Norway, NATO, and the Northern flank 1

Author(s):  
Karsten Friis
Keyword(s):  
Icarus ◽  
2007 ◽  
Vol 192 (2) ◽  
pp. 361-377 ◽  
Author(s):  
Giancarlo Bellucci ◽  
Joern Helbert ◽  
Francesca Altieri ◽  
Dennis Reiss ◽  
Jean-Pierre Bibring ◽  
...  
Keyword(s):  

2021 ◽  
Vol 126 (4) ◽  
pp. 401-420
Author(s):  
Bertrand Launay ◽  
Julien Barnasson ◽  
Juliette Becquet ◽  
Michel Brulin ◽  
Sophie Cauvy-Fraunie ◽  
...  

Discovery of a new population of Rhithrogena delphinensis Sowa & Degrange, 1987, in the Arves Massif, and additions to the morphological description of the larva (Ephemeroptera, Heptageniidae). Rhithrogena delphinensis, described originally on the basis of four larvae from the Western Alps, south of the Arves Massif and from the northern flank of the Ecrins Massif, had not been captured again since 1986. Here, we report the discovery of a new population from river Arvan, whose drainage basin is located between the Grandes Rousses Massif and the northern flank of the Arves Massif. This newly discovered population seems abundant in numbers, and reveals the particular ecological requirements of the species as well as its dependence on glacier fed or nival streams. The morphological characteristics of the larvae are described in detail, and illustrated by photographs. The variability of some of the proposed identification criteria is discussed, and a key to the identification of the Rhithrogena species from the alpestris group of the Western Alps, to which R. delphinensis belongs, is provided. Finally, a portion of 658 base pairs of the COI gene of R. delphinensis is sequenced for the first time and compared to already existing data on the alpestris group in the Western Alps.


2017 ◽  
Vol 476 (1) ◽  
pp. 1021-1025
Author(s):  
D. P. Gladkochub ◽  
T. V. Donskaya ◽  
M. Cho ◽  
V. S. Fedorovsky ◽  
A. M. Mazukabzov ◽  
...  
Keyword(s):  

1984 ◽  
Vol 27 (3) ◽  
pp. 697-713 ◽  
Author(s):  
A. B. Gaunson

After the fall of France in 1940, Britain's predicament in the Middle East became worse still when the French authorities in Syria and Lebanon aligned themselves with the new Vichy government. The British, already outnumbered by Italian forces and uncertain of Arab loyalties, now found their northern flank controlled by men susceptible to Axis pressure. Both Churchill and de Gaulle responded with the determination that the Levant should be denied to the Axis and placed in friendly hands. Despite this common resolve, however, fundamental differences emerged during the Anglo-Free French invasion of Syria in 1941. This hastily improvised venture was marred by rash political tactics, poor liaison, bad diplomacy and the interventions of Churchill and de Gaulle. Although the Syrian flank was secured, this affair did serious damage to Anglo-Free French relations, created new problems in the Levant, and precipitated personal antagonism between Churchill and de Gaulle.


1973 ◽  
Vol 10 (8) ◽  
pp. 1350-1353 ◽  
Author(s):  
L. Imreh

The pre-Kenoran Archean stratigraphy has always been of prime interest to geologists working in the Superior Province. However, one must realize that the problems raised have remained, for the most part, without satisfactory solution. Thus, the respective age relation of the thick lithostratigraphic metavolcanic and metasedimentary units (Pontiac), forming respectively the Baby Rift and its northern flank to the northeast of Ville-Marie in Temiscaming, has not been defined with certainty to date.During a geological mapping project on a scale of 1:12 000, covering the township of Baby and adjacent parts of the townships of Guérin and Guigues, it has become possible for us to remove the uncertainty and to define the age relation of the two units mentioned. We can now state that the metasedimentary unit (Pontiac) forms the stratigraphic base of the metavolcanic unit.To arrive at this conclusion it was first necessary to determine the size of the main folded structures in the region of Rapide des Quinze, then to uncover and let weather the outcrops over several kilometers, in order to define the actual contact of the two units. [Translated by the Journal]


2021 ◽  
Author(s):  
Vincent Wicker ◽  
Mary Ford

<p>Detailed structural and stratigraphic field mapping is used to reconstruct the Jurassic to Late Cretaceous diapiric and tectonic evolution of the Toulon Fault Zone, eastern Beausset Syncline and Toulon Belt, southern France, which represents the easternmost vestige of the Pyrenean orogen in Provence. This complex salt-rich area records a complete history from Jurassic-early Cretaceous subsidence and Aptian-Albian oblique rifting to Late Cretaceous Pyrenean-Provençal shortening. Halokinetic sequences and geometries were preserved principally on the northern flank of the Mont Caume salt diapir sourced from the Upper Triassic Keuper unit. Our field observations are best explained by a model where halokinetic activity interacted with regional deviatoric stresses from early-Jurassic to Santonian/Campanian times. Halokinetic wedges of Jurassic and Early Cretaceous carbonates thin toward the diapir, recording early salt mobilisation. Inverted relics of Apto-Albian rift depocenters are aligned along the northern margin of the Toulon Belt and the adjacent Bandol belt that lies to the west.  The Turonian-Coniacian Revest depocenter developed due to localized strong asymmetrical growth of the Mont Caume diapir. The three-dimensional form and growth of the diapir controlled lateral migration of the Revest depocenter, thickness variations, progressive unconformities, and the westward increase in stratal overturning of a flap. A component of N-S compression with related accelerated halokinetic activity can explain our observations and can be considered as the earliest expression of N-S convergence in the Provencal fold belt.  Further west, the overturned Beausset klippe can be interpreted as the remnant of a megaflap on the northern flank of the Bandol diapir. The Toulon belt salt structures are excellent field analogues to others observed in the external Alps and Pyrenees.</p>


1947 ◽  
Vol S5-XVII (4-6) ◽  
pp. 293-299
Author(s):  
Maurice Dreyfuss ◽  
M. Gottis

Abstract Pre-Lutetian (probably early Eocene for the most part) and pre-Oligocene crustal movements caused the formation and folding of the Saint-Martin de Londres lacustrine basin at the foot of the north slope of the Pic Saint-Loup anticline, Herault, France. Post-Oligocene dislocations caused thrusting and overturning of Jurassic strata of the northern flank of the anticline.


1963 ◽  
Vol S7-V (5) ◽  
pp. 844-851 ◽  
Author(s):  
Jean Nicolas ◽  
Jean Paul Sagon

Abstract Observations on the dolerites of the northern flank of the E-W-trending Laniscat-Merleac anticline in NW France suggest that the rocks were emplaced as coulees. A well-marked granular differentiation in the rock supports this hypothesis; the coarse-grained rocks are in contact with Devonian rocks at the bottom of the coulee and the fine-grained rocks are in contact with Dinantian rocks at the top. Chemical analysis shows that there is a diminishing of Na <sub>2</sub> O and an augmentation of the percentage of CaO ranging from the boundary of the coarse-grained rock to that of the fine-grained. Overlying the green rocks are green schists of comparable chemical composition attributed to former tuffs which were subject to regional epimetamorphism. Finally, a coarse-grained, green rock sample has been traced to the spilite family.


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