Претрага
65 items
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Mapping and classifying large deformation from digital imagery: application to analogue models of lithosphere deformation
kontinentalna tektonika: kompresija, kontinentalna tektonika: ekstenzija, kontinentalna tektonika: transkurentni i transformni rasedi, pukotine, rasedi, zone snažnih deformacija, kinematika deformacija kore i omotača, teorijska mehanika, modelovanje... holds: F = RU = VR (B1) Knowledge on U and U−1 leads to V and R (recall that RRT = I) by: R = FU−1 V = FRT (B2) Hoger & Carlson (1984) provide expressions for U in closed form as well as its inverse, without the need to determine the tensor square root of the right Cauchy-Green tensor C, as U = √ ...
... decomposition holds: F=RU=VR (Bl) Knowledge on U and U~! leads to V and R (recall that RR’ = I) by: R=FU! V=FR’ (B2) Hoger & Carlson (1984) provide expressions for U in closed form as well as its inverse, without the need to determine the tensor square root of the right Cauchy-Green tensor C, as U = VC. ...Taco Broerse, Nemanja Krstekanić, Cor Kasbergen, Ernst Willingshofer. "Mapping and classifying large deformation from digital imagery: application to analogue models of lithosphere deformation" in Geophysical Journal International, Oxford University Press (OUP) (2021). https://doi.org/10.1093/gji/ggab120
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Threshold-induced correlations in the Random Field Ising Model
... the size of the avalanche type i, while ˆT iSb and ˆS iSb are duration and size of the scaled avalanche type ˆ iSb , respectively. Analogous expressions = = −ˆ ˆT i b V T i V b S i b V b S i V(S ; ) ( ; )/ , (S ; ) ( ; ), (4)b x b x x th th th 1 th hold for the duration T(i; Vth) and size ∫= ...Sanja Janićević, Dragutin Jovković, Lasse Laurson, Đorđe Spasojević. "Threshold-induced correlations in the Random Field Ising Model" in Scientific Reports, Springer Science and Business Media LLC (2018). https://doi.org/10.1038/s41598-018-20759-6
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Application of Project Management Process on Environmental Management System Improvement in Mining-Energy Complexes
... one activity (i, j) [8]. The total, free, and independent time reserves are determined according to activity duration, by means of the following expressions [8]: P ij = (TL)j − (TE)i − tij (5) S ij = (TE)j − (TE)i − tij (6) Energies 2016, 9, 1071 13 of 20 N ij = max {0, (TE)j − (TL)i − tij} (7) ...Jelena Malenović Nikolić, Dejan Vasović , Ivana Filipović , Stevan Mušicki, Ivica Ristović . "Application of Project Management Process on Environmental Management System Improvement in Mining-Energy Complexes" in Energies (2016). https://doi.org/https://doi.org/10.3390/en9121071
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Strain partitioning in a large intracontinental strike-slip system accommodating backarc-convex orocline formation: The Circum-Moesian Fault System of the Carpatho-Balkanides
Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga (2022)oroklini, raspodela deformacija, transkurentna kretanja, Karpato-balkanidi, Cirkum-mezijski rasedni sistem... Timok Faults (Mladenović et al., 2019; Krstekanić et al., 2020. This observation enabled a sepa- ration of kinematics of these different coeval expressions of strain par- titioning during the oroclinal formation (see also Krstekanić et al., 2020). It is important to note that in most situations of ...Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga. "Strain partitioning in a large intracontinental strike-slip system accommodating backarc-convex orocline formation: The Circum-Moesian Fault System of the Carpatho-Balkanides" in Global and Planetary Change, Elsevier BV (2022). https://doi.org/10.1016/j.gloplacha.2021.103714
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Badenske školjke jugoistočnog oboda Panonskkog basena (Centralni Paratetis)
Gordana M. Jovanović (2014-12-05)Rad obuhvata detaljnu studiju badenskih školjaka koje potiču sa terenajugoistočnog oboda Panonskog basena (Centralni Paratetis). Proučavani su lokaliteti naprostorima Srbije (Fruška gora, Golubac, okolina Beograda, Aranđelovca, Koceljeva,Loznica) i severoistočne Bosne (Ugljevik). Pored taksonomske analize i paleontološkihopisa bivalvija, u radu je dat i spisak revidovanih vrsta koje su do sada pronađene usedimentima badenskog kata istraživanog terena. Do sada je ukupno poznato 41familija, 108 rodova i 174 taksona. Identifikovano je 170 bivalvijskih vrsta, međukojima su neke prvi put konstatovane na ovim ...školjke, baden, Panonski basen (Centralni Paratetis), stratigrafija,paleoekologija, paleogeografija, paleobiogeografija... paleontologie Univ. de Paris. Fac. des Science d' Orsay, 103 pp. Laurain, M. 1980. Crassostrea gryphoides et C. gingensis (Schlotheim, 1813) deux expressions morphologiques d'une meme espece (Miocene, Bivalvia). Geobios, 13: 21-43. Lauriat-Rage, A., Ben Moussa, A., Piquet, J.-P. Saint Martin J.P. 1999 ...Gordana M. Jovanović. "Badenske školjke jugoistočnog oboda Panonskkog basena (Centralni Paratetis)" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2014-12-05)