Titlebook: Supercomputing; Third Russian Superc Vladimir Voevodin,Sergey Sobolev Conference proceedings 2017 Springer International Publishing AG 2017

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An Approach for Parallel Solving the Multicriterial Optimization Problems with Non-convex Constraintis provided. The results of the computational experiments have demonstrated such an approach to allow reducing the computational costs of solving the multicriterial optimization problems essentially – tens and hundred times.

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The Combinatorial Modelling Approach to Study Sustainable Energy Development of Vietnamcience of Vietnamese Academy of Science and Technology performed the study of Vietnam sustainable energy development from 2015 to 2030. Based on data of this study the combinatorial modelling methods are applied to the formation and analysis of Vietnam energy development options taking into account

dysphagia

efinition, “because form is a response to a process operating over time” as Giardino and Vitek (1988) state. Based on the definition in Chapter 1, the genesis and the phenotypes of active (Sect. 8.1.1), inactive (Sect. 8.1.2) and relict (Sect. 8.1.3) rockglaciers will be discussed first. In comparis

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efinition, “because form is a response to a process operating over time” as Giardino and Vitek (1988) state. Based on the definition in Chapter 1, the genesis and the phenotypes of active (Sect. 8.1.1), inactive (Sect. 8.1.2) and relict (Sect. 8.1.3) rockglaciers will be discussed first. In comparis

纪念

Iosif Meyerov,Sergey Bastrakov,Konstantin Barkalov,Alexander Sysoyev,Victor Gergelefinition, “because form is a response to a process operating over time” as Giardino and Vitek (1988) state. Based on the definition in Chapter 1, the genesis and the phenotypes of active (Sect. 8.1.1), inactive (Sect. 8.1.2) and relict (Sect. 8.1.3) rockglaciers will be discussed first. In comparis

苦涩

Nikolai Zamarashkin,Dmitry Zheltkovular and submolecular scales. The primary weathering mechanisms are triggered by activating processes, promoted by a variety of activating agencies (Table 5.1). The weathering response is the progression of mineralogical, petrological and mechanical properties as they change through time. These chan

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