Abstract
Displacement of the daughter isotope by α-recoil results in an open system on the nanoscale. For a heterogeneous distribution of U and Th, this redistribution of intermediate and stable daughter isotopes results in subvolumes with a deficit of Pb and others with an excess of Pb. Whether such heterogeneities affect the analyzed U–Pb system depends on: (1) the volume of the analyzed sample, (2) the degree and scale of heterogeneity in the U and Th distribution, and (3) the analytical procedure. Spatial separation of parent and daughter through α-recoil affects the U–Pb systematics of leached samples, where leaching gives access to domains less than 1 μm wide. Anomalous data patterns originating from recoil induced parent-to-daughter fractionation are more important if there are strong heterogeneities in the U and Th distribution, whereby Pb excess appears more pronounced than Pb deficit. Fractionation of parent and daughter elements through selective dissolution of U-REE-rich growth zones in zircon and U-inclusions in columbite, as well as the presence of U–Th-rich micro-inclusions in silicates dated using a step-leaching scheme, may result in anomalous 207Pbrad/206Pbrad, scattered 206Pbrad/238U and 207Pbrad/235U, and reverse discordance. The accumulated structural damage controls the leaching and dissolution behavior, but may also influence the non-stoichiometric element mobilization during sputtering or ablation in the analysis of U-rich samples by SHRIMP and LA-MC-ICP-MS.
Similar content being viewed by others
References
Aldrich LT, Davis GL, Tilton GR, Wetherill GW (1956) Radioactive ages of minerals from the Brown Derby Mine and the Quartz Creek Granite near Gunnison, Colorado. J Geophys Res 61:215-232
Black LP, Kinny PD, Sheraton JW (1991) The difficulties of dating mafic dykes: an Antarctic example. Contrib Mineral Petrol 109:183–194
Chen F, Siebel W, Satir M (2002) Zircon U-Pb and Pb isotope fractionation during stepwise HF acid leaching and geochronological implications. Chem Geol 191:155–164
Cerny P, Chapman R, Göd R, Niedermayr G, Wise MA (1989) Exsolution intergrowths of titanian ferrocolumbite and niobian rutile from the Weinebene spodumene pegmatites, Carinthia, Austria. Mineral Petrol 40:197–206
Claesson S, Williams IS (1987) Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides: I. conventional U–Pb zircon and Sm–Nd whole rock data. Contrib Mineral Petrol 97:196–204
Compston W, Williams IS, Meyer C (1984) U-Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass-resolution ion microprobe. J Geophys Res 89: B525–B534
Corfu F (2000) Extraction of Pb with artificially too-old ages during stepwise dissolution experiments on Archean zircon. Lithos 53:279–291
Dahl PS and Frei R (1995) Step-leach Pb-Pb dating of inclusion-bearing garnet and staurolite, with implications for Early Proterozoic tectonism in the Black Hills collisional orogen, South Dakota, United States. Geology 26:111–114
Davis DW, Krogh TE (2000) Preferential dissolution of 234U and radiogenic Pb from alpha-recoil-damaged lattice sites in zircon; implications for thermal histories and Pb isotopic fractionation in the near surface environment. Chem Geol 172:41–58
Frei R, Biino GG, Prospert C (1995) Dating a Variscan pressure-temperature loop with staurolite. Geology 23:1095–1098
Frei R, Villa IM, Nägler ThF, Kramers JD, Przybylowicz WJ, Prozesky VM, Hofmann BA, Kamber BS (1997) Single mineral dating by the Pb-Pb step-leaching method: assessing the mechanism. Geochim Cosmochim Acta 61:393–414
Geisler T, Ulonska M, Schleicher H, Pidgeon RT, van Bronswijk W (2001) Leaching and differential recrystallization of metamict zircon under experimental hydrothermal conditions. Contrib Mineral Petrol 141:53–65
Geisler T (2002) Isothermal annealing of partially metamict zircon: evidence for a three-stage recovery process. Phys Chem Minerals 29:420–429
Goetze J, Kempe U, Habermann D, Nasdala L, Neuser RD, Richter DK (1999) High resolution cathodoluminescence combined with SHRIMP ion probe measurements of detrital zircons. Mineral Mag 63:179–187
Hanchar JM, Miller CF (1993) Zircon zonation patterns as revealed by cathodoluminescence and backscattered electron images: implications for interpretation of complex crustal histories. Chem Geol 110:1–13.
