The Rb–Sr Method

Alan P. Dickin

doi:10.1017/9781316163009.004

Chapter 3 - The Rb–Sr Method

Published online by Cambridge University Press: 01 February 2018

Alan P. Dickin

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Alan P. Dickin: Affiliation:
McMaster University, Ontario

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Information: Radiogenic Isotope Geology , pp. 40 - 66

DOI: https://doi.org/10.1017/9781316163009.004 [Opens in a new window]

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Print publication year: 2018

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References

Albarede, F., Michard, A., Minster, J. F. and Michard, G. (1981). ⁸⁷Sr/⁸⁶Sr ratios in hydrothermal waters and deposits from the East Pacific Rise at 21 °N. Earth Planet. Sci. Lett. 55, 229–36.CrossRef Google Scholar

Aleinikoff, J. N., Horton, J. W., Drake, A. A. et al. (2004). Deciphering multiple Mesoproterozoic and Paleozoic events recorded in zircon and titanite from the Baltimore Gneiss, Maryland: SEM imaging, SHRIMP U-Pb geochronology, and EMP analysis. In: Tollo, R. P., Corriveau, L., McLelland, J. and Bartholomew, M. J. (Eds) Proterozoic tectonic evolution of the Grenville orogen in North America: An introduction: Geol. Soc. America Mem. 197, 411–34.Google Scholar

Allegre, C. J., Louvat, P., Gaillardet, J. et al. (2010). The fundamental role of island arc weathering in the oceanic Sr isotope budget. Earth Planet. Sci. Lett. 292, 51–6.CrossRef Google Scholar

Amelin, Y. and Zaitsev, A. N. (2002). Precise geochronology of phoscorites and carbonatites: The critical role of U-series disequilibrium in age interpretations. Geochim. Cosmochim. Acta 66, 2399–419.Google Scholar

Ando, A., Nakano, T., Kawahata, H., Yokoyama, Y. and Khim, B. K. (2010). Testing seawater Sr isotopic variability on a glacial–interglacial timescale: An application of latest high-precision thermal ionization mass spectrometry. Geochem. J. 44, 347–57.Google Scholar

Armstrong, R. L. (1971). Glacial erosion and the variable isotopic composition of strontium in sea water. Nature Phys. Sci. 230, 132–3.Google Scholar

Asmerom, Y., Jacobsen, S. B., Knoll, A. H., Butterfield, N. J. and Swett, K. (1991). Strontium isotopic variations of Neoproterozoic seawater: implications for crustal evolution. Geochim. Cosmochim. Acta 55, 2883–94.Google Scholar

Basu, A. R., Jacobsen, S. B., Poreda, R. J., Dowling, C. B. and Aggarwal, P. K. (2001). Large groundwater strontium flux to the oceans from the Bengal Basin and the marine strontium isotope record. Science 293, 1470–3.Google Scholar

Beck, A. J., Charette, M. A., Cochran, J. K., Gonneea, M. E. and Peucker-Ehrenbrink, B. (2013). Dissolved strontium in the subterranean estuary–Implications for the marine strontium isotope budget. Geochim. Cosmochim. Acta 117, 33–52.Google Scholar

Becker, T. W., Conrad, C. P., Buffett, B. and Müller, R. D. (2009). Past and present seafloor age distributions and the temporal evolution of plate tectonic heat transport. Earth Planet. Sci. Lett. 278, 233–42.Google Scholar

Begemann, F., Ludwig, K. R., Lugmair, G. W. et al. (2001). Call for an improved set of decay constants for geochronological use. Geochim. Cosmochim. Acta 65, 111–21.Google Scholar

Birck, J. L. and Allegre, C. J. (1978). Chronology and chemical history of the parent body of basaltic achondrites studied by the ⁸⁷Rb)⁸⁷Sr method. Earth Planet. Sci. Lett. 39, 37–51.Google Scholar

Blum, J. D. and Erel, Y. (1995). A silicate weathering mechanism linking increases in marine ⁸⁷Sr/⁸⁶Sr with global glaciation. Nature 373, 415–18.Google Scholar

