scholarly journals Congruences of Local Origin and Automorphic Induction

Author(s):  
Neil Dummigan ◽  
David Spencer
1997 ◽  
pp. 20-32
Author(s):  
Valeriy Grynko

Complex processes that accompany the formation and development of Ukrainian statehood have created favorable conditions for the spread of neo-religious churches, currents and trends. Most of them are mentally rooted, are spread predominantly owing to the activity of foreign missionaries. Therefore, given the local origin and social resonance, the Great White Brotherhood's phenomenon, whose propagation of faith was carried out and had some success in most of the post-Soviet countries, needs special attention.


1925 ◽  
Vol 15 (3) ◽  
pp. 257-271 ◽  
Author(s):  
James Hendrick ◽  
George Newlands

1. Previous investigations showed that certain Scottish soils were of glacial drift origin, that they were comparatively rich in unweathered silicates and therefore in reserves of plant-food, that they showed considerable variation in such silicates and were capable of classification accordingly. Some indication was also shown that the glacial drift, and hence the resulting soil, was sometimes of local origin, its character being determined by the underlying rock. In the present investigation a more extensive survey of Scottish soils has been made in order to discover to what extent these preliminary findings might be applicable generally.2. For this purpose soils have been collected from various localities in the north, north-east, west and south of Scotland, and have been analysed mechanically and the “fine sand” fraction examined mineralogically.


2010 ◽  
Vol 16 (3) ◽  
Author(s):  
N. Papp ◽  
J. Nyéki ◽  
Z. Szabó ◽  
É. Stefanovits-Bányai ◽  
T. Szabó ◽  
...  

Sour cherry (Prunus cerasus L.) cultivars grown in Hungary are of local origin while most sweet cherry cultivars in Hungary are introduced from other countries.A great phenotypic variability is displayed by both species. In the present study, we analyzed 10 sour and 9 sweet cherry cultivars for their antioxidant capacity, total polyphenolics (TPC) and total anthocyanin (TMAC) contents. In general, sour cherries showed higher levels of antioxidant capacity, TPC and TMAC. The anthocyanin contents varied from 0.16 to 6.85 and 1.41 to 127.56 mg/100 g for sweet and sour cherries, respectively. However, TMAC generally seems to have a limited influence on the antioxidant capacity of cherries.An amarelletype sour cherry, ‘Pipacs 1’ showed the highest antioxidant capacity (21.21mmolAA/l) and TPC (44.07mgGA/l) in contrast to its lowanthocyanin content. The detected diversity presents a choice that can satisfy different consumer preferences, and meet specific nutritional requirements.


Author(s):  
Владимир И. Кулаков

The catalogue of copies from the Roman-German Central Museum (Mainz) poses an opportunity to present to the modern researcher the volume of Prussian archaeological material available on the second floor dedicated to the 19th century. By collecting what is considered the most representative exhibits, the museum authorities put on display items copied in Mainz and stored in Prussia-Museum (Königsberg). They were created by masters from Aesti and Prussia. The only imports among the small array of findings published in the catalogue include a helmet from the Dollkeim-Kovrovo burial ground (its local origin has not been excluded) and a lock and key from the Löbertshof cemetery / Tyulenino.


Author(s):  
G. A. Eiby

The manner in which an earthquake produces a tsunami , or seismic sea-wave , is not well understood. In Japan and in Chile they accompany most large shallow submarine earthquakes close to the coast, while in New Zealand and much of the South West Pacific tsunamis of local origin have been of comparatively rare occurrence, and are usually small. Nevertheless, both tsunamis and seiches (resonant oscillations of enclosed bodies of water) constitute an appreciable component of our earthquake risk.


1998 ◽  
Vol 88 (5) ◽  
pp. 1198-1203
Author(s):  
Ronald Doig

Abstract The 1988, magnitude mb 5.9 (mbLg 6.5) Saguenay, Quebec, earthquake occurred in a region considered to be aseismic, but the epicenter was less than 100 km northwest of the seismically active region of Charlevoix. Lake sediment cores representing some 3000 yr of sediment accumulation contain abnormal silt layers attributed to seismic shaking events prior to the 1988 earthquake. The layers are formed by the relatively rapid settling of the silt portion of the seismically resuspended organic-rich sediment. Cores were obtained over a distance of 120 km, perpendicular to the Saguenay graben structure. Several silt layers are much thicker and more widely distributed than the effect of the 1988 earthquake and are comparable to those observed at Charlevoix that were produced by magnitude 6 to 7 events. The silting events do not correlate between the sampled lakes nor does the pattern match that at Charlevoix, so that the shaking events are interpreted to be of local origin. The recurrence interval for magnitude ≧6 earthquakes ranges from 350 to 1000 yr, in contrast to the roughly 75-yr historical recurrence of earthquakes of magnitude greater than 6 at Charlevoix.


1957 ◽  
Vol S6-VII (7) ◽  
pp. 949-963
Author(s):  
Philibert Russo

Abstract Ground-water aquifers in the southwestern part of the Dombes plateau, France, consist of lenses in Tortonian or Pontian deposits of the Molasse (Tertiary) sequences where they occur between the impermeable crystalline basement and an overlying impermeable layer of Pleistocene glacial clays. The aquifers are dome-shaped masses whose orientation differs, in part, from the general southeast dip of the basement. Ground waters of the Croix-Rousse hill, at Lyons, seem to be of purely local origin.


1984 ◽  
Vol 81 ◽  
pp. 204-210
Author(s):  
George W. Clark

Comparison of the SAS-3 soft X-ray sky survey (F. Marshall and G. Clark 1984) with the 21-cm neutral hydrogen survey of Stark et al. (1984) confirms the well-known anticorrelation between the counting rates in the C-band (0.10-0.28 keV) and the column density of neutral hydrogen, and demonstrates that this anticorrelation is significant on all angular scales ranging from that of the general trend from the galactic equator to the poles down to the angular resolution of the detector (2°.7 FWHM). Included in this general anticorrelation are numerous instances of what appear to be soft X-ray “shadows” of nearby (100-300 pc) 21-cm features, and several bright X-ray regions coincident with “holes” in the ISM.


Astrophysics ◽  
1989 ◽  
Vol 29 (3) ◽  
pp. 758-762
Author(s):  
G. S. Martirosyan
Keyword(s):  

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