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5 items
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Constraints on the sources of post-collisional K-rich magmatism: The roles of continental clastic sediments and terrigenous blueschists
Wang Yu, Prelević Dejan, Buhre Stephan, Foley Stephen. "Constraints on the sources of post-collisional K-rich magmatism: The roles of continental clastic sediments and terrigenous blueschists" in Chemical Geology, :Elsevier BV (2016). https://doi.org/DOI:10.1016/j.chemgeo.2016.10. M21
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Experimental production of K-rich metasomes through sediment recycling at the slab-mantle interface in the fore-arc
Sediment contribution to the mantle is the key step for the generation of orogenic magmatism to produce its isotopic and geochemical inventory. Even though they are exceptional for the post-collisional settings, there are worldwide examples of arc-related ultrapotassic mafic magmas which require complex multi-stage processes along with sediment melting e.g. in Italy or Pontides of Türkiye. To understand the metasomatism leading mantle to produce ultrapotassic mafic melts, we simulated the reactions of depleted (harzburgite) and fertile (lherzolite) mantle with ...Fatma Gülmez, Dejan Prelević, Michael W. Förster, Stephan Buhre, Jennifer Günther . "Experimental production of K-rich metasomes through sediment recycling at the slab-mantle interface in the fore-arc" in Scientific Reports (2023) М21
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Variation of olivine composition in the volcanic rocks in the Songliao basin, NE China: lithosphere control on the origin of the K-rich intraplate mafic lavas
Zhang, L.-Y., Prelević Dejan, Li, N., Mertz-Kraus, R., Buhre, S.. "Variation of olivine composition in the volcanic rocks in the Songliao basin, NE China: lithosphere control on the origin of the K-rich intraplate mafic lavas" in Lithos 262 (2016): 153-168. https://doi.org/https://doi.org/10.1016/j.lith M21
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Recent advances made by reaction experiments on melting of heavily metasomatized hydrous mantle
Dejan Prelević, Michael W. Förster, Stephan Buhre, Fatma Gülmez, Tobias Grützner, Yu Wang, Stephen F. Foley (2024)Mantle-derived magmas are traditionally assumed to originate by melting of an upper mantle consisting of uniform spinel- or garnet peridotite dominated by olivine. However, extensive studies of mantle-derived basalts suggest that the mantle is more mineralogically heterogeneous, so that the genesis of even the most common magmas requires consideration of mixed source regions within the mantle involving pyroxenites and hydrous minerals. We refer to these with the group term metasomes. However, most experimental studies on mantle melting have assumed ...Dejan Prelević, Michael W. Förster, Stephan Buhre, Fatma Gülmez, Tobias Grützner, Yu Wang, Stephen F. Foley. "Recent advances made by reaction experiments on melting of heavily metasomatized hydrous mantle" in Earth-Science Reviews (2024) М21а
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Melting and dynamic metasomatism of mixed harzburgite + glimmerite mantle source: implications for the genesis of orogenic potassic magmas
Förster Michael, Prelević Dejan, Schmück Harald, Buhre Stephan, Veter Marina, Mertz-Kraus Regina, Foley Stephen, Jacob Dorrit (2016)Förster Michael, Prelević Dejan, Schmück Harald, Buhre Stephan, Veter Marina, Mertz-Kraus Regina, Foley Stephen, Jacob Dorrit. "Melting and dynamic metasomatism of mixed harzburgite + glimmerite mantle source: implications for the genesis of orogenic potassic magmas" in Chemical Geology, :Elsevier BV (2016). https://doi.org/10.1016/j.chemgeo.2016.08.037 M21