scholarly journals Leksykalne wykładniki hipotetyczności w litewskiej gwarze puńskiej z odniesieniami do języków polskiego i litewskiego

2015 ◽  
Vol 35 ◽  
pp. 159-170
Author(s):  
Danuta Roszko
Keyword(s):  
Research Area ◽  
North East ◽  
The North ◽  
Local Dialect ◽  
Definition Of ◽  
Tertium Comparationis

Lexical indicators of the hypothetical modality in the Lithuanian local dialect of Puńsk with references to Polish and Lithuanian.The dissertation discusses the problem of lexical indicators of the hypothetical modality in the Lithuanian local dialect of Puńsk. The Lithuanian local dialect of Puńsk is used by the Lithuanians living in the north-east regions of Poland. In these very regions there run important ethnic borders between Slavs and Balts, and between the Eastern and the Western groups of Slavs. The author has applied the method of theoretical contrastive studies to characterize the local dialect of Puńsk. To begin with, the author forms the definition of the hypothetical modality along with its paraphrase. She analyzes the gradation of the hypothetical modality phenomenon. Therefore, she has distinguished 6 groups, each of which is characterized by a different degree of probability. Furthermore, she gives examples of all possible indicators of the hypothetical modality in the local dialect: lexical, morphological and syntactic, where lexical indicators are more precisely described. She has distinguished the differences and resemblances between the local dialect and the literary languages of Lithuanian and Polish. In the research area, she applies the experimental corpus of the local dialect of Puńsk. Лексические средства гипотетичности в литовском говоре окрестностей Пунска в сопоставлении с польским и литовским языкамиВ статье описывается проблема лексических показателей гипотетической модальности в литовском говоре окрес тностей Пунска. На литовском говоре окрестностей Пунска говорят литовцы проживающие на северо-востоке Польши. Именно там, на этой территории, многие столетия пересекаются этнические границы между славянами и балтами, между западными и восточными славянами. В статье используется метод теоретического сопоставления естественных языков с использованием так называемого языка-посредника (tertium comparationis). В самом начале представлено содержание категории гипотетической модальности и ее парафраза. Затем описывается изменение по степеням возможности и в связи с тем выделяются шесть групп, которые постепенно отражают повышение возможности, уверенности говорящего к высказываемому им самим содержанию. В описании гипотетической модальности упоминаются лексические, морфологические и синтаксические средства выражения гипотетических значений. Более точно описываются лексические средства. Обращается внимание на сходства и различия между говором и польским и литовским языками. В исследованиях используются данные экспериментального корпуса говора окрестностей Пунска.

scholarly journals Analysis of the data of hydrogeochemical monitoring of groundwater in the North Sivash artesian basin

2019 ◽  
pp. 64-71
Author(s):  
K. Ya. Bulakhova ◽  
S. M. Sudarikov
Keyword(s):  
Research Area ◽  
Geological Structure ◽  
Hydrogeological Model ◽  
Artesian Basin ◽  
Correlation And Regression Analysis ◽  
The North ◽  
Gypsum Content ◽  
Definition Of ◽  
Aquifer Complex ◽  
Made In

The results of hydrogeochemical monitoring of the Sarmat-Meotis-Pontic sediments aquifer complex of the North Sivash artesian basin have been analyzed. The analysis based on a routine observations for 16 producing wells. The observations were made in the period from 2014 to 2017 years. A correlation and regression analysis has been made for definition of dependencies between changes in the concentrations of the normalized components. The results obtained allow us to evaluate the main factors of formation of the chemical composition of groundwater. At the present stage, metamorphosed waters are pulled up from the lower strata of the complex, that leads to an increase in the amount of mineralization. The formation of sulphate waters is primarily associated with the peculiarities of the geological structure, namely, the high gypsum content of quaternary deposits and the presence of hydraulic connection with the overlying aquifers. One of the reasons for the formation of sulphate waters is the anthropogenic impact associated with the close location of the acid accumulator containing sulfur tailing. The results obtained allow us to proceed to the next stage of the survey — the creation of a natural hydrogeological model of the research area and the carrying of the thermodynamic modeling.

