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Most of the Proterozoic carbonate formations of Peninsular India, and the so-called ‘unfossiliferous’ carbonates of the Sub- and Lesser Himalaya, contain abundant columnar and branching stromatolites. Systematic study of some of these stromatolites supports their use in biostratigraphy and reveals their Riphean—Proterozoic affinity. A synthesis of stromatolite studies in India has been attempted. A biostratigraphic correlation of the stromatolitic formations of Sub- and Lesser Himalaya extending from Jammu in the west to Buxa in the eastern Himalaya has been established. A probable correlation of those of Peninsular India has been indicated, based on available information. A bibliography on Indian stromatolites is appended. 相似文献
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Edison Dayal Dr. 《GeoJournal》1985,11(4):369-382
The main objectives of this paper are to identify and account for the regional variations in the rural household incomes and inequalities in income distribution between and within regions in India. Clearly, higher average incomes are concentrated in the W and NW regions, and very low incomes in the densely populated E and S. These differences have been analysed through the use of correlation and regression model, based on 15 variables. The results indicate that agricultural development (reflected in mechanization and irrigation), size of holdings, and family size have a positive influence on incomes, and landlessness negative. Further, a significant negative correlation between low caste population density and household incomes suggests that, at least, some of the impoverishment in the villages may be attributed to an unfair social structure that has developed and has been maintained over a long time in India. This conclusion is further reinforced by comparing income data from regions dominated by tribal social system and community ownership of land with those where Hindu caste system and private ownership of land are dominant. 相似文献
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Martin J. Haigh 《Geoforum》1984,15(4):543-561
Ravine and gully erosion affects 1% of India's land area. Zones of severe ravine trenching are found along the margins of the Gangetic Basin and in the semi-arid northwest. Ravine reclamation is currently rated as a high national priority, and India has the Third World's leading soil conservation movement. This paper reviews the technical contributions made to the study of ravine origins and genesis by government soil conservation research workers in the light of the dissident views expressed by academic geoscientists. It also reviews the soil conservation establishment's major contributions to cost-effective ravine reclamation planning. However, it is emphasised that while great advances have been made towards technological remedies for ravine erosion, relatively little has been accomplished in the realm of social science. Successful ravine reclamation requires the support and involvement of the local cultivator and local community and, probably, reform of local land tenure and social arrangements. Towards this end, much experience has been accumulated in non-government circles through the activities of Gandhian sarvodaya groups. It is recommended that their ideas and methods are integrated into ravine reclamation activities. 相似文献
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S.K. Acharyya 《Tectonophysics》1979,56(3-4)
The fit and configuration of India and Southeast Asia vis-à-vis Australia—Antarctica are critically analysed together with the evolutionary history of the Himalaya. Peninsular India, Himalaya, Tibet and Southeast Asia appear to be tied up with the development of Paleozoic-Mesozoic peripheral “Gondwanide” and Mesozoic-Cenozoic Alpine-Himalayan-Indonesian orogenic belts. Southeast Asia and Tibet are usually included within Cathaysia-Laurasia. The extent of the Tethys, separating Gondwanaland from the latter, thus appears to be much narrower than commonly believed. An alternative Gondwanaland reconstruction is proposed, placing India amidst a proto-Indian Ocean adjacent to Africa, but separated from Antarctica-Australia. 相似文献
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Holocene paleoclimates of India 总被引：4，自引：0，他引：4
We present a comprehensive summary of the available palaeoclimate records from India and compare the results from different proxies. The results indicate (i) fluctuating lake levels during the early Holocene. The period of relatively higher lake levels from increased precipitation efficiency was reached only 7.2–6.0 cal kyr BP, possibly due to increased contribution from winter rainfall; (ii) the onset of aridity in NW India could have begun as early as 5.3 cal kyr BP. Subsequently, there were multiple wet events but of shorter duration and smaller magnitude than during the mid Holocene; (iii) there is evidence of several short term climate events in the proxy record. However, in the absence of a rigorous chronological framework a detailed regional correlation is not possible at this stage. Finally, a comparison between marine and terrestrial records indicates that episodes of strongest and weakest monsoon winds were not always associated with wettest and driest episodes respectively in the NW Indian lakes. 相似文献
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The paper describes in detail the Cambrian Stratigraphy of India. On the basis of fresh fossil finds, the paleogeographic conditions during the Cambrian Period have been discussed.
