scholarly journals Signification Des Structures N-S Du Plateau Des Aït Maghlif (Region D’eç-Çour, Versant Meridional Du Massif Ancien Du Haut Atlas, Maroc)

2016 ◽  
Vol 12 (15) ◽  
pp. 365
Author(s):  
Anas Emran ◽  
Fida Medina

Structural study of the recent deformations of the Eç-çour area, located on the southern slope of the massif ancien of the High Atlas, has allowed us to obtain the following results: (1) In the Ait Maghlif plateau, on the northern border of the Siroua volcanic massif, the N-S structures that are bounded by the reverse Imini fault to the north and the left-lateral Tawyalt−Agandiy fault in the south, correspond to forced folds on reverse faults and related folds related to a NW-SE compression, some of which were former normal syndepositional faults that were active in Cretaceous times; an intermediate phase corresponding to a NNE-SSW compression which is thought to have triggered the Siroua volcanism; (2) along de South Atlas Fault, the recent tectonism is expressed by folding and faulting of several Quaternary alluvial fans, some of which bear reverse/dextral slickensides.

2019 ◽  
Vol 46 (5) ◽  
pp. 485-495
Author(s):  
A. K. Ambrosimov

The experimental data presented in the article show that in the North-Eastern sector of the Middle Caspian sea in the area of Peschanomyssky uplift there is a disturbance of currents caused by the interaction of the cyclonic cycle with the southern slope of the uplift. As a result of this interaction, the waters of the cyclonic cycle are divided into branches – the lower and upper. The lower bottom branch is thrown by the uplift in the South-Western direction, where at the Cape of the uplift it collides with the waters flowing down the bottom of the South-Buzachinsky deflection in the South-Eastern direction, and the upper branch, consisting of near-surface and intermediate cold waters, is pushed up and passes through the uplift. As a result of the rise of cold water in the surface layer formed upwelling, which extends to the entire North-Eastern region of the sea.


2020 ◽  
Author(s):  
Morten Mattingsdal ◽  
S. Sunna Ebenesersdóttir ◽  
Kristjan H. S. Moore ◽  
Ole A. Andreassen ◽  
Thomas F. Hansen ◽  
...  

AbstractThe aim of the present study was to describe the genetic structure of the Norwegian population using genotypes from 6369 unrelated individuals with detailed information about places of residence. Using standard single marker- and haplotype-based approaches, we report evidence of two regions with distinctive patterns of genetic variation, one in the far northeast, and another in the south of Norway, as indicated by fixation indices, haplotype sharing, homozygosity and effective population size. We detect and quantify a component of Uralic Sami ancestry that is enriched in the North. On a finer scale, we find that rates of migration have been affected by topography like mountain ridges. In the broader Scandinavian context, we detect elevated relatedness between the mid- and northern border areas towards Sweden. The main finding of this study is that despite Norway’s long maritime history and as a former Danish territory, the region closest to mainland Europe in the south appears to have been the most isolated region in Norway, highlighting the open sea as a barrier to gene flow.


1965 ◽  
Vol S7-VII (3) ◽  
pp. 479-486 ◽  
Author(s):  
Michel Prager

Abstract The Saint-Guiral-Liron granite consists of a porphyritic granodiorite intruded into folded Paleozoic schists of the Cevennes mountains to the north and the Vigan nappe area to the south. The composition of the granodiorite is homogeneous and nearly isotropic. Metamorphism at the northern border of the granodiorite resulted in the formation of gneiss, and at the southern border, of flint. The southern contact indicates extremely intense emplacement with development of an aureole of exothermal contact metamorphism. The joint systems of the northern and southern borders are described and interpreted.


1990 ◽  
Vol 127 (5) ◽  
pp. 407-426 ◽  
Author(s):  
W. I. Mitchell ◽  
B. Owens

AbstractThe western part of the Fintona Block is divided into four fault-bounded segments that contain red-bed sediments formerly assigned to the Lower Old Red Sandstone.Dating by miospores indicates the presence of deposits of early Devonian age in the Irvinestown Segment, late Viséan–early Silesian age in the Tempo–Lisbellaw Segment, and late Viséan–early Silesian and late Silesian ages in the Milltown Segment. Northward migration of the early Carboniferous marine transgression in the northern part of Ireland coincided with the sequential propagation of back-stepping faults and resulted in the development of diachronous facies belts between late Courceyan and Arundian times. Tectonic uplift, of a possible southwesterly extension of the Tyrone Igneous Complex, gave rise to the deposition of Asbian to Pendleian red-beds to the south of a massif. An interface between these red-beds and contemporaneous marine sediments farther to the south is recognized and dated. A new non-marine basin, containing Brigantian and Pendleian red-beds, also developed to the north of the massif A waterlogged floodplain that developed during Westphalian A times may be coeval with more widespread coal-bearing sequences elsewhere in Ireland. Alluvial fans prograded southwards over this plain during Westphalian B times when faults bordering a northern landmass were reactivated.