Blum, J. D., Gazis, C. A., Jacobsen, A. D. and Chamberlain, C. P. (1998). Carbonate versus silicate weathering in the Raikot watershed within the High Himalayan Crystalline Series. Geology 26, 411–4.Google Scholar

Brand, U. and Veizer, J. (1980). Chemical diagenesis of a multicomponent carbonate system – 1: Trace elements. J. Sed. Petrol. 50, 1219–36.Google Scholar

Brannon, J. C., Podosek, F. A. and McLimans, R. K. (1992). Alleghenian age of the Upper Mississippi Valley zinc–lead deposit determined by Rb–Sr dating of sphalerite. Nature 356, 509–11.Google Scholar

Brass, G. W. (1976). The variation of the marine ⁸⁷Sr/⁸⁶Sr during Phanerozoic time: interpretation using a flux model. Geochim. Cosmochim. Acta 40, 721–30.Google Scholar

Brinkman, G. A., Aten, A. H. W. and Veenboer, J. T. (1965). Natural radioactivity of K-40, Rb-87 and Lu-176. Physica 31, 1305–19.Google Scholar

Brooks, C., Hart, S. R., Hofmann, A. and James, D. E. (1976a). Rb–Sr mantle isochrons from oceanic regions. Earth Planet. Sci. Lett. 32, 51–61.Google Scholar

Brooks, C., James, D. E. and Hart, S. R. (1976b). Ancient lithosphere: its role in young continental volcanism. Science 193, 1086–94.Google Scholar

Brown, E. H. (1971). Phase relations of biotite and stilpnomelane in the green-schist facies. Contrib. Mineral. Petrol. 31, 275–99.Google Scholar

Burke, W. H., Denison, R. E., Hetherington, E. A. et al. (1982). Variations of seawater ⁸⁷Sr/⁸⁶Sr throughout Phanerozoic time. Geology 10, 516–19.Google Scholar

Butterfield, D. A., Nelson, B. K., Wheat, C. G., Mottl, M. J. and Roe, K. K. (2001). Evidence for basaltic Sr in midocean ridge-flank hydrothermal systems and implications for the global oceanic Sr isotope balance. Geochim. Cosmochim. Acta 65, 4141–53.Google Scholar

Catanzaro, E. J., Murphy, T. J., Garner, E. L. and Shields, W. R. (1969). Absolute isotopic abundance ratio and atomic weight of terrestrial rubidium. J. Res. NBS 73A, 511–16.CrossRef Google Scholar PubMed

Chaudhuri, S. and Clauer, N. (1986). Fluctuations of isotopic composition of strontium in seawater during the Phanerozoic eon. Chem. Geol. (Isot. Geosci. Sect.) 59, 293–303.CrossRef Google Scholar

Christensen, J. N., Halliday, A. N., Leigh, K. E., Randell, R. N. and Kesler, S. E. (1995a). Direct dating of sulfides by Rb–Sr: a critical test using the Polaris Mississippi Valley-type Zn–Pb deposit. Geochim. Cosmochim. Acta 59, 5191–7.Google Scholar

Christensen, J. N., Halliday, A. N., Vearncombe, J. R. and Kesler, S. E. (1995b). Testing models of large-scale fluid flow using direct dating of sulfides: Rb–Sr evidence for early dewatering and formation of Mississippi Valley-type deposits, Canning Basin, Australia. Econ. Geol. 90, 877–84.Google Scholar

Clark, S. P. C. and Jager, E. (1969). Denudation rate in the Alps from geochronologic and heat flow data. Amer. J. Sci. 267, 1143–60.Google Scholar

Clauer, N. (1979). A new approach to Rb)Sr dating of sedimentary rocks. In: Jager, E. and Hunziker, J. C. (Eds) Lectures in Isotope Geology. Springer, pp. 30–51.Google Scholar

Clauer, N., Keppens, E. and Stille, P. (1992). Sr isotopic constraints on the process of glauconitization. Geology 20, 133–6.Google Scholar

Clemens, S. C., Farrell, J. W. and Gromet, L. P. (1993). Synchronous changes in seawater strontium isotope composition and global climate. Nature 363, 607–10.Google Scholar

