Improvement of recruitment system in a large regional Bank using agile technology

Final qualification work (master thesis) on 81 page (A4 format, font Times New Roman, font size 14, 1.5 line spacing), excluding attachments. Number of tables – 6 (excluding annexes). Number of figures – 16 (excluding applications). Number of formulas-0 (excluding applications). Final qualifying work consists of an introduction, three parts, conclusion, bibliography, applications. This work begins with an introduction that describes the relevance of the master's thesis, problem statement, definition of the purpose and objectives of the work, its object and subject, scientific novelty, research methods, practical significance and research methods. In the first Chapter of this work, recruitment as a key element of the human resources management system, as well as the features of recruitment in Russia and abroad are considered and analyzed. The second part of the work presents the characteristics of the organization as an object of management, analysis and evaluation of recruitment system in a large regional Bank, monitoring and evaluation of recruitment quality. The third part contains recommendations for changes, the introduction of agile-technology in the HR-business process "recruiting" is proposed, a list of necessary activities is developed.Выпускная квалификационная работа (магистерская диссертация) выполнена на 81 листе (формат А4, шрифт Times New Roman, кегль 14, интерлиньяж 1.5) без учета приложений. Количество таблиц – 6 (без учета приложений). Количество рисунков – 16 (без учета приложений). Количество формул – 0 (без учета приложений). Выпускная квалификационная работа состоит из введения, трех частей, заключения, библиографического списка, приложений. Данная работа начинается с введения, которое описывает актуальность магистерской диссертационной работы, постановку проблемы, определение цели и задач работы, её объекта и предмета, научной новизны, методов исследования, практической значимости и методов исследования. в первой главе данной работы рассмотрены и проанализированы рекрутинг как ключевой элемент системы управления человеческими ресурсами, а также особенности подбора персонала в России и за рубежом. во второй части работы представлены характеристика организации как объекта управления. анализ и оценка системы подбора персонала в крупном региональном банке, мониторинг и оценка качества рекрутинга. третья часть содержит рекомендации по изменениям. предложено внедрение agile-технологии в HR-бизнес-процесс «рекрутинг персонала», разработан перечень необходимых для этого мероприятий

Crustal structure of the Mendeleev Rise and the Chukchi Plateau (Arctic Ocean) along the Russian wide-angle and multichannel seismic reflection experiment “Arctic-2012”

We present a seismic and density model for the crust and the uppermost mantle of the Arctic Ocean off-shore Chukotka down to a 40 km depth along a 740-km long latitudinal (at ca. 77°N) “Arctic-2012” wide-angle/MCS profile. Joint seismic and gravity modeling indicates significant differences in the crustal velocity and density structure of the northeastern Vilkitsky Trough, the Mendeleev Rise, the Chukchi Basin, and the Chukchi Plateau. The Vilkitsky Trough and the Chukchi Basin have a thin crust (23 km and 18 km, correspondingly), 6–8 km thick sedimentary cover, 3–6 km thick upper/middle crust (with the smallest thickness of 3–4 km beneath the Chukchi Basin), and 9–10 km thick lower crust. The uppermost mantle of the Chukchi Basin has a high density (3.27–3.31 g/cm3) and a low velocity (Vp ∼ 7.8 km/s), which we explain by 5–10% serpentinization of mantle peridotite at a 22–35 km depth as a result of crustal hyperextension and seawater penetration. The Chukchi Plateau and the Mendeleev Rise have a thick crust (28–29 km and 33–34 km, correspondingly), underlain by a normal mantle (Vp ∼ 8.0 km/s). The Chukchi Plateau has a 2‐4 km thick sedimentary cover, a thick (15–18 km) upper/middle crust with low-Vp, low-density lenses interpreted as magmatic intrusions, and a 9–12 km thick lower crust. The Mendeleev Rise has a 3–7 km thick sedimentary cover (most of which is formed by metasediments with a possible presence of volcanic rocks), a 7–8 km thick upper/middle crust, and a thick (20 km) lower crust which includes a 3–4 km thick high-velocity (Vp ∼ 7.3 km/s) underplated magmatic material. The high density anomaly (at depths >35 km) below the Mendeleev Rise is interpreted as an eclogitic body in the upper mantle lithosphere. Seismic Vp and Vp/Vs structure of the crust along the “Arctic-2012” profile indicates its continental nature: a 3–18 km thick upper/middle crustal layer with Vp ∼ 6.0–6.8 km/s and Vp/Vs ∼ 1.70–1.73 typical of felsic-intermediate continental upper crust is present along the entire profile. Strong variability of the crustal structure along the profile reflects its significant modification by metamorphism and magmatism, possibly related to the High-Arctic Large Igneous Province and localized lithosphere extension beneath the Chukchi Basin