889 resultados para India - foreign relations


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The study examined immigrants´ attitudes towards acculturation, in other words the social and cultural changes that take place in the adaptation process. The perspective of acculturation studies was also expanded by examining immigrants´ cultural values and their experiences of majority´s expectations. In addition, special interest was directed to the relations between acculturation attitudes and values and both factors´ relevance on psychological well-being. Indian born immigrants were selected as subjects as they are one of the fastest growing ethnic minorities in Finland. This minority has not been included in immigration studies previously. The seventy-five immigrants that participated as subjects represent a highly educated subgroup of Indian born immigrants. The study was carried out with posted questionnaires. Most of the subjects received an inquiry of their motivation to participate by e-mail or phone before the postal questionnaire. The results were in line with previous studies in Finland as the attitudes emphasising cultural integration were dominant. However, attitudes towards marriage, reflecting deeper and less flexible parts of culture, were dominated by separation motives. Immigrants´ perceptions of majority´s expectations reflected partly the real assimilation wishes demonstrated in previous studies. Against hypotheses, discrepancies between acculturation attitudes and experiences of majority´s expectations did not predict immigrants´ psychological well-being in a clear way. The highly educated Indian born immigrants emphasised self-direction and universalism in their values. This separates them from the traditional cultural values of India. The hypotheses made of the predictive relations between values and acculturation attitudes were partly confirmed. Also, the assumptions concerning both the stress buffering role of collectivistic values and the positive effect of achievement values on feelings of mastery were confirmed. Despite the limitations in the data, this study strengthens the view that cultural and personal values play a significant role in immigrants´ adaptation process. Information about values can benefit individuals making hard decisions and coping with cultural change as well as officials modifying Finnish immigration policy and planning the support system for immigrants.

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The region around Waclakkancheri, in the province of Kerala, India, which lies in the vicinity of Palghat-Cauvery ;hear zone (within the Precambrian crystalline terrain), has been a site of microseismic activity since 1989. Earlier studies had identified a prominent WNW-ESE structure overprinting on the E-W trending lineaments associated with Palghat-Cauvery shear zone. We have mapped this structure, located in a chamockite quarry near Desamangalam, Waclakkancheri, which we identify as a ca. 30 km-long south dipping reverse fault. This article presents the characteristics of this fault zone exposed on the exhumed crystalline basement and discusses its significance in understanding the earthquake potential of the region. This brittle deformation zone consists of fracture sets with small-scale displacement and slip planes with embedded fault gouges. The macroscopic as well as the microscopic studies of this fault zone indicate that it evolved through different episodes of faulting in the presence of fluids. The distinct zones within consolidated gouge and the cross cutting relationship of fractures indicate episodic fault activity. At least four faulting episodes can be recognized based on the sequential development of different structural elements in the fault rocks. The repeated ruptures are evident along this shear zone and the cyclic behavior of this fault consists of co-seismic ruptures alternating with inter-seismic periods, which is characterized by the sealed fractures and consolidated gouge. The fault zone shows a minimum accumulated dip/oblique slip of 2.1 m in the reverse direction with a possible characteristic slip of 52 cm (for each event). The ESR dating of fault gouge indicates that the deformation zone records a major event in the Middle Quaternary. The empirical relationships between fault length and slip show that this fault may generate events M >= 6. The above factors suggest that this fault may be characterized as potentially active. Our study offers some new pointers that can be used in other slow deforming cratonic hinterlands in exploring the discrete active faults.

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In this work an attempt has been made to evaluate the seismic hazard of South India (8.0 degrees N-20 degrees N; 72 degrees E-88 degrees E) based on the probabilistic seismic hazard analysis (PSHA). The earthquake data obtained from different sources were declustered to remove the dependent events. A total of 598 earthquakes of moment magnitude 4 and above were obtained from the study area after declustering, and were considered for further hazard analysis. The seismotectonic map of the study area was prepared by considering the faults, lineaments and the shear zones in the study area which are associated with earthquakes of magnitude 4 and above. For assessing theseismic hazard, the study area was divided into small grids of size 0.1 degrees x0.1 degrees, and the hazard parameters were calculated at the centre of each of these grid cells by considering all the seismic sources with in a radius of 300 km. Rock level peak horizontal acceleration (PHA) and spectral acceleration (SA) values at 1 corresponding to 10% and 2% probability of exceedance in 50 years have been calculated for all the grid points. The contour maps showing the spatial variation of these values are presented here. Uniform hazard response spectrum (UHRS) at rock level for 5% damping and 10% and 2% probability of exceedance in 50 years were also developed for all the grid points. The peak ground acceleration (PGA) at surface level was calculated for the entire South India for four different site classes. These values can be used to find the PGA values at any site in South India based on site class at that location. Thus, this method can be viewed as a simplified method to evaluate the PGA values at any site in the study area.