Clemens, S. C., Gromet, L. P. and Farrell, J. W. (1995). Artifacts in Sr isotope records. Nature 373, 201.Google Scholar

Cliff, R. A. (1985). Isotope dating in metamorphic belts. J. Geol. Soc. Lond. 142, 97–110.Google Scholar

Coggon, R. M., Teagle, D. A., Smith-Duque, C. E., Alt, J. C. and Cooper, M. J. (2010). Reconstructing past seawater Mg/Ca and Sr/Ca from mid-ocean ridge flank calcium carbonate veins. Science 327, 1114–17.Google Scholar

Compston, W. and Jeffery, P. M. (1959). Anomalous common strontium in granite. Nature 184, 1792–3.CrossRef Google Scholar

Compston, W. and Pidgeon, R. T. (1962). Rubidium–strontium dating of shales by the total-rock method. J. Geophys. Res. 67, 3493–502.Google Scholar

Coogan, L. A. (2009). Altered oceanic crust as an inorganic record of paleoseawater Sr concentration. Geochem. Geophys. Geosys. 10 (4), 1–11.Google Scholar

Coogan, L. A. and Dosso, S. E. (2015). Alteration of ocean crust provides a strong temperature dependent feedback on the geological carbon cycle and is a primary driver of the Sr-isotopic composition of seawater. Earth Planet. Sci. Lett. 415, 38–46.Google Scholar

Cowie, J. W. and Johnson, M. R. W. (1985). Late Precambrian and Cambrian geological time-scale. In: Snelling, N. J. (Ed.) The chronology of the geological record. Mem. Geol. Soc. Lond. 10, 47–64.Google Scholar

Dasch, E. J. and Biscaye, P. E. (1971). Isotopic composition of strontium in Cretaceous-to-Recent, pelagic foraminifera. Earth Planet. Sci. Lett. 11, 201–4.Google Scholar

Davis, A. C., Bickle, M. J. and Teagle, D. A. (2003). Imbalance in the oceanic strontium budget. Earth Planet. Sci. Lett. 211, 173–87.Google Scholar

Davis, D. W., Gray, J. and Cumming, G. L. (1977). Determination of the ⁸⁷Rb decay constant. Geochim. Cosmochim. Acta 41, 1745–9.Google Scholar

Del Moro, A., Puxeddu, M. and Villa, I. M. (1982). Rb–Sr and K–Ar ages on minerals at temperatures of 300–400 °C from deep wells in the Larderello geothermal field (Italy). Contrib. Mineral. Petrol. 81, 340–9.Google Scholar

DePaolo, D. J. (1987). Correlating rocks with strontium isotopes. Geotimes 32, 16–18.Google Scholar

Derry, L. A., Keto, L. S., Jacobsen, S. B., Knoll, A. H. and Swett, K. (1989). Sr isotopic variations in Upper Proterozoic carbonates from Svalbard and East Greenland. Geochim. Cosmochim. Acta 53, 2331–9.CrossRef Google Scholar PubMed

Dia, A. N., Cohen, A. S., O'Nions, R. K. and Shackleton, N. J. (1992). Seawater Sr isotope variation over the past 300 ka and influence of global climate cycles. Nature 356, 786–8.Google Scholar

Dodson, M. H. (1973). Closure temperature in cooling geochronological and petrological systems. Contrib. Mineral. Petrol. 40, 259–74.Google Scholar

Dodson, M. H. (1979). Theory of cooling ages. In: Jager, E. and Hunziker, J. C. (Eds) Lectures in Isotope Geology. Springer, pp. 194–202.Google Scholar

Dunoyer de Segonzac, G. (1969). Les mineraux argileux dans la diagenese. Passage au metamorphisme. Mem. Serv. Carte Geol. Alsace Lorraine 29, 320 pp.Google Scholar

Edmond, J. M., Measures, C., McDuff, R. E. et al. (1979). Ridge crest hydrothermal activity and the balances of the major and minor elements in the ocean: the Galapagos data. Earth Planet. Sci. Lett. 46, 1–18.CrossRef Google Scholar

