North-South: Forecast of Socio-Economic and Political Dynamic (the end)

Author(s):  
I. Grishin

The publication represents the outcomes of the regular academic seminar “Modern problems of development” conducted by the IMEMO Center of the problems of development and modernization. The relationships between the Center and the Periphery, the prospects for the development of the North and the South in the light of Kondrat'ev's long cycles theory, new technological modes and transformation of social institutions are discussed. For the next ten years the major conflicts in the Middle East, Central Asia, Pakistan, Afghanistan and the Korean peninsula are forecasted.

Author(s):  
I. Grishin

This publication represents the material of the regular academic seminar “Modern problems of development” conducted by the IMEMO Center for the problems of development and modernization. The relationships between Center and Periphery, prospects for the development of the North and the South in the light of Kondratiev's long cycles theory, new technological modes and transformation of social institutions are discussed. It is forecasted that in the next ten years we will see new major conflicts in the Middle East, Central Asia, Pakistan, Afghanistan and the Korean Peninsula.


Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.


2015 ◽  
Vol 29 (2) ◽  
pp. 213-219 ◽  
Author(s):  
Elżbieta Radzka ◽  
Katarzyna Rymuza

Abstract The work is based on meteorological data recorded by nine stations of the Institute of Meteorology and Water Management located in east-central Poland from 1971 to 2005. The region encompasses the North Podlasian Lowland and the South Podlasian Lowland. Average values of selected agroclimate indicators for the growing season were determined. Moreover, principal component analysis was conducted to indicate elements that exerted the greatest influence on the agroclimate. Also, cluster analysis was carried out to select stations with similar agroclimate. Ward method was used for clustering and the Euclidean distance was applied. Principal component analysis revealed that the agroclimate of east-central Poland was predominantly affected by climatic water balance, number of days of active plant growth, length of the farming period, and the average air temperature during the growing season (Apr-Sept). Based on the analysis, the region of east-central Poland was divided into two groups (areas) with different agroclimatic conditions. The first area comprized the following stations: Szepietowo and Białowieża located in the North Podlasian Lowland and Biała Podlaska situated in the northern part of the South Podlasian Lowland. This area was characterized by shorter farming periods and a lower average air temperature during the growing season. The other group included the remaining stations located in the western part of both the Lowlands which was warmer and where greater water deficits were recorded.


2018 ◽  
Vol 5 ◽  
pp. 131-165 ◽  
Author(s):  
Valentin Zuchuat ◽  
Arve R.N. Sleveland ◽  
Douglas A. Sprinkel ◽  
Algirdas Rimkus ◽  
Alvar Braathen ◽  
...  

Based on a methodic sedimentological analysis, the Late Jurassic (Oxfordian) Curtis Formation unravels the intricate facies variability which occurs in a tide-dominated, fluvially starved, low-gradient, semi-enclosed epicontinental basin. This unit crops out in east-central Utah, between the eolian deposits of the underlying Middle Jurassic (Callovian) Entrada Sandstone, from which it is separated by the J-3 unconformity, and the conformable overlying supratidal Summerville Formation of Oxfordian age. A high-resolution sedimentary analysis of the succession led to the recognition of eight facies associations (FA) with six sub-facies associations. Based on the specific three-dimensional arrangement of these eight facies associations, it is proposed to separate the Curtis Formation into three sub-units: the lower, middle and upper Curtis. The J-3 unconformity defines the base of the lower Curtis, which consists of upper shoreface to beach deposits (FA 2), mud-domi­nated (FA 3a) and sand-dominated heterolithic subtidal flat (FA 3b), sand-rich sub- to supratidal flat (FA 4a) and correlative tidal channel infill (FA 4c). It is capped by the middle Curtis, which coincides with the sub- to intertidal channel-dune-flat complex of FA 5, and its lower boundary corresponds to a transgressive surface of regional extent, identified as the Major Transgressive Surface (MTS). This surface suggests a potential correlation between the middle and the upper Curtis and the neighboring Todilto Member of the Wanakah Forma­tion or Todilto Formation. The upper Curtis consists of the heterolithic upper sub- to intertidal flat (FA 6) and coastal dry eolian dunes belonging to the Moab Member of the Curtis Formation (FA 7), and it conformably overlies the middle Curtis. The spatial distribution of these sub-units supports the distinction of three different sectors across the study area: sector 1 in the north, sector 2 in the south-southwest, and sector 3 in the east. In sector 1, the Curtis Formation is represented by its three sub-units, whereas sector 2 is dominated by the middle and upper Curtis, and sector 3 encompasses the extent of the Moab Member of the Curtis Formation. This study also highlights the composite nature of the J-3 unconformity, which was impacted by various processes occurring before the Curtis Formation was deposited, as well as during the development of the lower and middle Curtis. Local collapse features within the lower and middle Curtis are linked to sand fluid over­pressure within a remobilized sandy substratum, potentially triggered by seismic activity. Furthermore, the occurrence of a sub-regional angular relationship between the middle Curtis and substratum implies that the area of study was impacted by a regional deformational event during the Late Jurassic, before the deposition of the middle Curtis. The spatial distribution of these sub-units supports the distinction of three different sectors across the study area: sector 1 in the north, sector 2 in the south-southwest, and sector 3 in the east. In sector 1, the Curtis For­mation is represented by its three sub-units, whereas sector 2 is dominated by the middle and upper Curtis, and sector 3 encompasses the extent of the Moab Member of the Curtis Formation. This study also highlights the composite nature of the J-3 unconformity, which was impacted by various processes occurring before the Curtis Formation was deposited, as well as during the development of the lower and middle Curtis. Local collapse features within the lower and middle Curtis are linked to sand fluid over­pressure within a remobilized sandy substratum, potentially triggered by seismic activity. Furthermore, the occurrence of a sub-regional angular relationship between the middle Curtis and substratum implies that the area of study was impacted by a regional deformational event during the Late Jurassic, before the deposition of the middle Curtis.


