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.
Authors:Ildikó Gyollai, Ákos Kereszturi and Elias Chatzitheodoridis
backscattered electrons (BSE) images acquired in slow rate of scan modes
Mineral composition was calculated using the INCA software with oxide composition in weight%, and elemental composition in atom%. Table 2 shows the atom% ratios of elements at
Schutter [ 14 , 22 ] on blended cements, the BFS was here added as a separate component to the concrete mix and the slag-to-binder ratios varied between 0 and 85%. Moreover, backscattered electron (BSE) images were taken in a scanning electron microscope
Authors:János Haas, Tamás Budai, István Dunkl, Éva Farics, Sándor Józsa, Szilvia Kövér, Annette E. Götz, Olga Piros and Péter Szeitz
fresh groundmass [backscattered electrons (BSE) image, 775.9 m]. (c) Tectonic breccia in the shear zone (1N, 779.5 m). (d) Andesite with strongly sericited plagioclase and pseudomorphs after pyroxene (1N, 790.4 m). (e) Texture of andesite with sericited
Authors:Alfredo Román-Tejeda and Heriberto Pfeiffer
scratched and pulverized, some preferential orientation was observed on the XRD pattern in the form of a considerably high-intensity 002 peak (2 θ = 30.6º).
XRD pattern ( A ) and BSEimage ( B ) of the α-LiBO 2
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
The plagioclases were analyzed in sample no. 9, collected at Vilma-pihenő rest. The back-scattered electron (BSE) images of idiomorphic minerals show darker (Na-rich) and lighter (Ca
Authors:Ildikó Gyollai, Ákos Kereszturi, Zsolt Kereszty, Máté Szabó and Elias Chatzitheodoridis
to host olivine. The BSEimage of ak11 shows floating lath-shaped crystallites in dark matrix; the matrix has feldspar composition. The rim of the akim11 object shows moderate Fe and Ca enrichment, but a decrease of Al. The ak11 object shows strong