Elderfield, H. and Gieskes, J. M. (1982). Sr isotopes in interstitial waters of marine sediments from Deep Sea Drilling Project cores. Nature 300, 493–7.Google Scholar

Elderfield, H., Wheat, C. G., Mottl, M. J., Monnin, C. and Spiro, B. (1999). Fluid and geochemical transport through oceanic crust: a transect across the eastern flank of the Juan de Fuca Ridge. Earth Planet. Sci. Lett. 172, 151–65.Google Scholar

English, N. B., Quade, J., DeCelles, P. G. and Garzione, C. N. (2000). Geologic control of Sr and major element chemistry in Himalayan rivers, Nepal. Geochim. Cosmochim. Acta 64, 2549–66.Google Scholar

Fairbairn, H. W., Hurley, P. M. and Pinson, W. H. (1961). The relation of discordant Rb–Sr mineral and rock ages in an igneous rock to its time of subsequent Sr⁸⁷/Sr⁸⁶ metamorphism. Geochim. Cosmochim. Acta 23, 135–44.Google Scholar

Farrell, J. W., Clemens, S. C. and Gromet, L. P. (1995). Improved chronostratigraphic reference curve of late Neogene seawater ⁸⁷Sr/⁸⁶Sr. Geology 23, 403–6.Google Scholar

Faure, G., Hurley, P. M. and Powell, J. L. (1965). The isotopic composition of strontium in surface water from the North Atlantic Ocean. Geochim. Cosmochim. Acta 29, 209–20.Google Scholar

Field, D. and Raheim, A. (1979a). Rb–Sr total rock isotope studies on Precambrian charnockitic gneisses from South Norway: evidence for isochron resetting during a low-grade metamorphic-deformational event. Earth Planet. Sci. Lett. 45, 32–44.Google Scholar

Field, D. and Raheim, A. (1979b). A geological meaningless Rb–Sr total rock isochron. Nature 282, 497–9.Google Scholar

Fietzke, J. and Eisenhauer, A. (2006). Determination of temperature-dependent stable strontium isotope (⁸⁸Sr/⁸⁶Sr) fractionation via bracketing standard MC–ICP–MS. Geochem. Geophys. Geosys. 7 (8), 1–6.Google Scholar

Flynn, K. F. and Glendenin, L. E. (1959). Half-life and β spectrum of Rb⁸⁷. Phys. Rev. 116, 744–8.Google Scholar

Gast, P. W. (1955). Abundance of Sr⁸⁷ during geologic time. Bull. Geol. Soc. Amer. 66, 1449–64.Google Scholar

Goldstein, S. J. and Jacobsen, S. B. (1987). The Nd and Sr isotopic systematics of river-water dissolved material: Implications for the sources of Nd and Sr in seawater. Chem. Geol.: Isot. Geosci. Sect. 66, 245–72.Google Scholar

Grant, N. K., Laskowski, T. E. and Foland, K. A. (1984). Rb–Sr and K–Ar ages of Paleozoic glauconites from Ohio–Indiana and Missouri, USA. Isot. Geosci. 2, 217–39.Google Scholar

Gray, C. M., Papanastassiou, D. A. and Wasserburg, G. J. (1973). The identification of early condensates from the solar nebula. Icarus 20, 213–39.Google Scholar

Gussone, N., Eisenhauer, A., Heuser, A. et al. (2003). Model for kinetic effects on calcium isotope fractionation (δ ⁴⁴Ca) in inorganic aragonite and cultured planktonic foraminifera. Geochim. Cosmochim. Acta 67, 1375–82.Google Scholar

Halliday, A. N. and Porcelli, D. (2001). In search of lost planets – the paleocosmochronology of the inner solar system. Earth Planet. Sci. Lett. 192, 545–59.Google Scholar

Harris, W. B. (1976). Rb–Sr glauconite isochron, Maestrichtian unit of Peedee Formation, North Carolina. Geology 4, 761–2.Google Scholar

Harvey, C. F. (2002). Groundwater flow in the Ganges Delta. Science 296, 1563.Google Scholar

