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- Kosminska, Karolina, et al.
(författare)
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Monazite in the eclogite and blueschist of the Svalbard Caledonides : its origin and forming-reactions
- 2023
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Ingår i: Contributions to Mineralogy and Petrology. - : Springer. - 0010-7999 .- 1432-0967. ; 178
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Tidskriftsartikel (refereegranskat)abstract
- 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.
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| 2. |
- Szilas, Kristoffer, et al.
(författare)
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Archaean andesite petrogenesis : insights from the Grædefjord Supracrustal Belt, southern West Greenland
- 2013
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Ingår i: Precambrian Research. - : Elsevier BV. - 0301-9268. ; 236, s. 1-15
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Tidskriftsartikel (refereegranskat)abstract
- We present new whole-rock major, trace and platinum-group element data, as well as Sm–Nd and Lu–Hfisotope data for meta-volcanic rocks from the Mesoarchaean Grædefjord Supracrustal Belt (GSB), locatedwithin the Tasiusarsuaq terrane, southern West Greenland. We also present new in situ zircon U–Pbisotope data (by LA-ICP-MS) for associated felsic rocks. This region has experienced amphibolite to lowergranulite facies metamorphism, causing re-equilibration of most mineral phases (including zircon).An intrusive tonalite sheet with a zircon U–Pb age of 2888 ±6.8 Ma, yields a minimum age for the GSB.The Sm–Nd and Lu–Hf isotope data do not provide meaningful isochron ages, but the isotope compositionsof the mafic rocks are consistent with the ca. 2970 Ma regional volcanic event, which is documented in pre-vious studies of the Tasiusarsuaq terrane. The major and trace element data suggest a significant crustalcontribution in the petrogenesis of andesitic volcanic rocks in the GSB. The trace element variation of theseandesitic leucoamphibolites cannot be explained by bulk assimilation–fractional-crystallisation (AFC)processes involving local basement. Rather, the observed patterns require binary mixing between basalticand felsic end-member magmas with between 50% and 80% contributions from the latter (depending onthe assumed felsic composition). Hf-isotope constraints point to contamination with pre-existing conti-nental crust with an age of ca. 3250 Ma. Basement gneisses of this age were previously described at twolocalities in the Tasiusarsuaq terrane, which supports the mixing hypothesis. Thus the felsic end-memberlikely represents melts derived from the local basement.Ultramafic rocks (18.35–22.80 wt.% MgO) in GSB have platinum-group element (PGE) patterns that aresimilar to magmas derived from high-degree melting of mantle, but they have relatively enriched traceelement patterns. We propose that the ultramafic rocks represent arc-related picrites or alternativelywere derived by melting of metasomatised sub-continental lithospheric mantle.Overall these new geochemical data from the Mesoarchaean Grædefjord Supracrustal Belt and thepetrogenetic mixing model in particular, are similar to observations from modern continental subductionzone environments, which also require large degrees of mixing with felsic basement melts. Therefore,we propose that the metavolcanic rocks formed in a modern-style subduction zone geodynamic setting,which due to the hotter Archaean mantle conditions allowed for substantial amounts of partial meltingand magma mixing, rather than assimilating pre-existing continental crust.
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