2019 ◽  
Vol 11 (03) ◽  
pp. 50-58
Author(s):  
Erik MOBRAND ◽  
Hyejin KIM

Southeast Asia’s significance to the Korean peninsula is growing. South Korea has deepening trade, investment and assistance relationships in the region, while ASEAN’s non-judgmental approach to diplomacy is useful in dealing with Pyongyang. Beyond hosting summits between American and North Korean leaders, Southeast Asia is in a position to mediate North Korea’s greater international engagement and to assist in the acceleration of interaction between the North and the South.


Author(s):  
Valery Yu. Mishin ◽  
◽  
Anna V. Simonenok ◽  

Moon Jae-in came to power in May 2017 in the wake of the Korean political crisis and impeachment of the previous president Park Geyn-hye. Since the very first days of his leadership President Moon has set a course for a sequential transformation of the inter-Korean relations and prevention of the nuclear crisis on the Korean Peninsula. The cornerstone of his program was the idea that the denuclearization of North Korea and the establishment of the long-lasting peace on the Korean Peninsula is possible provided that the North-South relations are normalized and Pyongyang is involved into the constructive peaceful dialogue. The authors demonstrate how Moon Jae-in was able to start the renaissance in the inter-Koran relations. He used the experience of the previous liberal governments of the Republic of Korea and successfully developed and enhanced the famous Sunshine Policy with his own ideas. The first stage of Moon Jane-in's presidency was marked with some serious foreign policy achievements. Thanks to the tactic of “summit diplomacy” President Moon was able to achieve significant reduction in tensions on the Korean Peninsula, which resulted in the fact that relations between the North and the South became more friendly and trustworthy. The historical documents signed during these summits - the Panmunjom Declaration (April 2018) and the Comprehensive Military Agreement (September 2018) - and their fast practical implementation can also be considered as President Moon's success. Further advancement of Moon Jae-in's course for building positive relationships with the DPRK faced serious obstruction from the United States. The authors show how simultaneously with settlement of inter-Korean relations President Moon had to deal with another difficult task - neutralization of the external factors (US sanctions and disagreements between Washington and Pyongyang) that were harmful for the development of the North Korea-South Korea relations. The tactics of being a mediator between the United States and North Korea chosen by Moon Jae-in was quite efficient in the beginning. The blatant enemies - Pyongyang and Washington - clamped down on their confrontation and sat at the negotiating table. However, the intransigence of Washington on the issue of a gradual and phase-based denuclearization of North Korea and withdrawal of sanctions altogether with the non-constructive criticism of the South Korean opposition made Moon Jae-in a hostage of the situation, limiting his potentially independent and substantive steps in foreign policy. Meanwhile, the authors of the research have come to the conclusion that on some issues President Moon was able to achieve much more than his predecessors. Despite the fact that he was unable to achieve a full-scaled settlement of the inter-Korean relations he did everything possible under the existing circumstances. Nowadays one can say that the challenges of the North Korean nuclear missile program and security on the Korean Peninsula are no longer entirely military topics, they are even more likely to be diplomatic issues. This fact is un-doubtfully his great accomplishment. Thus, it is possible to foresee good perspectives for the further declining level of the regional tensions and for the development of the inter-Korean relations.


