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The East Baltic accusative plural

Lingua, 1966
The traditional comparative grammars suppose that the East Baltic o-stem XC. plur. ending -us is to be derived from IndoEuropean * -6rcs which passed to *-tions and then to -zoos which in word final position was shortened to -zcs.l) Support for a posited Indo-European act. plur. ending -iins is thought to be found in the Skt. act. plur.
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Biodiversity of the Silurian osteostracans of the East Baltic

Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 2014
ABSTRACTThe sculpture and histology of osteostracan head shields and trunk squamations from the Silurian of Estonia are described, illustrated and used for the identification of disarticulated microremains collected from outcrop sections and numerous drill cores in Estonia and Latvia over the last 40 years.
T. Märss, O. Afanassieva, H. Blom
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On pseudo-suffixes in East Baltic

Journal of Baltic Studies, 1979
(1979). On pseudo-suffixes in East Baltic. Journal of Baltic Studies: Vol. 10, No. 2, pp. 148-151.
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Basic intrusives and hydrocarbonic potential of the South-East Baltic

Oceanology, 2014
The Paleozoic rocks of Kaliningrad oblast and the adjacent areas of the SE Baltic Sea have recently became exploration targets. The small size and number of prospective structures, as well as the small size of the oil reserves in the onshore areas, have resulted in a decline in production and a decrease in exploration activity.
G. S. Kharin, D. V. Eroshenko
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Palaeoproterozoic age of the East Baltic granulitic crust

Precambrian Research, 1993
Abstract The crust beneath the East European Platform is one of the largest domains of Precambrian crust in Europe. Granulites of poorly defined ages make up a substantial part of this crust. Representative samples from the granulites in southern Estonia are LREE-enriched and provide Nd T DM -model ages between 2.08 and 2.18 Ga. The equivalent ϵ Nd
V. Puura, H. Huhma
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VISIBLE MIGRATION IN THE EAST BALTIC AREA

Ibis, 1958
SUMMARYBird migration in the East Baltic area is characterised by the facts that the spring and autumn flights vary considerably in intensity; and that there are marked differences in the species represented in the southern and northern parts of the area.
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Interpreting the Meaning of East Baltic Neolithic Symbols

Cambridge Archaeological Journal, 1998
Three sets of symbolic material from sites of the East Baltic Neolithic non-Corded Ware culture c. 6500–3500 bp are presented and compared in order to interpret certain aspects of the ideology of these prehistoric communities, specifically as it relates to their faunal environment and gender distinctions.
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Telephinid trilobites from the Ordovician of the East Baltic

GFF, 1995
Abstract Telephinid trilobites are described from the Middle Ordovician (Viruan Series) in drill cores from western Latvia and the Pskov district in westernmost Russia. Three species, all assigned to Telephina Marek 1952, are discussed and illustrated: T. bicuspis (Angelin 1854) from the lowermost Uhaku Stage of western Latvia, T.
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A German ‘Heimat’ further east and in the Baltic region?

Journal of European Studies, 2006
Since the fall of the Berlin Wall, unification and the subsequent reinvention of the nation, German filmmakers have revisited their country's ‘Heimatfilm’ traditions with a view to placing themselves creatively in the context of its intellectual and artistic heritage.
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Marine Litter in the Russian Gulf of Finland and South-East Baltic: Application of Different Methods of Beach Sand Sampling

Handbook of Environmental Chemistry, 2021
Tatjana Eremina   +2 more
exaly  

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