scholarly journals Facies Development of Carbonate Rock and System Tract Influence Based on Fullbore Formation Microimager (FMI) and Well Log Analysis on Carbonate Reservoir Tuban Formation, North East Java Basin

2018 ◽  
Vol 73 ◽  
pp. 02021
Author(s):  
Fahrudin ◽  
Eka Sainyakit ◽  
Ahmad Syauqi Hidayatillah ◽  
Purnaning Tuwuh Triwigati ◽  
Muhajir
Keyword(s):  
Carbonate Rocks ◽  
Carbonate Rock ◽  
Gamma Ray ◽  
Research Area ◽  
Carbonate Reservoir ◽  
Log Analysis ◽  
Reef Facies ◽  
North East ◽  
The North ◽  
System Tract

The North East Java Basin is known to be one of the basins that consist of Miocene carbonate rocks, like the reef carbonate of Tuban Formation. It has the potential hydrocarbons that can be explored. Therefore, the FMI log analysis is very important to identify carbonate rocks of Tuban Formation to know facies and characteristics of that carbonate rocks. The method used descriptive and analysis process of FMI and Gamma Ray log to determine facies of the carbonate rock and the system tract. Based on the result of FMI log analysis, there are variations lithofasies include mudstone, wackestone, packstone, grainstone, floatstone, rudstone and claystone. A collection of rock associations can interpret the reef facies. It involves back reef facies, reef core facies, and fore reef facies. The changes of lithofasies and reef facies are caused by sea level fluctuations and subsidence resulting in the system tract. The system tracts generated in the research area include transgressive and highstand system tract.

The Context and Definition of Upper Palaeolithic Industries in Panchpir, Orissa, India

2000 ◽  
Vol 66 ◽  
pp. 47-59
Author(s):  
Asok Datta
Keyword(s):  
Upper Palaeolithic ◽  
North East ◽  
The North ◽  
History Of ◽  
Definition Of

This paper provides a brief outline of the history of Palaeolithic research in India as a background to the description of the distinctive Upper Palaeolithic industries that have now been identified. The assemblages from three sites in Orissa are described to illustrate the character of the industry in the north-east of the subcontinent.

Rembang Zone Petroleum Play, Stratigraphic and Petrographic Analysis of Ngrayong Formation as Reservoir, Jamprong Area, Tuban, East Java

2020 ◽  
Author(s):  
D., S. Reka
Keyword(s):  
Depositional Environment ◽  
Carbonate Platform ◽  
Research Area ◽  
Geological Mapping ◽  
Coarse Grained ◽  
Petrographic Analysis ◽  
North East ◽  
The North ◽  
Potential Reservoir ◽  
Sandstone Facies

The following research took place in the Jamprong area, Tuban Regency, East Java Province within a study area of 2 km2. Physiographically, the study area is situated in the anticlinorium of the Rembang Zone. This research aims to define the reservoir potential of outcrop samples from the Ngrayong Formation as an analogue for the subsurface. In addition, the depositional environment and the age of the rock in the research area was determined. The Ngrayong Formation is regarded as a potential reservoir in the North East Java Basin. The accumulated data consists of stratigraphy, petrographic analysisand paleontological analysis of rock samples, and geological mapping has been carried out to determine the distribution of rocks. Facies were determined based on outcrop observations and comprise predominantly arkose sandstone facies with fine – coarse grained, moderately sorted and with cross-bedding, herringbone, and lamination, and another facies namely massive carbonate grainstone. Based on these facies, the interpreted depositional environment is the transition of tidal flat to shallow marine carbonate platform with relative biostratigraphic age of Middle Miocene, Langhian to Serravallian (M6-M8 planktonic foraminiferal biozones). Rocks in the study area have porosity >20% or very good and permeability >130 or fair based on petrographic observations, and this supports the interpretation of the Ngrayong Formations as a potential reservoir of hydrocarbons.

