PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Datowanie cyrkonów z anortozytów : misja niemożliwa?

Treść / Zawartość
Identyfikatory
Warianty tytułu
EN
Dating zircons from anorthosites : mission impossible?
Języki publikacji
PL
Abstrakty
EN
Despite the low content of Zr element (<100 ppm) in the anorthosites from the Suwałki Massif and Sejny Intrusion, it was necessary to undertake U-Pb age investigation on zircons. It was a technical challenge, which required a modification of typical separation procedures. In anorthosites associated with Fe-Ti ores, zircon is rich in Fe-Ti oxide inclusions and it often ends up in the magnetic fraction. The drillcore samples were selected from four different drillings located in the Suwałki Massif and nearby Sejny Intrusion, where a dominant rock type is anorthosites. In these rocks, zircon crystallizes as a late phase, which is reflected by its interstitial morphology. The samples were collected from depth intervals spanning multiple sections of the core, therefore a large number of U-Pb SHRIMP measurements (n = 50-97) has been performed for each sample. Age results, presented as a weighted average (Mean age), range from ~1510Ma (Jezioro Szlinokiemskie IG 1) to ~1505 Ma (Sejny IG 2). The SHRIMP data provided evidence of a distinct magma composi¬tion reflected by diversity of zircon chemical composition. The later evolution of Fe-Ti oxides is recorded as zircon lamellae being an effect of the subsolidus Zr precipitation from the ilmenite network at 1482 Ma.
Rocznik
Strony
723--729
Opis fizyczny
Bibliogr. 27 poz., fot., rys., tab., wykr.
Twórcy
  • Uniwersytet Warszawski, Wydział Geologii, ul. Żwirki i Wigury 93, 02-089 Warszawa
  • Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy, ul. Rakowiecka 4, 00-975 Warszawa
  • Emerytowany pracownik Państwowego Instytutu Geologicznego - Państwowego Instytutu Badawczego
  • Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy, ul. Rakowiecka 4, 00-975 Warszawa
Bibliografia
  • 1. BELOUSOVA E.A., GRIFFIN W.L., O’REILLY S.Y., FISHER N.1.2002 - Igneous zircon: Trace element composition as an indicator of source rock type. Contrib. Mineral. Petrol., l43: 602-622.
  • 2. BORG L.E., CONNELLY J.N., BOYET M., CARLSON R.W. 2011 - The Age of Lunar Ferroan Anorthosite 60025 with Implications for the Interpretation of Lunar Chronology and the Magma Ocean Model. 42nd unar and Planetary Science; https://www.lpi.usra.edu/meetings/lpsc2011/pdf/1171.pdf
  • 3. CHARLIER B., NAMUR O., DUCHESNE J.C., WISZNIEWSKA J., PARECKI A., VANDER AUWERA J. 2009 - Cumulate Origin and Polybaric Crystallization of Fe-Ti Oxide Ores in the Suwalki Anorthosite, Northeastern Poland. Econ. Geol., 104: 205-221.
  • 4. CHERNIAK D.J., HANCHAR J.M., WATSON E.B. 1997 - Diffusion of tetravalent cations in zircon. Contrib. Mineral. Petrol., 127: 383-390.
  • 5. COMPSTON W., WILLIAMS I.S., MEYERC. 1984 -U-Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass-resolution ion microprobe. J. Geophys. Res. SolidEarth, 89: B525-B534.
  • 6. DE CARVALHO H., ALVES P.H. 1990 - Gabbro-Anorthosite Complex of SW Angola/NW Namibia. Comunicações Instituto Investigação Científica Tropical, 2: 5-64.
  • 7. DÖRR W., BELKA Z., MARHEINE D., SCHASTOK J., VALVERDE-VAQUERO P., WISZNIEWSKA J. 2002 - U-Pb and Ar-Ar geochronology of anorogenic granite magmatism of the Mazury Complex, NE Poland. Precam. Res., 119: 101-120.
  • 8. FROST C.D.M., MEIER F., OBERLI F. 1990 - Single-crystal U-Pb zircon age determination of the Red Mountain pluton, Laramie Anorthosite Complex, Wyoming. Am. Min., 75: 21-26.
  • 9. HOSKIN P.W.O., SCHALTEGGERU. 2003 - The composition of zircon and igneous and metamorphic petrogenesis. Rev. Mineral. Geochem., 53: 27-62.
