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Sökning: id:"swepub:oai:DiVA.org:uu-510779" > Monazite in the ecl...

Monazite in the eclogite and blueschist of the Svalbard Caledonides : its origin and forming-reactions

Kosminska, Karolina (författare)
AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Krakow, Poland.
Fassmer, Kathrin (författare)
Univ Innsbruck, Inst Geol, Innsbruck, Austria.
McClelland, William C. (författare)
Univ Iowa, Dept Earth & Environm Sci, Iowa City, IA USA.
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Majka, Jaroslaw (författare)
Uppsala universitet,Mineralogi, petrologi och tektonik,AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Krakow, Poland.
Coble, Matthew (författare)
GNS Sci, Surface Geosci Dept, Lower Hutt, New Zealand.
Thomas, Jay (författare)
Syracuse Univ, Dept Earth & Environm Sci, Syracuse, NY USA.
Manecki, Maciej (författare)
AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Krakow, Poland.
Lorenz, Henning, Dr. 1972- (författare)
Uppsala universitet,Geofysik
Bazarnik, Jakub (författare)
Polish Geol Inst, Natl Res Inst, Carpathian Branch, Krakow, Poland.
Münker, Carsten (författare)
Univ Cologne, Inst Geol & Mineral, Cologne, Germany.
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AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Krakow, Poland Univ Innsbruck, Inst Geol, Innsbruck, Austria. (creator_code:org_t)
Springer, 2023
2023
Engelska.
Ingår i: Contributions to Mineralogy and Petrology. - : Springer. - 0010-7999 .- 1432-0967. ; 178
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • High-pressure low-temperature rocks from Svalbard are an excellent target for studying metamorphic reactions in Phanerozoic subduction zones. This study reveals the presence of monazite in an eclogite and a blueschist from the Vestgotabreen Complex, southwestern Svalbard. In order to investigate the monazite-forming reaction, we obtained pressure-temperature estimates coupled with U-Pb and Lu-Hf dating. Combined geothermobarometry allows to constrain three evolutionary stages of garnet growth in the eclogite: nucleation (1.6 & PLUSMN; 0.3 GPa at 460 & PLUSMN; 60 & DEG;C), peak-pressure (2.3 & PLUSMN; 0.3 GPa at 507 & PLUSMN; 60 & DEG;C), and peak-temperature (2.1 & PLUSMN; 0.3 GPa at 553 & PLUSMN; 60 & DEG;C). A zircon age of 482 & PLUSMN; 10 Ma is interpreted to belong to the prograde part of the pressure-temperature path. Monazite forms inclusions within garnet rims, or it is surrounded by allanite and apatite, altogether forming pseudomorphs of a tabular shape in the matrix. Textures, geothermobarometry and geochronology support the conclusion the monazite formed under high-pressure conditions at 471 & PLUSMN; 6 Ma. We propose that the monazite crystallization in the eclogite happened due to a decomposition of accessory phases during the decompression after peak-pressure of the metamorphic cycle. Monazite in the blueschist occurs as inclusions in garnet cores and gives an indicative age of 486 & PLUSMN; 6 Ma, which is interpreted to reflect the prograde growth of the garnet. Lu-Hf garnet dating resolves an age of peak-pressure metamorphism in the blueschist at 471.1 & PLUSMN; 4 Ma under conditions of 2.0 & PLUSMN; 0.03 GPa and 500 & PLUSMN; 30 & DEG;C. The Vestgotabreen Complex provides evidence for an early Ordovician modern-style subduction system in the proximity of the Baltica margin. Hence, this study also supports the tectonic models that favour a mixed Baltican and Laurentian provenance of south-western Svalbard.

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

Eclogite
Blueschist
Monazite
High-pressure low-temperature metamorphism
Vestgotabreen Complex
Svalbard

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