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, Buckley HR, Spriggs M, Bedford S, Ottley CJ, Nowell GM et al. 2007. Lapita migrants in the Pacific’s oldest cemetery: isotopic analysis at Teouma, Vanuatu. Am Atiq 645–56. Bentley RA, Krause R, Price TD, Kaufmann B. 2003. Human Mobility at the early Neolithic settlement of Vaihingen, Germany: evidence from strontium isotope analysis. Archaeometry 45(3):471–86. Bentley RA, Price TD, Stephan E. 2004. Determining the ‘local’ 87 Sr/ 86 Sr range for archaeological skeletons: a case study from Neolithic Europe. J Archaeol Sci 31(4):365–75. Bentley RA., 2006. Strontium

. In: S. Czopek (Ed.) Autostradą w przeszłość. Katalog wystawy. Motorway to the past. Exhibition catalogue, 133-295. Rzeszów. Marks L, Ber A, Gogołek W, Piotrowska K. 2006 Geological Map of Poland 1: 500 000. Warszawa. Maurer A.F., Galer S.J., Knipper C., Beierlein L., Nunn E.V., Peters D., Tutken T., Alt K.W., Schone B.R. 2012 Bioavailable 87 Sr/ 86 Sr in different environmental samples – effects of anthropogenic contamination and implications for isoscapes in past migration studies. Science of the Total Environment 433: 216-229. Montgomery J. 2010 Passports

. During the period of investigation a 143 Nd/ 144 Nd ratio of 0.511850 ± 0.000005 (n = 5) and a 87 Sr/ 86 Sr ratio of 0.710274 ± 0.000008 (n = 5) were determined for the La Jolla (Nd) and the NBS987 (Sr) international standards, respectively. Details of techniques, accuracy and data precision of Rb-Sr and Sm-Nd isotopic measurements are given by Thöni et al. (2008) . Zircon separation, CL imaging and U-Th-Pb MC-ICP-MS dating Zircon crystals were separated using standard techniques (crushing, hydrofracturing, washing, Wilfley table, magnetic separator and handpicking

side filament in a triple filament arrangement. Both Sr and Nd isotopic ratios were determined by a multicollector Thermal Ionization Mass Spectrometer (TIMS) VG Sector 54. Data were acquired in dynamic mode with peak measurements at 1–2 V for 88 Sr and 0.5–1.0 V for 144 Nd. Typical runs consisted of acquisition of 60 isotopic ratios. Strontium and neodymium isotopic ratios were corrected for mass fractionation relative to 88 Sr/ 86 Sr = 0.1194 and 146 Nd/ 144 Nd = 0.7219. During this study, the SRM-987 standard gave an average value of 87 Sr/ 86 Sr = 0

-Nielsen (Eds): Plankton stratigraphy. Cambridge University Press, Cambridge, 155-262. Bueno, G.V., Zacharias, A.A., Oeiro, S.G., Cupertino, J.A., Falkenhein, F.U.H. & Martins Neto, M.A., 2007. Bacia de Pelotas. [Pelotas Basin]. Boletim de Geociências da Petrobras 15, 551-559. Burke, W.H., Denison, R.E., Hetherington, E.A., Koepnick, R.B., Nelson, H.F. & Otto, J.B., 1982. Variation of seawater 87Sr/86Sr through Phanerozoic time. Geology 10, 516-519. Cainelli, C. & Mohriak, W.U., 1999. Some remarks on the evolution of sedimentary basins along the eastern Brazilian continental

Ree and Sr-Nd Isotope Compositions of Clinopyroxenites, Phoscorites and Carbonatites of the Seblyavr Massif, Kola Peninsula, Russia