  • 10. KIRKLAND C.L., SMITHIES R.H., TAYLOR R.J.M., EVANS N., MCDONALD B. 2015 - Zircon Th/U ratios in magmatic environs. Lithos, 212: 397-414.
  • 11. LEE Y., CHO M., CHEONG W., YI K. 2014. Amassif-type (~1.86 Ga) anorthosite complex in the Yeongnam Massif, Korea: late-orogenic emplacement associated with the mantle delamination in the North China Craton. Terra Nova, 26: 408-416.
  • 12. LUDWIK H.R. 2003 - User’s manual Isoplot/Ex version 3.00, a geochronological toolkit for Microsoft Exel. Berkeley Geochrology Center Special Publications, 4: 72.
  • 13. McKAY M.P., JACKSON W.T., HESSLER A.M. 2018 - Tectonic stress regime recorded by zircon Th/U. Gondwana Res., 57: 1-9.
  • 14. MEIS C., GALE J.D. 1998 - Computational study of tetravalent uranium and plutonium lattice diffusion in zircon. Mater. Sci. Eng., B, 57: 52-61.
  • 15. MORGAN J., STEIN H., HANNAH J. MARKEY R.J., WISZNIEWSKA J. 2000 - Re-Os study of Fe-Ti-V oxide and Fe-Cu-Ni sulfide deposits, Suwałki Anorthosite Massif, northeast Poland. Mineral. Depos., 35: 391-401.
  • 16. MORISSET C.E., SCOATES J.S. 2008 - Origin of zircon rims around ilmenite in mafic plutonic rocks of Proterozoic anorthosite suites. Canad.Mineral., 46: 289-304.
  • 17. OWENS B.E., DYMEK R.F. 2001 - Petrogenesis of the Labrieville alkalic anorthosite massif, Grenville Province, Quebec. J. Petrol., 42: 1519-1546.
  • 18. PETECKI Z., WISZNIEWSKA J. 2021 - Internal structure of the buried Suwałki Anorthosite Massif (East European Craton, NE Poland) based on borehole, magnetic and gravity data combined with new petrological results. Geol. Quart., 65: 1-17.
  • 19. ROSENBLUM S., BROWNFILED I.K. 2000 - Magnetic susceptibilities of minerals. U.S. Geol. Surv., 99-529: 1-37.
  • 20. RUBATTO D. 2002 - Zircon trace element geochemistry: partitioning with garnet and the link between U-Pb ages and metamorphism. Chem. Geol., 184: 123-138.
  • 21. RUSZKOWSKI M., WISZNIEWSKA J. 2018 - Wstępne rozpoznanie obwódek cyrkonowo-hafnowych wokół minerałów kruszcowych w złożach Fe-Ti-V w suwalskim masywie anortozytowym (północno-wschodnia Polska). Prz. Geol., 66: 107-110.
  • 22. SATO M., YAMAMOTO S., YAMAMOTO Y., OKADA Y., OHNO M., TSUNAKAWA H., MARUYAMA S. 2015 - Rock-magnetic properties of single zircon crystals sampled from the Tanzawa tonalitic pluton, central Japan. EPS, 67: 1-14.
  • 23. SCHÄRER U., WILMART E, DUCHESNE J.C. 1996 - The short duration and anorogenic character of anorthosite magmatism: U-Pb dating of the Rogaland complex, Norway. Earth Planet. Sci. Lett., 139: 335-350.
  • 24. SCOATES J.S., CHAMBERLAIN K.R. 1995 - Baddeleyite (ZrO2) and zircon (ZrSiO4) from anorthositic rocks of the Laramie anorthosite complex, Wyoming: Petrologic consequences and U-Pb ages. Am. Mineral., 80: 1317-1327.
  • 25. WALLC.J., SCOATES J.S., WEIS D. 2016 - Zircon from the Anorthosite zone II of the Stillwater Complex as a U-Pb geochronological referen¬ce material for Archean rocks. Chem. Geol., 436: 54-71.
  • 26. WISZNIEWSKA J., CLAESSON S., STEIN H., AUWERA J.V., DUCHESNE J.C. 2002 - The north-eastern Polish anorthosite massifs: petrological, geochemical and isotopic evidence for a crustal derivation. Terra Nova, 14: 451-460.
  • 27. WISZNIEWSKA J., KRZEMIŃSKA E. 2021 - Advances in geochronology in the Suwałki anorthosite massif and subsequent granite veins, northeastern Poland. Precam. Res., 361: 106265.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2025).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c9920eb5-a972-41b2-b034-512275b9891a
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.