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https://ceet.vsb.cz/en/ceet
personalities, where innovative thoughts and ideas are born and developed. Learning for practice has become an integral part of our work culture. CENET ENET Centre visit
https://advances.vsb.cz/data/articles/2013/Vol%2011,%20No%201/Electrical%20and%20Electronic%20Engineering/Second%20Order%20Low-Pass%20and%20High-Pass%20Filter%20Designs%20Using%20Method%20of%20Synthetic%20Immitance%20Elements.pdf
These electronic applications can be used especially in mobile devices mainly because of positive properties of current con- veyors. These active elements allow
http://homel.vsb.cz/~hor10/Vyuka/PGIT/Cestovni_prikaz_formular_vzor.xls
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https://advances.vsb.cz/data/articles/2013/Vol%2011,%20No%203/Applied%20Mathematics/Semi-Smooth%20Newton%20Method%20for%20Solving%202D%20Contact%20Problems%20with%20Tresca%20and%20Coulomb%20Friction.pdf
let mk be their number. Moreover, we denote n = n1 + n2 and m = m1. The stiffness matrix and the load vector corresponding to Ωk are denoted by Kk ∈ R2nk×2nk and
https://gisak.vsb.cz/GIS_Ostrava/GIS_Ova_2000/Sbornik/Pokorny/Referat.htm
ovac� k�ivky (1966). Tyto metody byly ur�eny hlavn� pro pr�ci s objekty ve vnit�n� pam�ti. V �l�nku se zam���me na PDS podporuj�c�
http://geologie.vsb.cz/geomorfologie/Cviceni/Zadani_1/Zadani_1.htm
Geomorfologie Geomorfologie Zad�n�: 1 Pr�ce s topografickou mapou Pom�cky: Topografick� mapa (obr. 1); prav�tko (2 x troj�heln�k); kru��tko; �hlom�r; psac� pot�eby.
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323 Thu(2) 35-319 82 College of Science and Technology Department of Electronics and Information Engineering EIEN315-03 Major Elective FUNDAMENTALS OF SEMICONDUCTOR DEVICES II(English)
http://geologie.vsb.cz/PETROLOGIE2013/horninotvorne-mineraly-muskovit.htm
zv�tr�v�n� (jako biotit). Vyskytuje se v magmatick�ch hornin�ch - v pegmatitech (P�stecko, K��enec u Plan� u Mari�nsk�ch L�zn�, Doln� Bory, Mar��kov), v granitoidech (P�ibyslavice, Mr�kot�
https://kf.vsb.cz/Kontakt/pubziv.htm
O. �ivotsk�, I. �afa��k, L. Obalov�, Magnetically modified nanogold-biosilica composite as an effective catalyst for CO oxidation, Arabian Journal of Chemistry,
http://geologie.vsb.cz/PETROLOGIE2013/horninotvorne-slozky-dolomit.htm
2,9 g/cm3. D�le�it� upozorn�n�: na rozd�l od kalcitu a aragonitu NEREAGUJE s kyselinou chlorovod�kovou. Petrografick� charakteristika
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tetraedrit TETRAEDRIT - Cu12Sb4S13 �ed� krystal tetraedritu v kalcitov� �ilovin�. P��bram, d�l Anna. ���ka vzorku 5�4 cm. Sb�rky �esk� geologick� slu�by, foto J.
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stupn�m, kter� prob�h� jako prvn� metamorfn� reakce p�i metamorf�ze poh�ben�m. Horniny v t�to f�zi prod�l�vaj� jen rekrystalizaci za n�zk�ch
http://geologie.vsb.cz/PETROLOGIE2013/horninotvorne-slozky-biotit.htm
krystaly s pseudohexagnon�ln�m omezen�m, �ast�ji v podob� lupen�, kter� jsou pru�n� a� k�ehk�. M� �ernou �i tmav�hn�dou barvu, perle�ov� lesk, b�l
https://www.fei.vsb.cz/export/sites/fei/480/.content/galerie-souboru/Jena15_poster.pdf
mirror. 1. Experimental setup Spectrometer CL BS P BC A Polystyrene Box M2 MO Wavelength (nm) In te n si ty (A .U .) S p e c tr a l
https://kf.vsb.cz/Veda/poster/Jena15_poster.pdf
mirror. 1. Experimental setup Spectrometer CL BS P BC A Polystyrene Box M2 MO Wavelength (nm) In te n si ty (A .U .) S p e c tr a l
https://advances.vsb.cz/data/articles/2015/Vol%2013,%20No%204/Electrical%20and%20Electronic%20Engineering/Processor%20PIC18F46K22%20Applied%20as%20DTMF%20Generator.pdf
down peak), see Fig. 2. Fig. 2: Approximation of sinus function by 32 values. The period of sinus function is divided into 32 el- ements and appropriate time interval
https://ieec.vsb.cz/export/sites/ieec/en/programme/presentations-2025/presentations-en/section-4/presentation_dziok.pdf
E P , G lo b a l M e rc u ry A s s e s s m e n t – S o u rc e s , E m is s io n s , R e le a s e s a n d E n v ir o n m e n ta l T ra
https://advances.vsb.cz/data/articles/2013/Vol%2011,%20No%202/Electrical%20and%20Electronic%20Engineering/Performance%20Investigation%20of%20the%20RBF%20Localization%20Algorithm.pdf
1. Introduction The basic requirement for Location Based Services (LBS) [1], [2], is knowledge of the mobile device po- sition. This can be achieved in many different
http://geologie.vsb.cz/inzgeol/sylaby/01%20Uvod/01%20kap.htm
a hodnocen� in�en�rskogeologick�ch pom�r�. Podle specifick�ho zam��en� se vyvinuly n�kter� d�l�� obory jako: � In�en�rsk� petrologie, zam��
http://gisak.vsb.cz/GIS_Ostrava/GIS_Ova_2014/proceedings/papers/gis201452681752c3ba5.pdf
indicators which cannot be used Brno A,B,C,D,E,G,L,M,N,O,P, Q,R F,H,I,J,K Ostrava F,H,I,J,K,L,M,N,O,P,Q,R A,B,C,D,E,G Plzeň A,B,C,D,E,F,G,H,I,J,K,