Zusammenfassung Diese Arbeit beschreibt ausführlich die kambrische Stratigraphie Indiens. Anhand neuer Fossilfunde werden die paläogeographischen Bedingungen während der kambrischen Periode diskutiert.
Résumé L'article décrit en détail la stratigraphie du Cambrien de l'Inde. Partant de nouvelles découvertes de fossiles, les auteurs discutent les conditions paléogégraphiques au cours de la période cambrienne.
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In this paper, flood problems in India, regional variabilityof the problem, present status of the ongoing management measures, their effectiveness and futureneeds in flood management are covered. Flood problems in India are presented by four zonesof flooding, viz. (a) Brahmaputra River Basin, (b) Ganga River Basin, (c) North-WestRivers Basin, and (d) Central India and Deccan Rivers Basin. Some special problems,related to floods like dam break flow, and water logging in Tal areas, are also mentioned.Progress of various flood management measures, both structural and non-structural, arediscussed. In addition, future needs to achieve efficient and successful flood managementmeasures in India are also pointed out. 相似文献
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Two magnetometer array experiments were conducted in India during 1978–1980, under an Indo-Australian collaboration project, using 21 Australian three-component magnetometers of the Gough-Reitzel type. The first array study was made in the northwestern region covering the Aravallis, the Punjab, and the lesser Himalaya, while the second experiment was carried out in the southern peninsular shield area. Both these sets of geomagnetic deep sounding (GDS) observations yielded valuable results on the crustal and upper mantle structure in the two geologically and geophysically important regions of India.Geomagnetic induction patterns observed in northwest India have revealed a variety of electrical conductivity structures. The primary conductivity structure providing paths for induced currents is found to be striking at right-angles to the Himalayan Mountains. The conductivity structure is indicated to be a northward continuation of the Aravalli belt and, thus, suggesting the continuation of the Indian shield at depth into the base of the Himalayan foothills under the Ganga basin.The induction effects observed in the southern tip of peninsular India are by far the most complex geophysical phenomenon due to the simultaneous occurrence of the sea coast, the crustal and upper mantle conductivity anomalies between India and Sri Lanka under the sea, and the day-time equatorial electrojet as part of the external heterogeneous inducing field. It is further complicated by the existence of a conductive step, structure along the coastline at the Moho boundary and a “graben” structure in the Palk Strait, as revealed by the array observations. 相似文献
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The tectonic map of India and contiguous areas 总被引：1，自引：0，他引：1
T. S. Balakrishnan P. Unnikrishnan A. V. S. Murty 《Journal of the Geological Society of India》2009,74(2):158-168
The existing tectonic maps of India produced by the GSI and ONGC are largely based on the geological map of India combined
with the topographic maps and the lineations evident in satellite pictures of the earth’s surface. Broadly speaking, these
consider only features observed on the surface of the earth. The third dimension is not much in evidence.