1987 ◽  
Vol 4 ◽  
Author(s):  
Daniel Schelling

Between the Tethyan sediments to the north and the Main Boundary Thrust to the south ten lithotectonic units have been identified in the Rolwaling-Lapchi Kang Himalayas and the Tamba Kosi region of east-central Nepal. These are (1) the Rolwaling Granites, (2) the Rolwaling Paragneisses, (3) the Rolwaling Migmatites, (4) the Alampu Schists, (5) the Khare Phyllites , (6) The Chagu-ChilangkaAugen Gneisses; (7) The Laduk Phyllites, (8) the Suri Dhoban Augen Gneisses, (9) the Rarnechap Group, and (10) the Mahabharat Crystallines. The Main Central Thrust (MCT) is a major lithologic, metamorphic and structural discontinuity separating the overthrust Higher Himalayan crystallines from the underthrust Lesser Himalayan metasediments. The Mahabharat Crystallines are an outlying klippe of Higher Himalayan rocks, underlain by the MCT, that has been thrust a minimum of 80 kilometers over the underlying Lesser Himalayan metasediments. Extending approximately 5 km below the MCT and 15 km above the MCT the Himalayas are a shear-thrust zone exhibiting ductile, brittle-ductile and brittle deformation as well as an inverted metamorphic sequence.


Author(s):  
Bernard Reich ◽  
Sanford R. Silverburg ◽  
David Ettinger

Dating back to biblical times, the area we refer to as the Middle East has, throughout the course of history, defied attempts to precisely define it. Until today, the region’s contours remain shrouded in geographic ambiguity. Through the centuries, the Middle East, or parts thereof, has been variously referred to as “Le Orient,” “Proche Orient,” “Anatolia,” “North Africa,” “the Persian Gulf region,” “Arabian Peninsula,” “the Levant,” “the Fertile Crescent,” “Asia Minor,” “the Maghreb,” “Southwest Asia,” “the Caspian region,” and “Greater Middle East.” Merriam-Webster Geographical Dictionary labels it “an indefinite and unofficial term.” Long before being adopted in common parlance, the term “Middle East” was a Western invention used by military strategists and governments in the 19th and 20th centuries to denote areas to the east of western Europe. As part of the Ottoman Empire, it extended from Algeria in the west to Iraq in the east, parts of Russia and Hungary to the north, and the Arabian Peninsula to the south. The term “Near East,” often used synonymously, was popularized after the dismantlement of the Ottoman Empire after World War I, referring to the area at the hub of Europe, Africa, and Asia that served as a crossroads and bridge among the three continents and to the various states around the eastern areas of the Mediterranean Sea. After World War II, the geographical demarcation of the Middle East included areas at the eastern end of the Mediterranean, as well as Greece, Turkey, North Africa, and Iran, reflecting the region’s strategic and geopolitical significance in the wake of the Cold War. Although scholars of the area continue to differ in their definitions of the region, this bibliography will focus on the core region generally regarded as the Middle East, bounded by Turkey to the north, Iran to the east, Egypt to the west, and Yemen to the south. It does not include North Africa, the Sudan, or Central Asia. The first section includes a list of General Overviews and introductory works and those on the region’s Geography, History, Politics, Economics, and International Relations. Important related topics such as Petroleum and Energy and the Arab-Israeli Conflict are also treated. In light of recent developments, we have added the “Arab Spring”. The second section is devoted individually to The Countries of the Middle East. Although the emphasis is on contemporary works, classic titles are included as well, in keeping with the authors’ goal to assist researchers in locating the best works on the region.


Zootaxa ◽  
2019 ◽  
Vol 4555 (2) ◽  
pp. 187 ◽  
Author(s):  
ANTE VUJIĆ ◽  
SNEŽANA RADENKOVIĆ ◽  
LAURA LIKOV ◽  
ANDRIJANA ANDRIĆ ◽  
EBRAHIM GILASIAN ◽  
...  

Two new remarkable species of the genus Merodon Meigen (Diptera: Syrphidae) are described from biodiversity hotspots in the Middle East: Merodon eumerusi Vujić, Radenković et Likov sp. n. and Merodon mixtum Vujić, Radenković et Likov sp. n. Although M. eumerusi, from the Mountains of Central Asia, belongs clearly to the lineage of M. avidus-nigritarsis, it possesses some unique features within the genus that are also present in other Merodontini genera. M. mixtum, from the Irano-Anatolian mountains, has typical characters of different species groups within the M. albifrons lineage. Here, we discuss the unusual apomorphic characters of these newly discovered taxa and highlight the need for further analyses to ascertain the phylogenetic relationships within the tribe Merodontini and the genus Merodon. 


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