Henderson, G. M., Martel, D. J., O'Nions, R. K. and Shackleton, N. J. (1994). Evolution of seawater ⁸⁷Sr/⁸⁶Sr over the last 400 ka: the absence of glacial/interglacial cycles. Earth Planet. Sci. Lett. 128, 643–51.Google Scholar

Hess, J., Bender, M. and Schilling, J. G. (1991). Assessing seawater/basalt exchange of strontium isotopes in hydrothermal processes on the flanks of mid-ocean ridges. Earth Planet. Sci. Lett. 103, 133–42.Google Scholar

Hess, J., Bender, M. L. and Schilling, J. G. (1986). Evolution of the ratio of strontium-87 to strontium-86 in seawater from Cretaceous to present. Science 231, 979–84.CrossRef Google Scholar PubMed

Hodell, D. A., Mead, G. A. and Mueller, P. A. (1990). Variation in the strontium isotopic composition of seawater (8 Ma to present): implications for chemical weathering rates and dissolved fluxes to the oceans. Chem. Geol. (Isot. Geosci. Sect.) 80, 291–307.Google Scholar

Hofmann, A. W. and Giletti, B. J. (1970). Diffusion of geochronologically important nuclides under hydrothermal conditions. Eclogae Geol. Helv. 63, 141–50.Google Scholar

Hunziker, J. C. (1974). Rb–Sr and K–Ar age determination and the Alpine tectonic history of the Western Alps. Mem. Inst. Geol. Min. Univ. Padova 31, 1–54.Google Scholar

Hurley, P. M., Cormier, R. F., Hower, J., Fairbairn, H. W. and Pinson, W. H. (1960). Reliability of glauconite for age measurement by K–Ar and Rb–Sr methods. Amer. Assoc. Pet. Geol. Bull. 44, 1793–808.Google Scholar

Jacobson, A. D. and Blum, J. D. (2000). Ca/Sr and ⁸⁷Sr/⁸⁶Sr geochemistry of disseminated calcite in Himalayan silicate rocks from Nanga Parbat: influence on river-water chemistry. Geology 28, 463–6.Google Scholar

Jager, E. (1973). Die Alpine orogenese im lichte der radiometrischen altersbestimmung. Eclogae Geol. Helv. 66, 11–21.Google Scholar

Jager, E., Niggli, E. and Wenk, E. (1967). Rb)Sr altersbestimmungen an glimmern der Zentralalpen. Beitr. Geol. Karte Schweiz N. F. 134, 1–67.Google Scholar

Jones, M. T., Gislason, S. R., Burton, K. W. et al. (2014). Quantifying the impact of riverine particulate dissolution in seawater on ocean chemistry. Earth Planet. Sci. Lett. 395, 91–100.Google Scholar

Kaufman, A. J., Jacobsen, S. B. and Knoll, A. H. (1993). The Vendian record of Sr and C isotopic variations in seawater: implications for tectonics and paleoclimate. Earth Planet. Sci. Lett. 120, 409–30.Google Scholar

Kossert, K. (2003). Half-life measurements of ⁸⁷Rb by liquid scintillation counting. Applied Rad. Isot. 59, 377–82.Google Scholar

Krabbenhoft, A., Eisenhauer, A., Bohm, F. et al. (2010). Constraining the marine strontium budget with natural strontium isotope fractionations (⁸⁷Sr/⁸⁶Sr*, δ ^88/86Sr) of carbonates, hydrothermal solutions and river waters. Geochim. Cosmochim. Acta 74, 4097–109.Google Scholar

Kubler, B. (1966). La cristallinite d'illite et les zones tout a fait superieures du metamorphisme. Colloque. sur les Etages Tectoniques. Univ. Neuchatel, pp. 105–22.Google Scholar

Lanphere, M. A., Wasserburg, G. J., Albee, A. L. and Tilton, G. R. (1964). Redistribution of strontium and rubidium isotopes during metamorphism, World Beater complex, Panamint Range, California. In: Craig, H., Miller, S. L. and Wasserburg, G. J. (Eds) Isotopic and Cosmic Chemistry. North Holland Pub., pp. 269–320.Google Scholar

