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spectral attributes; thus, they can be distinguished based on certain combinations of their respective Raman spectra ( F1, F2 discriminant functions in Skultéti et al. 2014 ) (Fig.  4 ). The U–S–R spectral space (or the U–S–R “triangle”) can therefore

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measured in mining wells (triangles), water wells (blue dots), hydrocarbon wells (crosses), geothermal wells (squares), and in thermometric wells (pentagons) in the area shown in Fig.  3 ] varies between 60 and 100 mW/m 2 ( Fernández et al. 1998 ; Correia

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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

. G: Columnar calcite microfabric in the VK-1 stalagmite, 2N photomicrograph. The white triangle indicates a series of upward-thinning laminae. H: Lateral truncation of laminae on the side of the stalagmite. I: Micritic laminae (M) with very reduced

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triangulation point land surveying triangle, in the crested wheatgrass population, in January 2012, on a cold winter day, under frozen soil and pollen-free conditions, in order to reduce disturbance caused by the drilling. Results The

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), triangles = sample MBFSZ-11133 (Sukoró) While sample MBFSZ-11133 (Sukoró) is chemically relatively homogeneous, sample HOM-2009.215 (Pákozd) exhibits two types of transformation zones ( Fig. 5d ). The type 1 zone appears as a thin infiltration inside the

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