Clinopyroxenites, phoscorites and carbonatites from the Devonian Seblyavr intrusion (Kola Peninsula, Russia) have petrographic characteristics indicating that they are accumulative in origin. Their geochemical (major and rare earth elements) compositions can be accounted for by mixtures of their major rock-forming minerals and accessory phases, i.e. they reflect the record of mineral accumulation. All of the analysed Seblyavr rocks are strongly LREE-enriched with (La/Yb)N mostly ranging from 38 to 189. However, a dolomite carbonatite with hydrothermal LREE-Sr mineralization has an extreme (La/Yb)N value of 1659. Such late-stage dolomite carbonatites were formed by hydrothermal (rather than magmatic) processes. Whole-rock samples of representative magmatic lithologies from Seblyavr have initial 87Sr/86Sr and εNd that fall in a very narrow range from 0.7031 to 0.7033 and +4.9 to +5.9, respectively. We therefore conclude that clinopyroxenites, phoscorites and carbonatites were formed by differentiation and crystallization of a single batch of melt. The parental melt was derived from a depleted upper mantle source that had been meta-somatised prior to melting.

-Karkonosze Block (Sudetes, Poland). Terra Nostra 8: 122. Pin C, Mierzejewski MP and Duthou JL, 1987. Wiek izochronowy Rb/Sr granitu karkonoskiego z kamieniołomu Szklarska Poręba Huta oraz oznaczenie stosunku inicjalnego 87 Sr/ 86 Sr w tymże granicie. (Rb-Sr isochron age of the Karkonosze granite from the quarry Szklarska Poręba Huta and determination of its 87 Sr/ 86 Sr initial ratio). Przegląd Geologiczny 35: 512-517 (in Polish). Przewłocki K, Magda W, Thomas HH and Faul H, 1962. Ages of some granitic rocks in Poland. Geochimica et Cosmochimica Acta 26: 1069

deposit. Kwartalnik Geologiczny, 21, 27-35. Pin, C., Mierzejewski, M.P., & Duthou, J.L. (1987). Wiek izochronowy Rb/Sr granitu karkonoskiego z kamieniołomu Szklarska Poręba oraz oznaczenie stosunku inicjalnego 87Sr/86Sr w tymże granicie / Isochronous age Rb/Sr of Karkonosze granite from the quarry Szklarska Poręba Huta and significance of initial 87Sr/86Sr in this granite. Przegląd Geologiczny, 35, 512-517. Robb, L. (2005). Introduction to ore-forming processes , Oxford: Blackwell Publishing. Sharman, E.R., Wing, B.A., Minarik, W.G., Taylor, B.E., & Dube, B. (2010

geologischen Gesellschaft, 24, 191-206. Pieczka, A., Pieczonka, J., & Piestrzyński, A. (1988). Minerals of the weathering zone of Miedzianka polymetallic deposit, Rudawy Janowickie (Lower Silesia, Poland). Mineralogia Polonica, 19 , 75-98. Pin, C., Mierzejewski, M.P., & Duthou, J.L. (1987). Wiek izochronowy Rb/Sr granitu karkonoskiego z kamieniołomu Szklarska Poręba Huta oraz oznaczenie stosunku inicjalnego 87Sr/86Sr w tymże granicie. [Isochronous age Rb/Sr of Karkonosze granite from the quarry Szklarska Poręba Huta and significance of initial 87Sr/86Sr in this granite

Mineralogiczne - Prace Specjalne (Mineralogial Society of Poland - Special Papers) 25, 167-171. PIESTRZYŃSKI, A., 2005: Rudy miedzi i srebra. (Copper and silver ores). In: Fabiszewski J. (ed.) - Przyroda Dolnego Śląska. Polska Akademia Nauk, Wrocław, 229-241 (in Polish). PIN, C., MIERZEJEWSKI, M. P., DUTHOU, J. L., 1987: Isochronous age Rb/Sr of Karkonosze granite from the quarry Szklarska Poręba Huta and significance of initial 87 Sr/ 86 Sr in this granite. Przegląd Geologiczny 10, 512-517 (in Polish with English abstract). RAMDOHR, P., 1969: The ore minerals and their