a ductile-brittle shear zone, Macraes mine, Otago Schist, New Zealand. Mineral. Deposita, 34, 1999, 382–94.
   Web of Science ®Google Scholar
• Debacker T. N. Folds trending at various angles to the trans-port direction in the Marcq area, Brabant Massif, Belgium. Geologica Belgica, 2, 1999, 159–72.
   Google Scholar
• Debacker T. N. Palaeozoic deformation of the Brabant massif within eastern Avalonia: how, when & why? Ph.D. thesis, R.U. Gent, 2001.
   Google Scholar
• De Vos W. et al. A new geological map of the Brabant Massif, Belgium. Geol. Mag., 130, 1993, 605–11.
   Web of Science ®Google Scholar
• Dewaele S. et al. P-T-X variation along a polysulphide mineralized low-angle shear zone in the Lower Palaeozoic Anglo-Brabant fold belt (Belgium). In Mineral deposits at the beginning of the 21st century (Rotterdam: Balkema, 2001), 727–31.
   Google Scholar
• Duller P. R. et al. Gledinning deposit—an example of turbidite-hosted arsenic-antimony-gold mineralization in the Southern Uplands, Scotland. Trans. Instn Min. Metall. (Sect. B: AppL earth sci.), 106, 1997, B119–34.
   Web of Science ®Google Scholar
• Everaerts M. et al. Integrated geophysical/geological modelling of the western Brabant Massif and structural implications. Bull. Societe beige de Géologie, 105, 1997, 41–59.
   Google Scholar
• Gilbert L. A. and Foland K. A. The Mount Saint Hilaire plu-tonic complex: an occurrence of excess 40Ar and short intrusion history. Can. J. Earth Sci., 23, 1987, 948–58.
   Web of Science ®Google Scholar
• Goldfarb R. J., Groves D. I. and Gardoll S. Orogenic gold and geologic time: a global synthesis. Ore Geol. Rev., 18, 2001, 1–75.
   Web of Science ®Google Scholar
• Groves D. I. et al. Orogenic gold deposits: a proposed classifi-cation in the context of their crustal distribution and relationship to other gold deposit types. Ore Geol. Rev., 13, 1998, 7–27.
   Web of Science ®Google Scholar
• Hertogen J. and Verhaeren M. Studie van het magmatisme in het Massief van Brabant. Unpublished report ANRE VLA96-3.5.4, K.U. Leuven, Belgium, 1999, 24 p.
   Google Scholar
• Ilchik R. P. 40Ar/39Ar, K/Ar and fission track geochronology of sediment-hosted disseminated gold deposits at Post-Betze, Carlin Trend, northeastern Nevada—a discussion. Econ. Geol., 90, 1995, 208–10.
   Web of Science ®Google Scholar
• Ixer R. A. F., Pattrick R. A. D. and Stanley C. J. Geology, mineralogy and genesis of gold mineralization at the Calliachar-Urlar Burn, Scotland. Trans. Instn Min. Metall. (Sect. B: AppL earth sci.), 106, 1997, B99–108.
   Web of Science ®Google Scholar
• Kontak D. J. et al. Integrated model for the Meguma Group lode gold deposits, Nova Scotia, Canada. Geology, 18, 1990, 238–42.
   Web of Science ®Google Scholar
• Kontak D. J., Smith P. K. and Reynolds P. H. Geology and 40Ar/39Ar geochronolgy of the Beaver Dam gold deposit, Meguma Terrane, Nova Scotia, Canada: evidence for mineralization at 370 Ma. Econ. Geol., 88, 1993, 139–70.
   Web of Science ®Google Scholar
• Lowry D. et al. Sources of sulphur, metals and fluids in granitoid-related mineralization of the Southern Uplands, Scotland. Trans. Instn Min. Metall. (Sect. B: AppL earth sci.), 106, 1997, B157–68 .
   Web of Science ®Google Scholar
• Mason J. S., Fitches W. R. and Bevins R. E. Evidence of a pre-tectonic origin for the auriferous vein-type mineralization of the Dolgellau gold belt, north Wales. Trans. Instn Min. Metall. (Sect. B: AppL earth sci.), 108, 1999, B45–52.
   Web of Science ®Google Scholar
• Nguyen P. T. et al. Fault-valve behaviour in optimally orien-tated shear zones; an example at the Revenge gold mine, Kambalda, Western Australia. J. struct. Geol., 20, 1998, 1625–40.
