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Sökning: id:"swepub:oai:DiVA.org:uu-414315" > U-Pb Zircon Dating ...

U-Pb Zircon Dating of Migmatitic Paragneisses and Garnet Amphibolite from the High Pressure Seve Nappe Complex in Kittelfjäll, Swedish Caledonides

Bukala, Michal (författare)
AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, PL-30059 Krakow, Poland.;CSIC, Inst Andaluz Ciencias Tierra, Granada 18100, Spain.;Univ Granada, Granada 18100, Spain.
Majka, Jaroslaw (författare)
Uppsala universitet,Mineralogi, petrologi och tektonik,AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, PL-30059 Krakow, Poland
Walczak, Katarzyna (författare)
AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, PL-30059 Krakow, Poland.
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Wlodek, Adam (författare)
AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, PL-30059 Krakow, Poland.
Schmitt, Melanie (författare)
Swedish Museum Nat Hist, Dept Geosci, S-10405 Stockholm, Sweden.
Zagorska, Anna (författare)
Polish Acad Sci, Krakow Res Ctr, Inst Geol Sci, PL-31002 Krakow, Poland.
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AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, PL-30059 Krakow, Poland;CSIC, Inst Andaluz Ciencias Tierra, Granada 18100, Spain.;Univ Granada, Granada 18100, Spain. Mineralogi, petrologi och tektonik (creator_code:org_t)
2020-03-25
2020
Engelska.
Ingår i: Minerals. - : MDPI AG. - 2075-163X. ; 10:4
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Seve Nappe Complex exposed in the Kittelfjall area of the northern Scandinavian Caledonides comprises a volcano-sedimentary succession representing the Baltica passive margin, which was metamorphosed during the Iapetus Ocean closure. Garnet amphibolites, together with their host migmatitic paragneisses, record a potential (U)HP event followed by decompression-driven migmatization. The garnet amphibolites were originally thought to represent retrogressively altered granulites. The petrological and geochemical features of a studied garnet amphibolite allow for speculation about a peridotitic origin. Zirconium (Zr) content in rutile inclusions hosted in garnet in paragneisses points to near-peak temperatures between 738 degrees C and 780 degrees C, which is in agreement with the c. 774 degrees C obtained from the matrix rutile in the garnet amphibolite. The matrix rutile in multiple paragneiss samples records temperatures below 655 degrees C and 726 degrees C. Whereas the LA-ICP-MS U-Pb dating of zircon cores revealed the age spectrum from Paleoproterozoic to early Paleozoic, suggesting a detrital origin of zircon cores in paragneisses, the metamorphic zircon rims show an Early Ordovician cluster c. 475-469 Ma. Additionally, zircon cores and rims from the garnet amphibolite yielded an age of c. 473 Ma. The REE patterns of the Caledonian zircon rims from the paragneisses show overall low LREE concentrations, different from declining to rising trends in HREE (Lu-N/Gd-N = 0.49-38.76). Despite the textural differences, the cores and rims in zircon from the garnet amphibolite show similar REE patterns of low LREE and flat to rising HREE (Lu-N/Gd-N = 3.96-65.13). All zircon rims in both lithologies display a negative Eu anomaly. Hence, we interpret the reported ages as the growth of metamorphic zircon during migmatization, under granulite facies conditions related to exhumation from (U)HP conditions.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Nyckelord

geochronology
subduction
metamorphism
migmatite
decompression

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