Lear, C. H., Elderfield, H. and Wilson, P. A. (2003). A Cenozoic seawater Sr/Ca record from benthic foraminiferal calcite and its application in determining global weathering fluxes. Earth Planet. Sci. Lett. 208, 69–84.Google Scholar

MacLeod, K. G., Huber, B. T. and Fullagar, P. D. (2001). Evidence for a small (∼0.000 030) but resolvable increase in seawater ⁸⁷Sr/⁸⁶Sr ratios across the Cretaceous–Tertiary boundary. Geology 29, 303–6.Google Scholar

Martin, E. E. and Macdougall, J. D. (1991). Seawater Sr isotopes at the Cretaceous/Tertiary boundary. Earth Planet. Sci. Lett. 104, 166–80.Google Scholar

McArthur, J. M., Thirlwall, M. F., Engkilde, M., Zinsmeister, W. J. and Howarth, R. J. (1998). Strontium isotope profiles across K/T boundary sequences in Denmark and Antarctica. Earth Planet. Sci. Lett. 160, 179–92.Google Scholar

McMullen, C. C., Fritze, K. and Tomlinson, R. H. (1966). The half-life of rubidium-87. Can. J. Phys. 44, 3033–8.Google Scholar

Minster, J-F., Birck, J-L. and Allegre, C. J. (1982). Absolute age of formation of chondrites studied by the ⁸⁷Rb–⁸⁷Sr method. Nature 300, 414–19.Google Scholar

Mokadem, F., Parkinson, I. J., Hathorne, E. C. et al. (2015). High-precision radiogenic strontium isotope measurements of the modern and glacial ocean: Limits on glacial–interglacial variations in continental weathering. Earth Planet. Sci. Lett. 415, 111–20.Google Scholar

Morton, J. P. and Long, L. E. (1980). Rb)Sr dating of Palaeozoic glauconite from the Llano region, central Texas. Geochim. Cosmochim. Acta 44, 663–72.Google Scholar

Morton, J. L. and Sleep, N. H. (1985). A mid-ocean ridge thermal model: Constraints on the volume of axial hydrothermal heat flux. J. Geophys. Res. 90 (B13), 11345–53.Google Scholar

Nakai, S., Halliday, A. N., Kesler, S. E. and Jones, H. D. (1990). Rb–Sr dating of sphalerites from Tennessee and the genesis of Mississippi Valley type ore deposits. Nature 346, 354–7.Google Scholar

Nakai, S., Halliday, A. N., Kesler, S. E. et al. (1993). Rb–Sr dating of sphalerites from Mississippi Valley-type (MVT) ore deposits. Geochim. Cosmochim. Acta 57, 417–27.Google Scholar

Nebel, O., Scherer, E. E. and Mezger, K. (2011). Evaluation of the ⁸⁷Rb decay constant by age comparison against the U–Pb system. Earth Planet. Sci. Lett. 301, 1–8.Google Scholar

Neumann, W. and Huster, E. (1974). The half-life of ⁸⁷Rb measured as a difference between the isotopes of ⁸⁷Rb and ⁸⁵Rb. Z. Physik 270, 121–7.Google Scholar

Neumann, W. and Huster, E. (1976). Discussion of the ⁸⁷Rb half-life determined by absolute counting. Earth Planet. Sci. Lett. 33, 277–88.Google Scholar

Nicolaysen, L. O. (1961). Graphic interpretation of discordant age measurements on metamorphic rocks. Ann. N. Y. Acad. Sci. 91, 198–206.Google Scholar

Odin, G. S. and Dodson, M. H. (1982). Zero isotopic age of glauconies. In: Odin, G. S. (Ed.) Numerical Dating in Stratigraphy. Wiley, pp. 277–305.Google Scholar

Odin, G. S., Gale, N. H. and Dore, F. (1985). Radiometric dating of Late Precambrian times. In: Snelling, N. J. (Ed.) The chronology of the geological record. Mem. Geol. Soc. Lond. 10, 65–72.Google Scholar

Palmer, M. R. and Edmond, J. M. (1989). The strontium isotope budget of the modern ocean. Earth Planet. Sci. Lett. 92, 11–26.Google Scholar

