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petrography are also recognized, due to the recrystallization of the studied sample inherited from mylonitization, which is probably ubiquitous in the study area. Geologic background MZ (Ófalu Group) The MZ is a

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structure of honey can change, the mobility of ions and charged groups can increase causing a decrease of electrical impedance of honey. The recrystallization of honey, the recovery to the original state presumably takes a relatively long time – some weeks

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garnets in deformed aplite. Szederkényi ( 1977 , 1983 ) described intensive shearing at greenschist/amphibolite facies in amphibolite, whereas M. Tóth et al. ( 2005 ) assumed the recrystallization temperature of mylonite to be approximately 350 °C. The

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Central European Geology
Authors: Ildikó Gyollai, Ildikó Gyollai, Szaniszló Bérczi, Krisztián Fintor, Szabolcs Nagy, and Arnold Gucsik

The Mócs chondrite was studied by optical microscopy, element mapping, as well as scanning electron microscope backscattered electron (SEM—BSE) imaging, in order to gain a better understanding of the thermal metamorphic as well as post-shock annealing evolution and the mineralogical signatures in this meteorite. The studied thin section of Mócs meteorite contains 26 chondrules with a variety of chondrule textures, which are characterized by a blurry rim. The chondrules mostly consist of pyroxene and olivine, whereas feldspars occur only in the recrystallized groundmass, chondrule mesostasis, and mineral melt inside and beyond the shock veins. It was found that the matrix was completely recrystallized. According to the scanning electron microscope and optical microscope observations mentioned above, it can be concluded that the Mócs chondrite is a 6.5 petrographic type.

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Interventional Medicine and Applied Science
Authors: Sergei N. Danilchenko, Aleksei N. Kalinkevich, Roman A. Moskalenko, Vladimir N. Kuznetsov, Aleksandr V. Kochenko, Evgenia V. Husak, Vadim V. Starikov, Fuyan Liu, Junhu Meng, and Jinjun Lü

) recrystallization of bioapatite accompanied by the removal of CO 3 2− at the temperatures of 600–900 °C; and (3) bioapatite phase decomposition with the formation of other calcium phases [e.g., beta-tricalcium phosphate (β-TCP) and CaO] in the range from 900 to 1

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“destabilization” of this microstructure and the consequent recrystallization of the Sn phase due to thermal stress under thermal shock conditions pose considerable challenges to the reliability testing of solder joints [ 14 ]. Under the effect of high temperature

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transformation, which previously overlapped as an effect of the MA process (Figs. 2 , 3 ). This phenomenon may be connected with the recovery and recrystallisation effects. Intensity and position of endothermic peaks were similar to those of the based Astaloy

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digestion. Components of starch, amylose, and amylopectin are responsible for the short-term and long-term retrogradation, respectively. Crystalline amylose was found to be the nucleus for amylopectin recrystallisation in long-term processes ( Keetels et al

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Central European Geology
Authors: Máté Zsigmond Leskó, Richárd Zoltán Papp, Boglárka Anna Topa, Ferenc Kristály, Tamás Vigh, and Norbert Zajzon

contained “tripoli.” Tripoli is pure recrystallized quartz, of a crumbly nature, which appears randomly within the footwall. Tripoli can be found in mm-dm-sized lenses. It does not dissolve in acetic acid, so the amount of tripoli is added to the common

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PET recrystallization was observed [ 20 ]. Addition of waste PET caused changes occurring in studied compositions as an effect of temperature, while the biggest changes were observed in decomposition temperature. The increase of PET addition

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