The introduction of 3D-geophysical data into these maps ensured a substantial advance in the study of the crustal structure
at depth. The new tectonic map is the result of this integration. 相似文献
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The present study is mainly concerned with detecting the trend of run-off over the mainland of India, during a time period of 35 years, from 1971–2005 (May–October). Rainfall, soil texture, land cover types, slope, etc., were processed and run-off modelling was done using the Natural Resources Conservation Service (NRCS) model with modifications and cell size of 5×5 km. The slope and antecedent moisture corrections were incorporated in the existing model. Trend analysis of estimated run-off was done by taking into account different analysis windows such as cell, medium and major river basins, meteorological sub-divisions and elevation zones across India. It was estimated that out of the average 1012.5 mm of rainfall over India (considering the study period of 35 years), 33.8% got converted to surface run-off. An exponential model was developed between the rainfall and the run-off that predicted the run-off with an R2 of 0.97 and RMSE of 8.31 mm. The run-off trend analysed using the Mann–Kendall test revealed that a significant pattern exists in 22 medium, two major river basins and three meteorological sub-divisions, while there was no evidence of a statistically significant trend in the elevation zones. Among the medium river basins, the highest positive rate of change in the run-off was observed in the Kameng basin (13.6 mm/yr), while the highest negative trend was observed in the Tista upstream basin (?21.4 mm/yr). Changes in run-off provide valuable information for understanding the region’s sensitivity to climatic variability. 相似文献
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Indu Jain P. Chittibabu Neetu Agnihotri S. K. Dube P. C. Sinha A. D. Rao 《Natural Hazards》2007,42(1):67-73
The northeastern sector of the Arabian Sea, which covers the Gujarat coast of India and western coast of Pakistan, is a region
vulnerable to extreme sea levels associated with tropical cyclones (TCs). Although the frequency of tropical cyclones in the
Arabian Sea is not high, the coastal regions of India and Pakistan suffer in terms of loss of life and property caused by
the surges. In view of this a location-specific fine resolution model is developed for the Gujarat coast of India and adjoining
Pakistan coast. The east–west and north–south grid distance is about 3.0 km. Using this model, numerical experiments are carried
out to simulate the surges generated by 1999 and 2001 cyclones which struck the Pakistan coast. The model computed surges
are in agreement with the available observational estimates. 相似文献
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Proterozoic terrains in South India and Madagascar provide important clues in understanding the Gondwanaland tectonics, especially the assembly of this mega-continent during the Pan-African period. The Archaean terrains in both Madagascar and India are characterized by N-S trending greenstone belts occurring within gneissose granitic rocks in the northern part. Extensive development of K-rich granitic rocks of ca. 2.5 Ga is also characteristic in both areas. Such a broad age zonation of younger Dharwar (ca 2.6–3.0 Ga) in the north and the older Sargur (ca 3.0–3.4 Ga) in the south as in South India remains to be identified in future studies from Madagascar. The occurrence of greenschist facies rocks in the northeastern part and higher grade rocks in most of other parts in the north-central terrain of Madagascar is comparable with the general tendency of increasing metamorphic grade from northwestern to southern areas ranging from greenschist to granulite facies in South India. The Proterozoic crystalline rocks in both continents show pronounced lithological similarity with the wide occurrence of graphite-bearing khondalite in association with charnockitic rocks. While the Archaean-Proterozoic boundary is well defined in southern India by the Palghat-Cauvery or the KKPT shear zones as recently identified, this boundary is ill-defined in Madagascar due to extensive Pan-African overprinting, as well as the development of the Proterozoic cover sequence, the Itremo Group. There is also a possible general correlation between the Mesoproterozoic cover sequences in Madagascar and India, such as between the Itremo Group of west-central Madagascar and the Kaladgi and Cuddapah sequences of South India. The Pan-African granulite facies metamorphism of ca. 0.5 Ga extensively developed in both India and Madagascar is generally comparable in intensity and extent. P-T conditions and P-T-t paths also appear comparable, with the general range of ca. 700–1000°C and 6–9 kb, and near-isothermal decompressional paths. A-type granite plutons and alkaline rocks including anorthosites and mafic plutonic rocks of ca. 500–800 Ma develop in both terrains, provide strong basis for the correlation of both terrains, and define a Pan-African igneous province within East Gondwanaland. Major shear zones in both continents are expected to play a critical role in the correlation, albeit are still poorly constrained. Detailed elucidation of the tectonic history of the shear zones, and the timing of various events along the shear zones would provide important constraints on the correlation of the two continental fragments. 相似文献
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K K Nagpaul 《Journal of Earth System Science》1981,90(3):389-401
The fission track ages of cogenetic/co-existing minerals namely garnet, muscovite and apatite from three mica beltsi.e., Bihar, Rajasthan, Nellore of peninsular India and Himalayan region, coupled with the corresponding closing temperatures of the minerals have been used to reveal the thermal and uplift histories of these regions. The data show that the extra-peninsular part of the subcontinent during Himalayan orogenic cycle (upper cretaceous-tertiary) witnessed the highest cooling and uplift rates in comparison to the older cycles in peninsular India. 相似文献