Palmer, M. R. and Edmond, J. M. (1992). Controls over the strontium isotope composition of river water. Geochim. Cosmochim. Acta 56, 2099–111.Google Scholar

Papanastassiou, D. A. and Wasserburg, G. J. (1969). Initial strontium isotopic abundances and the resolution of small time differences in the formation of planetary objects. Earth Planet. Sci. Lett. 5, 361–76.Google Scholar

Papanastassiou, D. A., Wasserburg, G. J. and Burnett, D. S. (1970). Rb–Sr ages of lunar rocks from the Sea of Tranquillity. Earth Planet. Sci. Lett. 8, 1–19.Google Scholar

Pearce, C. R., Parkinson, I. J., Gaillardet, J. et al. (2015). Reassessing the stable (δ^88/86Sr) and radiogenic (⁸⁷Sr/⁸⁶Sr) strontium isotopic composition of marine inputs. Geochim. Cosmochim. Acta 157, 125–46.Google Scholar

Peterman, Z. E., Hedge, C. E. and Tourtelot, H. A. (1970). Isotopic composition of strontium in sea water throughout Phanerozoic time. Geochim. Cosmochim. Acta 34, 105–20.Google Scholar

Pettke, T. and Diamond, L. W. (1996). Rb–Sr dating of sphalerite based on fluid inclusion–host mineral isochrons: a clarification of why it works. Econ. Geol. 91, 951–6.Google Scholar

Pierson-Wickmann, A.-C., Reisberg, L. and France-Lanord, C. (2002). Impure marbles of the Lesser Himalaya: another source of continental radiogenic osmium. Earth Planet. Sci. Lett. 204, 203–14.Google Scholar

Popp, B. N., Podosek, F. A., Brannon, J. C., Anderson, T. F. and Pier, J. (1986). ⁸⁷Sr/⁸⁶Sr ratios in Permo-Carboniferous sea water from the analyses of well-preserved brachiopod shells. Geochim. Cosmochim. Acta 50, 1321–8.Google Scholar

Provost, A. (1990). An improved diagram for isochron data. Chem. Geol. (Isot. Geosci. Sect.) 80, 85–99.Google Scholar

Purdy, J. W. and Jager, E. (1976). K)Ar ages on rock-forming minerals from the Central Alps. Mem. Inst. Geol. Mineral. Univ. Padova 30, 3–31.Google Scholar

Rahaman, W. and Singh, S. K. (2012). Sr and ⁸⁷Sr/⁸⁶Sr in estuaries of western India: Impact of submarine groundwater discharge. Geochim. Cosmochim. Acta 85, 275–88.Google Scholar

Rausch, S., Böhm, F., Bach, W., Klügel, A. and Eisenhauer, A. (2013). Calcium carbonate veins in ocean crust record a threefold increase of seawater Mg/Ca in the past 30 million years. Earth Planet. Sci. Lett. 362, 215–24.Google Scholar

Raymo, M. E., Ruddiman, W. F. and Froelich, P. N. (1988). Influence of late Cenozoic mountain building on ocean geochemical cycles. Geology 16, 649–53.Google Scholar

Rotenberg, E., Davis, D. W., Amelin, Y., Ghosh, S. and Bergquist, B. A. (2012). Determination of the decay-constant of ⁸⁷Rb by laboratory accumulation of ⁸⁷Sr. Geochim. Cosmochim. Acta 85, 41–57.Google Scholar

Rundberg, Y. and Smalley, P. C. (1989). High-resolution dating of Cenozoic sediments from northern North Sea using ⁸⁷Sr/⁸⁶Sr stratigraphy. AAPG Bull. 73, 298–308.Google Scholar

Schreiner, G. D. L. (1958). Comparison of the Rb-87/Sr-87 age of the Red granite of the Bushveld complex from measurements on the total rock and separated mineral fractions. Proc. Roy. Soc. Lond. A. 245, 112–17.Google Scholar

Sheppard, T. J. and Darbyshire, D. P. F. (1981). Fluid inclusion Rb–Sr isochrons for dating mineral deposits. Nature 290, 578–9.Google Scholar