2002 ◽  
Vol 90 (6) ◽  
Author(s):  
A. Choukri ◽  
J.-L. Reyss ◽  
O.K. Hakam ◽  
J. C. Plaziat

SummaryIn this work, radiochemical analysis results of 126 unrecrystallized coral samples from the Egyptian shoreline of northwestern Red Sea and 120 fossil mollusk shell samples from the Atlantic coast of Moroccan High Atlas at the North of Agadir City in Morocco are presented and discussed. The coral samples were collected in Egypt from the emerged coral reef terraces over 500 km from The Ras Gharib-Ras Shukeir depression (28°10') in the north to Wadi Lahami (north of Ras Banas, 24°10') in the south. The fossil mollusk shells were collected in Morocco from Agadir-Harbour in the south to Tamri village in the north extending over about 50 km. The statistical distributions of results (For corals,For mollusk shells, except for Holocene sea level,


2001 ◽  
Vol 172 (3) ◽  
pp. 285-293 ◽  
Author(s):  
A. K. Yelles-Chaouche ◽  
R. Ait Ouali ◽  
R. Bracene ◽  
M. E. M. Derder ◽  
H. Djellit

Abstract The Ksour mountains (northwest Algeria) belong to the western part of the Saharan Atlas. They are located between the High Plateau to the north, the South Atlas Front to the south and the Moroccan High Atlas to the west (fig. 1a). During the last decades, the Ksour mountains were the focus of several studies, mainly based on sedimentary analyses [Cornet, 1952; Bassoulet, 1973; Baiche, 1975; Ameur, 1978; Ait Ouali, 1991; Mekahli, 1995; Elmi et al., 1998]. These studies indicate that the Ksour mountains correspond to an old asymmetric rift, trending NE-SW, which underwent extension during the Triassic and Liassic [Ait Ouali, 1991; Frizon de Lamotte et al., 2000]. In order to precise the timing of the rifting processes we have analysed subsurface data (seismic lines and borehole data) from the Sonatrach Company.


Author(s):  
Valeriy Rudenko ◽  
Kateryna Grek

The creative work of Dr. Myron Korduba (1876 - 1947) is revealed in his fundamental geographical research "Territory and population of Ukraine" (1918). The article covers the well-grounded and clearly defined by scientists the boundaries of the ethnographic territory of Ukraine as a whole, as a foundation for establishing the political boundaries of the future Ukrainian state.  Only those counties (which are the primary territorial unit of assessment) where the proportion of Ukrainians exceeds 50% of the total population, or when the Ukryayans in these counties are quantitatively dominant, are the first among other nationalities, are referred to the "continuous Ukrainian ethnographic territory" by Dr. Myron Korduba. The basis for determining the boundaries of "ethnographic Ukraine" by Dr. Myron Korduba was the materials of the all-Russian 1897 population census and a similar population census in Austria-Hungary in 1900. In the ethnographic borders of Ukraine defined by scholars, almost 9/10 of the total territory accounted for "Russian Ukraine", about 8% - for "Austrian", less than 2% - for "Hungarian Ukraine". The population of Ukraine within its ethnographic borders, according to Myron Korduba, in January 1914 amounted to more than 46 million souls, of which 86% lived within Tsarist Russia, about 13% - in "Austrian Ukraine", more than 1% - in "Hungarian Ukraine. ". The ethnic composition of the population of "ethnographic Ukraine": 71.0% - Ukrainians, 11.7% - Great Russians, 8.2% - Jews, 4.5% - Poles, 1.9% - Germans, 0.9% - Volokhs, 1.8% - other nationalities. The most important result of Dr. Myron Korduba's geographical study is the definition of the northern, eastern, southern and western borders of the "continuous Ukrainian territory", the so-called "ethnographic borders of Ukraine". In the north-west, scientists outline them as follows: Brest, Kobrin, Bielsk counties of Grodno province; in the north - Pinsk and the southern part of Mozyr district of Minsk province, then - northeast of Ovruch - the northern border of Kiev province to the Dnieper - then along the Dnieper to the north of its tributary Sozh and the basin of the river Snov. The Great Russian-Ukrainian border stretched: from the upper Snov to the mouth of the Sudota River, which flows into the Desna, then - east along the administrative border between Chernihiv and Orel provinces, then - Ukrainian were Grayvoronsky, Novo-Oskolsky, Putivelsky and the southern part of Sudzhansky district of Kursk. province. In the southern part of the Voronezh province - in Biryuchensky, Bogucharsky, Valuysky, Ostrogodsky and in the south of Pavlovsky counties Ukrainians "live in continuous masses…". Then the border ran along the watershed of the Potudan and Saena rivers to the Don, and in the Don Army Region Ukrainians predominated only in Rostov and Taganrog counties. Myron Korduba referred to the Kuban region, Blagodarensky and Svyatokhrestovsky districts of Stavropol as "continuous Ukrainian territory". "Ethnographic Ukraine" in the south included Berdyansk, Melitopol and Dnieper counties of the Tavriya province, all counties of the Kherson province (except Odessa). In Austria-Hungary, the Ukrainian-Wallachian border ran west from Novoselytsia near Chernivtsi to the Suceava-Zolota Bystritsa River. In Hungary, the Ukrainian ethnographic territory included separate parts of the Maramarosky, Ugotsky, Berezky, Uzhsky, Zemplinsky, Sharyshsky, and Spysky counties. The south-western and western wedges of the Ukrainian ethnic territory were located on the right bank of the Poprad - Hrybiv - Horlytsia - Zhmyhorod - Yasolky - Ivanych - Rymaniv - north of Sanok - upper Xiang - Dinov - stream Rokytnytsia - Sinyava - mouth of Zolota - north to the Russian-Galician . Finally, in the northwest, in the newly formed Kholm province, Ukrainians constituted an absolute majority in Bielsko, Volodavsk, Hrubieszów, and Konstantinów, with an overwhelming majority in Kholm and Zamość counties. Key words: Myron Korduba, ethnographic borders and population of Ukraine.