   Web of Science ®Google Scholar
• O'Connor P. J. and Gallagher V. Gold prospectivity in the Caledonides of southeast Ireland: application of the upper-crustal reservoir model. Trans. Instn Min. Metall. (Sect. B: AppL earth sci.), 103, 1994, B175–87.
   Web of Science ®Google Scholar
• Pettke T., Diamond L. W. and Villa I. M. Mesothermal gold veins and metamorphic devolatilization in the nortwestern Alps: the temporal link. Geology, 27, 1999, 641–4.
   Web of Science ®Google Scholar
• Pharaoh T. C., England R. and Lee M. K. The concealed Caledonide basement of eastern England and the southern North Sea—a review. Studia Geophysica Geodaetica, 39, 1995, 330–46.
   Web of Science ®Google Scholar
• Pickering K. T. and Smith A. G. Arcs and backarc basins in the early Palaeozoic Iapetus Ocean. The Island Arc, 4, 1995, 1–67.
   Google Scholar
• Piessens K. et al. Fluid flow, alteration, and polysulphide min-eralization associated with a low-angle reverse shear zone in the Lower Palaeozoic of the Anglo-Brabant fold belt, Belgium. Tectonophys., 348, 2002, 73–92.
   Web of Science ®Google Scholar
• Rey P., Burg J.-P. and Casey M. The Scandinavian Caledonides, and their relationship to the Variscan belt. In Burg J.-P. and Ford M. eds Orogeny through time (London: Geological Society, 1997), 179–200. Spec. PubL geoL Soc. Lond. 121
   Google Scholar
• Shepherd T. J., Bottrell S. H. and Miller M. F. Fluid inclusion volatiles as an exploration guide to balck shale-hosted gold deposits, Dolgellau gold belt, north Wales, UK. J. geochem. Explor., 42, 1991, 5–24.
   Web of Science ®Google Scholar
• Sletten V. W. and Onstott T. C. The effect of the instability of muscovite during in vacuo heating on 40Ar/39Ar step-heating spectra. Geochim. Cosmochim. Acta, 62, 1998, 123–41.
   Web of Science ®Google Scholar
• Sintubin M. Arcuate fold and cleavage patterns in the south-eastern part of the Anglo-Brabant fold belt (Belgium): tectonic implications. Tectonophys., 309, 1999, 81–97.
   Web of Science ®Google Scholar
• Steed G. M. and Morris J. H. Isotopic evidence for the origins of a Caledonian gold-arsenopyrite-pyrite deposit at Clontibret, Ireland. Trans. Instn Min. Metall. (Sect. B: AppL earth sci.), 106, 1997, 109–18.
   Google Scholar
• Stegman C. L. Cobar deposits: still defying classification! SEG Newsletter, 44, 2000, 1, 15–26.
   Google Scholar
• Van Grootel G. et al. Timing of magmatism, foreland basin development, metamorphism and inversion in the Anglo-Brabant fold belt. Geol. Mag., 134, 1997, 607–16.
   Web of Science ®Google Scholar
• Verniers J. et al. The Cambrian to mid Devonian basin devel-opment, and deformation history of eastern Avalonia, east of the Midlands Microcraton: new data, and a review. In Winchester J., Verniers J. and Pharaoh T. eds Palaeozoic amalgamation of central Europe. Spec. PubL geol. Soc. Lond., 201, 2002, 47–93.
   Google Scholar
• Verniers J. et al. Cambrian—Ordovician—Silurian lithostrati-graphical units (Belgium). In Bultynck P. and Dejonghe L. eds Guide to a revised stratigraphical scale of Belgium. Geologica Belgica, 4, 2001, 5–39.
   Google Scholar
• Werner O. and Lippolt H. White mica 40Ar/39Ar ages of Erzgebirge metamorphic rocks: simulating the chronological results by a model of Variscan crustal imbrication. In Franke W. et al. eds Orogenic processes: quantification and modelling in the Variscan Belt (London: Geological Society, 2000), 323–36. Spec. PubL geol. Soc. Lond. 179
   Google Scholar
• Wilkinson J. J. et al. Gold remobilization by low-temperature brines: evidence from the Curraghinalt gold deposit, Northern Ireland. Econ. Geol., 94, 1999, 289–96.
   Google Scholar