Shih, C. Y., Nyquist, L. E., Bogard, D. D. et al. (1985). Chronology and petrogenesis of a 1.8 g lunar granitic clast: 14321, 1062. Geochim. Cosmochim. Acta 49, 411–26.Google Scholar

Spooner, E. T. C. (1976). The strontium isotopic composition of seawater, and seawater–oceanic crust interaction. Earth Planet. Sci. Lett. 31, 167–74.Google Scholar

Steiger, R. H. and Jager, E. (1977). Subcommission on geochronology: convention on the use of decay constants in geo- and cosmo-chronology. Earth Planet. Sci. Lett. 36, 359–62.Google Scholar

Steuber, T. and Veizer, J. (2002). Phanerozoic record of plate tectonic control of seawater chemistry and carbonate sedimentation. Geology 30, 1123–6.Google Scholar

Stoll, H. M. and Schrag, D. P. (1998). Effects of Quaternary sea level cycles on strontium in seawater. Geochim. Cosmochim. Acta 62, 1107–18.Google Scholar

Sun, S. S. and Hansen, G. N. (1975). Evolution of the mantle: geochemical evidence from alkali basalt. Geology 3, 297–302.Google Scholar

Tatsumoto, M. (1966). Genetic relationships of oceanic basalts as indicated by lead isotopes. Science 153, 1094–101.Google Scholar

Tilton, G. R. (1988). Age of the solar system. In: Kerridge, J. F. and Matthews, M. S. (Eds) Meteorites and the Early Solar System, Univ. Arizona Press, pp. 259–75.Google Scholar

Tretbar, D. R., Arehart, G. B. and Christensen, J. N. (2000). Dating gold deposition in a Carlin-type gold deposit using Rb/Sr methods on the mineral galkhaite. Geology 28, 947–50.Google Scholar

Vance, D., Teagle, D. A. and Foster, G. L. (2009). Variable Quaternary chemical weathering fluxes and imbalances in marine geochemical budgets. Nature 458, 493–6.Google Scholar

Veizer, J. and Compston, W. (1974). ⁸⁷Sr/⁸⁶Sr composition of seawater during the Phanerozoic. Geochim. Cosmochim. Acta 38, 1461–84.Google Scholar

Veizer, J. and Compston, W. (1976). ⁸⁷Sr/⁸⁶Sr in Precambrian carbonates as an index of crustal evolution. Geochim. Cosmochim. Acta 40, 905–14.Google Scholar

Veizer, J. and 14 others. (1999). ⁸⁷Sr/⁸⁶Sr, δ¹³C and δ¹⁸O evolution of Phanerozoic seawater. Chem. Geol. 161, 59–88.Google Scholar

Verschure, R. H. Andriessen, P. A. M., Boelrijk, N. A. I. M. et al. (1980). On the thermal stability of Rb–Sr and K–Ar biotite systems: evidence from co-existing Sveconorwegian (ca. 870 Ma) and Caledonian (ca. 400 Ma) biotites in S.W. Norway. Contrib. Mineral. Petrol. 74, 245–52.Google Scholar

Villa, I. M., De Bièvre, P., Holden, N. E. and Renne, P. R. (2015). IUPAC–IUGS recommendation on the half life of ⁸⁷Rb. Geochim. Cosmochim. Acta 164, 382–5.Google Scholar

Wasserburg, G. J., Papanastassiou, D. A. and Sanz, H. G. (1969). Initial strontium for a chondrite and the determination of a metamorphism or formation interval. Earth Planet. Sci. Lett. 7, 33–43.Google Scholar

Wetherill, G. W., Davis, G. L. and Lee-Hu, C. (1968). Rb–Sr measurements on whole rocks and separated minerals from the Baltimore Gneiss, Maryland. Geol. Soc. Amer. Bull. 79, 757–62.Google Scholar

Wickman, F. E. (1948). Isotope ratios: a clue to the age of certain marine sediments. J. Geol. 56, 61–6.Google Scholar

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Chapter 3 - The Rb–Sr Method

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