Krogh TE (1973) A low-contamination method for hydrothermal decomposition method of zircon and extraction of U and Pb for isotopic age determination. Geochim Cosmochim Acta 37:485–494
Krogh TE (1982a) Improved accuracy of U-Pb zircon dating by selection of more concordant fractions using a high gradient magnetic separation technique. Geochim Cosmochim Acta 46:631–635
Krogh TE (1982b) Improved accuracy of U-Pb zircon ages by the creation of more concordant systems using an air abrasion technique. Geochim Cosmochim Acta 46:637–649
Kurz S (2000) Hydrothermale Alterationsprozesse in Zirkonen — Isotopengeologische und geochemische Implikationen. PhD Thesis, Univ Göttingen, 112 pp
Mattinson JM (1994) A study of complex discordance in zircons using step-wise dissolution techniques. Contrib Mineral Petrol 116:117–129
Mattinson JM (1997) Analysis of zircon by multi-step partial dissolution: the good, the bad, and the ugly. Geol Assoc Can Meet, Ottawa'97, Abstract A98
Mattinson JM (2000) U-Pb zircon analysis by "chemical abrasion": combined high-temperature-annealing and partial dissolution analysis. EOS Trans Am Geophys Union 81:S27
Mattinson JM (2001) Zircon radiation damage, annealing, dissolution, and Pb diffusion. 11th Annual VM Goldschmidt Conf, Abstr vol, 3625.pdf
Mattinson JM, Gaubard CM, Parkinson DL, McLelland WC (1996) U-Pb reverse discordance in zircons: the role of fine-scale oscillatory zoning and sub-microscopic transport of Pb. Am Geophys Union Geophys Monogr 95:355–370
McClelland WC, Mattinson JM (1996) Resolving high precision U-Pb ages from Tertiary plutons with complex zircon systematics. Geochim Cosmochim Acta 60:3955–3965
Meldrum A, Boatner LA, Weber WJ, Ewing RC (1998) Radiation damage in zircon and monazite. Geochim Cosmochim Acta 62:2509–2520
Murakami T, Chakoumakos BC, Ewing RC, Lumpkin GR, Weber WJ (1991) Alpha-decay event damage in zircon. Am Mineral 76:1510–1532
Nasdala L, Wenzel M, Vavra G, Irmer G, Wenzel T, Kober B (2001) Metamictisation of natural zircon: accumulation versus thermal annealing of radioactivity-induced damage. Contrib Mineral Petrol 141:125–144
Parrish RR (1987) An improved micro-capsule for zircon dissolution in U–Pb geochronology. Chem Geol 66:99–102
Petit J-C, Dran J-C, Paccanella A, Della Mea G (1989) Structural dependence of crystalline silicate hydration during aqueous dissolution. Earth Planet Sci Lett 93:292–298
Romer RL, Smeds S-A (1994) Implications of U-Pb ages of columbite-tantalites from granitic pegmatites for the Palaeoproterozoic accretion of 1.90–1.85 Ga magmatic arcs to the Baltic Shield. Precambrian Res 67:141–158
Romer RL, Smeds S-A (1996) U–Pb columbite ages of pegmatites from Sveconorwegian terranes in southwestern Sweden. Precambrian Res 76:15–30
Romer RL, Smeds S-A (1997) U–Pb columbite chronology of post-kinematic Palaeoproterozoic pegmatites in Sweden. Precambrian Res 82:85–99
Romer RL, Wright JE (1992) U–Pb dating of columbite: a geochronologic tool to date magmatism and ore deposits. Geochim Cosmochim Acta 56:2137–2142
Romer RL, Smeds S-A, Cerny P (1996) Crystal-chemical and genetic controls of U–Pb systematics of columbite-tantalite. Mineral Petrol 57:243–260
Sergeev SA, Meier M, Steiger RH (1995) Improving the resolution of single-grain U/Pb dating by use of zircon extracted from feldspar; application to the Variscan magmatic cycle in the Central Alps. Earth Planet Sci Lett 134:37–51
Sergeev SA, Komarov AN, Bickel RA, Steiger RH (1997) A new microtome for cutting hard submilimeter-sized crystalline objects for promoting high-resolution instrumental microanalysis. Eur J Mineral 9:449–456