1930 ◽  
Vol 34 (237) ◽  
pp. 747-757
Author(s):  
Fritz Stamer

The site of the Flying School was selected on a gentle eastward slope about midway between the southern slope of the “ Wasserkuppe ” and the western slope of the “ Weltensegler,” a ridge running at right angles to the former, the slopes of which are most used for training glides. The hangar, 60m. by 12m., was built of timber, with a cantilever roof requiring few supports and with drop doors at each end. The pupils are boarded at the school for convenience and for better supervision and direction of their spare time activities. It was also necessary to provide workshops and offices, and quarters for the mechanics and instructors and for the head of the school. A single building, also 60m. by 12m., adjacent to the hangar contains living quarters below, and a workshop above; a long central passage leads to a hall, on the south side, off which are the quarters of the Director of Research and of the Head of the School, and the kitchen premises; on the north side a woodworking shop equipped with a combined plane and shaping machine, a combined circular saw milling and slotting machine, and a hand saw.


Author(s):  
M. V. Fedorova ◽  
O. G. Shvets ◽  
Yu. V. Yunicheva ◽  
I. M. Medyanik ◽  
T. E. Ryabova ◽  
...  

Objective of the study was to investigate the current borders of the invasive species Ae. aegypti and Ae. albopictus distribution in the south of the Krasnodar Region and climatic factors limiting their expansion. Material and methods. Mosquito larvae, pupa and imago were collected in 21 inhabited localities in August–September, 2017, using conventional entomological methods, and identified through standard morphological keys. Climatic data found on the website pogoda. ru were analyzed using SPSS program. Results and conclusions. Ae. albopictus is widely spread along the Black Sea coast, from Adler to Novorossiysk (Ozereyevka), as well as on the north slopes of Caucasus up to Maikop. Additional investigations are required to specify the northern border of species distribution and to evidence the existence of established populations here. Ae. aegypti were not found in the south of the Krasnodar Region. The obtained data suggest a possibility of much wider spreading of dengue, Chikungunya and Zika fevers in case of pathogen importation to the south of Krasnodar Region, than was assumed earlier.


1957 ◽  
Vol 94 (6) ◽  
pp. 452-464 ◽  
Author(s):  
Kevin Burke

AbstractRemapping of parts of the Galway granite has shown that over most of its outcrop it is a homogeneous adamellite. A steeply dipping belt of basic rocks borders the intrusion on the north where there is a reaction zone between adamellite and basic rock. A similar but gently dipping belt of basic rocks overlies the granite to the west. In the south, where there is no reaction zone, the granite intrudes and hornfelses a group of pillow lavas, greywackes, and conglomerates. The structural features of the northern border indicate that the granite has been emplaced as a diapir and radial fractures in the north-east border further indicate that the granite and its basic envelope moved upward and outward together into the Connemara schists.


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