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) according to Mika et al. ( 2010 ) Several examples can be found in the literature for the application of the Mann–Kendall trend test, for example, Patle and Libang ( 2014 ) argued on trend analysis of annual and seasonal

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in cores from boreholes or rock samples from outcrops, or estimated from literature or using the results of thermal response tests. Heat-flow density varies significantly across Europe and is usually higher in active volcanic zones with shallower

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Permian felsic volcanic rocks are collectively named the Gyűrűfű Rhyolite Formation in the Hungarian lithostratigraphic literature and they form the regionally most widespread Permian formation ( Fülöp 1994 ; Császár 2005 ; Szemerédi et al. 2020

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Permian felsic volcanic rocks are collectively named the Gyűrűfű Rhyolite Formation in the Hungarian lithostratigraphic literature and they form the regionally most widespread Permian formation ( Fülöp 1994 ; Császár 2005 ; Szemerédi et al. 2020

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literature on quartz recrystallization (for a detailed summary, see Tullis et al. 2000 ; Passchier and Trouw 2005 ). The quartz lens displays heterogeneous deformation, with domains of different recrystallization features (Fig.  2 ). The

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Central European Geology
Authors: Zsófia Pálos, István János Kovács, Dávid Karátson, Tamás Biró, Judit Sándorné Kovács, Éva Bertalan, Anikó Besnyi, György Falus, Tamás Fancsik, Martina Tribus, László Előd Aradi, Csaba Szabó, and Viktor Wesztergom

comprehensive overview with special respect to the estimated magmatic water contents. This will also provide a framework to interpret our results (Table  2 ). Table 2 Published literature data of volcanic phenocryst trace

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Central European Geology
Authors: Ildikó Gyollai, Ákos Kereszturi, and Elias Chatzitheodoridis

literature, the Zagami meteorite contains high p–T mineral phases. The shock features occur in thin veins and black glasses; the determined peak shock is p–T 31 ± 2 GPa and 1,220 °C ( Marti et al. 1995 ). El Goresy et al. ( 2000 ) and Malavergne et al. ( 2001

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, these fragments cannot be stromatolite fragments, but these clasts may represent pieces of calcite veins or any fresh-water limestone form, e.g., a speleothem or a laminated accrete fragment. As there is no data in the literature about a vein type

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Thus, such a diagram may be a useful tool in differentiating between partial melting and refertilization processes. However, in the vast xenolith literature, one can find a great number of papers publishing whole-rock analyses and many others publishing

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Central European Geology
Authors: Attila Demény, Alexandra Németh, Zoltán Kern, György Czuppon, Mihály Molnár, Szabolcs Leél-Őssy, Mihály Óvári, and József Stieber

review, in which the possible factors governing δ 13 C and δ 18 O carb values are thoroughly investigated. Due to the large number of related papers, the reader is advised to see their review of the scientific literature. The carbon isotope compositions

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