Smith S (2001) Geochemistry and geochronology of rare-element pegmatites from the Superior province of Canada. PhD Thesis, The Open University, Milton Keynes, UK
Steiger RH, Bickel RA, Meier M (1993) Conventional U-Pb dating of single fragments of zircon for petrogenetic studies of Phanerozoic granitoids. Earth Planet Sci Lett 115:197–209
Tagami T, Carter A, Hurford AJ (1996) Natural long-term annealing of the zircon fission-track system in Vienna basin deep borehole samples: constraints upon the partial annealing zone and closure temperature. Chem Geol 130:147–157
Tilton GR (1960) Volume diffusion as a mechanism for discordant lead ages. J Geophys Res 65:178–190
Todt WA, Büsch W (1981) U–Pb investigations on zircons from pre-Variscan gneisses, I. A study from the Schwarzwald, West Germany. Geochim Cosmochim Acta 45:1789–1801
Trachenko KO, Dove MT, Salje EKH (2001) Atomistic modeling of radiation damage in zircon. J Phys Condens Matter 13:947–952
Trindle AG, Breaks FW (1998) Oxide minerals of the Separation Rapids rare-element granitic pegmatite group, northwestern Ontario. Can Mineral 36:609–635
Trindle AG, Breaks FW, Webb PC (1998) Wodginite-group minerals from the Separation Rapids rare-element granitic pegmatite group, northwestern Ontario. Can Mineral 36:637–658
Uher P, Cerny P, Chapman R, Hatar J, Miko O (1998) Evolution of Nb,Ta-oxide minerals in the Prasiva granitic pegmatites, Slovakia. II. External hydrothermal Pb,Sb overprint. Can Mineral 36:535–545
Vavra G, Gebauer D, Schmid R (1996) Multiple zircon growth and recrystallization during polyphase Late carboniferous to Triassic metamorphism of the Ivrea Zone (Southern Alps): an ion microprobe (SHRIMP) study. Contrib Mineral Petrol 122:337–358
Vavra G, Schmid R, Gebauer D (1999) Internal morphology, habit and U–Th–Pb microanalysis of amphibolite-to-granulite facies zircons: geochronology of the Ivrea Zone (Southern Alps). Contrib Mineral Petrol 134:380–404
Wasserburg GJ (1963) Diffusion processes in lead-uranium systems. J Geophys Res 68:4823–4845
Weber WJ, Ewing RC, Wang L-M (1994) The radiation-induced crystalline-to-amorphous transition in zircon. J Mater Res 9:688–698
White NM, Parrish RR, Bickle MJ, Najman YMR, Burbank D, Maithani A (2001) Metamorphism and exhumation of the NW Himalaya constrained by U-Th-Pb analyses of detrital monazite grains from early foreland basin sediments. J Geol Soc Lond 158:625–635
Wiedenbeck M (1995) An example of reverse discordance during ion microprobe zircon dating: an artifact of enhanced ion yields from a radiogenic labile Pb. Chem Geol 160:201–224
Ziegler JF, Biersack JP, Littmark U (1985) The stopping and range of ions in solids. In: Ziegler JF (ed) The stopping and range of ions in matter, vol 1. Pergamon, Oxford
Acknowledgements
I thank Sten Littmann (GFZ Potsdam) for Fig. 2b, c. The SEM images of leached columbite-tantalite crystals were made by Ulf Sturesson (Uppsala) in the course of an earlier project (with Sten-Anders Smeds, Uppsala). I am grateful to James M Mattinson (Santa Barbara) and Fernando Corfu (Oslo) for detailed and constructive reviews.
Author information
Authors and Affiliations
Corresponding author
Additional information
Editorial responsibility: J. Hoefs
Rights and permissions
About this article
Cite this article
Romer, R.L. Alpha-recoil in U–Pb geochronology: effective sample size matters. Contrib Mineral Petrol 145, 481–491 (2003). https://doi.org/10.1007/s00410-003-0463-0
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00410-003-0463-0