Sustainability Assessment Method of GRIHA for Sustainable Built Environment: A Review Based on a Design Perspective

2016 ◽  
Vol 4 (2) ◽  
pp. 156-164
Author(s):  
Shiva Ji ◽  
◽  
Ravi Mokashi Punekar ◽  
Keyword(s):  
Built Environment ◽  
Sustainability Assessment ◽  
Well Being ◽  
Assessment Method ◽  
Local Conditions ◽  
North East ◽  
The North ◽  
World Energy ◽  
Design Perspective ◽  
Definition Of

Building industry is the largest world energy consumer at 40% of total world energy. Various agencies across the world have formulated Sustainability Assessment (SA) methods for its assessment. In India, TERI and Ministry of New and Renewable Energy, Govt. of India, have established GRIHA as the assessment guideline for the built environment. SA methods recommend a pre-design check list and post completion assessment of the projects. The major parameters of evaluation aim to address environmental, social and economic impact on well- being of society. A comparison is drawn on the broader definition of sustainability which has been adopted world over and it is felt by local practitioners that the parameters need to be adapted to deal with local situations and conditions for effective results. This paper attempts to review the various assessment parameters considered under the GRIHA model in the design evaluation of the built environment considering local conditions in specific locations in the north east. The paper infers to devise a normalization factor to help achieve equalized balance in achieving sustainability.

scholarly journals The silica road: Field trip notes

2016 ◽  
Vol 3 (2) ◽  
Author(s):  
María Soto ◽  
Bruno Gómez de Soler
Keyword(s):  
Raw Materials ◽  
Field Trip ◽  
Middle Palaeolithic ◽  
Stratigraphic Sequence ◽  
Depositional Sequence ◽  
North East ◽  
The North ◽  
10Th International Symposium ◽  
Abric Romaní ◽  
Definition Of

During the 10th International Symposium on Knappable Materials (ISKM) held at Barcelona (Spain) in 2015, a field trip along “The Silica Road” was organized. It included the visit to different chert outcrops located along the Montsant Massif (Tarragona, NE Iberian Peninsula), and to the Middle Palaeolithic site of the Abric Romaní (Capellades, Barcelona), as important locations for the Prehistory of the North East of the Iberian Peninsula.This paper present some keynotes distributed to the symposium attendants. It consists on: 1) a brief geological framework of the Montsant Massif, located at the southern margin of the Catalan Central Depression. It includes the definition of their Palaeozoic to Cenozoic depositional sequence and the localization of some points of interests with panoramic views and source areas where Tertiary chert nodules were available. They represent a significant focus for the raw materials procurement of several Paleolithic occupations since Lower Pleistocene. 2) A general presentation of the Middle Palaeolithic site of the Abric Romaní site, including a brief reference of the three research phases initiated at the beginning of 20th Century, the description of its 50 meters stratigraphic sequence, where 27 archaeological levels have been identified dating since 110 to 39 ka BP, and some of the main traits of the archaeological assemblages recovered.

scholarly journals COMPETITIVENESS FACTORS IN THE INNOVATIVE ENTERPRISES IN THE NORTH-EAST VOIVODESHIPS IN POLAND

2020 ◽  
Vol 21 (2) ◽  
pp. 503-518
Author(s):  
Kamil Decyk
Keyword(s):  
Action Plan ◽  
Research Problem ◽  
Research Area ◽  
Chi Square ◽  
Research Hypothesis ◽  
North East ◽  
The North ◽  
Knowledge Based Economy ◽  
Measure Of Association

The research problem was the connection about the problematics of competitiveness factors with the planned action of innovation within the managing of the enterprise. In such research area the purpose of the study was to identify and evaluate the competitiveness factors used in innovative companies while taking into consideration companies’ ownership of long-term plan of action connected with managing the innovations. To achieve this objective, the following research methods were used: analysis of national and foreign literature resources, survey measurement (observation technique), direct and indirect interview, research tool: questionnaire. The results were analysed with statistical methods such as arithmetic mean, test of Kruskal-Wallis, Chi-square test (χ2), and measure of association including Cramér’s V coefficient were applied. Based on research results and mentioned statistical tools, it was stated that having of long-term plan of action connected with innovations statistical significant affected on the evaluated competitiveness factors (innovativeness, quality, marketing and logistics activities) except the price. It was confirmed in such wat the first research hypothesis. The research also showed a relationship between competing using innovativeness and having an action plan related to innovations, however, this relationship was not statistically significant. As a result, the research hypothesis can be neither rejected nor confirmed. In practical terms, the conducted research points out the competitiveness factors which are suggested to use by the innovative enterprises in order to improve their competitiveness against competitiveness and in surroundings of knowledge based economy, as well the digital economy. Results of the research indicate at the same time, the necessity of development of long-term plan of action connected with innovations, which provides bigger possibilities in range of usage of competitiveness instruments on the market by enterprises.

