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2021 | 12 | 85-91

Article title

Datowanie metamorfizmu z początku Układu Słonecznego: wiek U-Pb apatytu z meteorytu Leoncin (chondryt zwyczajny LL5-6 o charakterze brekcji monomiktycznej)

Content

Title variants

EN
U-Pb age of the early Solar System metamorphism by using apatite from the Leoncin meteorite (LL5-6 ordinary chondrites – monomictic breccia)

Languages of publication

PL

Abstracts

EN
The U-Pb system is a useful chronometer for understanding the formation history of chondritic materials. Modern studies showed that the formation ages of chondrites (4.55–4.56 Ga) effectively equal the formation age of the solar system. Recently, researchers have undertaken U-Pb isotopic studies of phosphates separated from equilibrated ordinary chondrites, which are the major hosts for U and are enriched by an order of magnitude or more relative to the bulk rock (typical U concentrations of 0.1–3 ppm in phosphates). The observed Pb-Pb model ages for these phosphates range from 4.563–4.502 Ga, with an analytical precision of 1 Ma and the U-Pb system is apparently concordant. They also argued that the Pb-Pb ages of the phosphates from several H chondrites show a negative correlation with metamorphic grade. They concluded that thermal processing of the equilibrated chondrites took place over a 60 Ma interval and grain size of the phosphates increases with the degree of metamorphism. In the Leoncin meteorite, apatite reveal the 207Pb/206Pb age, which is 4549±61 Ma. The obtained apatite age in the Leoncin meteorite reflects the early solar system formation process. Moreover, the age is an example of the early solar system metamorphism, which confirms a slightly younger event of secondary changes of the parent body for this meteorite. It is also the first isotopic age of a Polish meteorite.

Keywords

Year

Volume

12

Pages

85-91

Physical description

Dates

published
2021

Contributors

  • Instytut Nauk o Ziemi, Wydział Nauk Przyrodniczych, Uniwersytet Śląski w Katowicach
  • Instytut Nauk o Ziemi, Wydział Nauk Przyrodniczych, Uniwersytet Śląski w Katowicach

References

  • Chamberlain K.R., Bowring A.B., 2000, Apatite–feldspar U–Pb thermochronometer: a reliable, mid-range (~450C), diffusion-controlled system, Chemical Geology, 172, s. 173–200.
  • Dahl P.S., 1997, A crystal-chemical basis for Pb retention and fission-track annealing systematics in U-bearing minerals, with implications for geochronology, Earth and Planetary Scientific Letters, 150(3–4), s. 277–290.
  • Karwowski Ł., Szopa K., 2020, Leoncin – nowy polski chondryt LL4-6, Acta Societatis Metheoriticae Polonorum, 11, s. 31–44.
  • Krogstad E.J., Walker R.J., 1994, High closure temperatures of the U–Pb system in large apatites from the Tin Mountain Pegmatite, Black Hills, South Dakota, USA, Geochimica et Cosmochimica Acta, 58(18), s. 3845–3853.
  • Schoene B., Bowring S.A., 2006, U-Pb systematics of the McClure Mountain syenite: thermochronological constraints on the age of the Ar-40/Ar-39 standard MMhb, Contributions to Mineralogy and Petrology, 151(5), s. 615–630.
  • Terada K., Sano Y., 2012, In-situ U-Pb dating of apatite by Hiroshima-SHRIMP, Contributions to Earth and Planetary Science. Mass Spectrometry, 1, p. A0011.
  • Watson E.B., Harrison T.M., Ryerson F.J., 1985, Diffusion of Sm, Sr, and Pb in fluorapatite, Geochimica et Cosmochimica Acta, 49(8), s. 1813–1823.
  • Zhang A.C., Li Q.L., Yurimoto H., Sakamoto N., Li X.H., Hu S., Lin Y.-T., Wang R.-C., 2016, Young asteroidal fluid activity revealed by absolute age from apatite in carbonaceous chondrite, Nature Communication, 7, 12844.

Document Type

article

Publication order reference

Identifiers

YADDA identifier

bwmeta1.element.ojs-issn-2080-5497-year-2021-issue-12-article-8abd989d-2f1a-31a8-adbf-9b1bafe3f8fe
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