Analyses of Awareness, Perception and Attitude towards Embedded Librarianship among Librarians in North-Eastern Universities, Nigeria

2019 ◽  
Vol 9 (3) ◽  
pp. 37-43
Author(s):  
Augustine Uzoma Madu ◽  
Emmanuel M. K. Dawha
Keyword(s):  
Current Trend ◽  
Research Area ◽  
Academic Librarians ◽  
Library Services ◽  
University Libraries ◽  
North East ◽  
The North ◽  
North Eastern ◽  
New Research ◽  
High Level

Innovations in library services and need for professional development among librarians with growth in research have brought to bear on the concept of embedded librarianship as a new research area in librarianship. It is expected that librarians in Nigeria must do all to move with the current trend in the discipline. This study aims to under the roles of awareness, attitude and perception of academic librarians in North-east Nigeria towards embedded librarianship practice. A survey of 11 university libraries in the region was undertaken with 356 conveniently selected samples. The descriptive result indicates a high level of awareness while attitude and perception recorded significant agreement to answer the research questions. The null hypothesis of non-significant effect of awareness, perception and attitude on embedded librarianship among academic librarians in university libraries in the north-east, Nigeria was rejected at F(3: 352) =2376.807, P<.0005, R2 =.953 and was replaced with the alternate hypothesis. The study concludes that academic librarians in the study area have a high awareness level, positive attitude and perception about embedded librarianship. However, the actual practice of the term is still low from the practical assessment.

The Parisian Basin

2005 ◽  
Author(s):  
Yvette Dewolf ◽  
Charles Pomerol
Keyword(s):  
Sedimentary Basins ◽  
Geological Time ◽  
Geological Time Scale ◽  
Massif Central ◽  
North East ◽  
The North ◽  
Geological Map ◽  
Intracratonic Basin ◽  
Definition Of ◽  
Armorican Massif

The Parisian basin is a geographical entity whose limits are easily defined by the Armorican massif, the Massif Central, the Vosges, the Ardennes, and the English Channel. Both Burgundy and Poitou are transitional areas. The Paris basin, a more restrictive term, corresponds according to some geologists (Cavelier and Lorenz 1987) essentially to the Tertiary ‘part’ of the basin: the Île de France and surroundings. The relief of the Parisian basin results from two sets of factors: tectonic and climatic. These have operated from Triassic times until the Pleistocene and have led to the development of a geographically simple whole in its gross structure and form. However, within this framework individual natural regions (or geotypes) may be recognized. The Parisian basin is frequently considered as a model for sedimentary basins, displaying as it does, a classic framework of sedimentary formations (Pomerol 1978; Cavelier and Pomerol 1979; Cavelier et al. 1979; Pomerol and Feugueur 1986; Debrand-Passard 1995). This is evident from the geological map of France, and on the related cross-section. Indeed, the section shows the superposition of strata in a subsiding area, with a maximal thickness (3,200 m) in the Brie country. This arrangement illustrates the geometric definition of the Parisian basin, an intracratonic basin, 600 km in diameter, limited towards the west by the Armorican massif, the south by the Massif Central, the east by the Vosges, and the north-east by the Ardenno-Rhenan massif. The following geological overview is based upon the previously mentioned studies and the geological time scale. However, the analysis of the evolution of these sedimentary areas from Triassic to Neogene shows that the area named as the ‘Parisian basin’ was included in successive palaeogeographies (which were strongly influenced by adjacent seas) and overflowed across the basement regions that now act as the limits of the basin. The chronological order of the geological formations involved in the evolution of the Parisian basin according to Robin et al. (2000) is used in the following text. During the Triassic, the future Parisian basin was a gulf of the German Sea. This sea transgressed westwards and reached the meridian of Paris during the Keuper.

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