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121.
North-eastern Himalaya is said to be one of the world most complex geological set-up with different kinds of seismotectonic systems. Region has experienced two of the world’s strongest earthquakes, such as Shillong earthquake of 1897 known as Assam earthquake and subsequent 1950 earthquake in Arunachal Pradesh, both of with magnitude of 8.7, and also several other strong earthquakes. Various techniques have been applied to understand the past strong earthquake mechanism as well as hazard estimation carried out for future earthquake. Fractal correlation dimension (D c) is being used in this study with the seismicity for the period 1961 to recent for understanding the pattern of seismic hazard. The entire area has been divided into four major tectonic blocks, and each block event was divided into consecutive fifty events window for seeing spatiotemporal patterns. After comparing the patterns, we have identified that Block of Eastern Himalaya near Main Central Thrust, Main Boundary Thrust, north of Kopili lineament and Block of Shillong plateau near Dauki fault are having relatively intense clustering of events in recent times, which may be identified as the zones of most potential to have a strong event. 相似文献
122.
123.
Sarkar Dipu Ao Taliakum Gunturi Sravan Kumar 《Theoretical and Applied Climatology》2022,148(3-4):1111-1125
Theoretical and Applied Climatology - Electricity is an essential commodity that must be generated in response to demand. Hydroelectric power plants, fossil fuels, nuclear energy, and wind energy... 相似文献
124.
In the past, researchers tried hard classification techniques with contextual information to improve classification results. While modelling the spatial contextual information for hard classifiers using Markov Random Field it has been found that the Metropolis algorithm is easier to program and it performs better when compared with the Gibbs sampler. In this study, it has been found that in the case of soft contextual classification, the Metropolis algorithm fails to sample from a random field efficiently and the Gibbs sampler performs better than the Metropolis algorithm, due to the high dimensionality of the soft classification outputs. 相似文献
125.
Sejuti Naha Biswas Nallamuthu Godhantaraman Ranjit K. Sarangi Bhaskar D. Bhattacharya Santosh K. Sarkar Kamala K. Satpathy 《洁净——土壤、空气、水》2013,41(4):333-339
An intense monospecies bloom of the centric diatom Hemidiscus hardmannianus (Greville) Mann. (Bacillariophyceae) occurred in the coastal waters of Sundarban mangrove wetland, India on 22 July, 2010. The species was abruptly flourished (mean density 8.86 × 106 cells/L) resulting intense green coloration of water. The greatest impoverishment of diversity and density of phytoplankton, micro‐ and mesozooplankton community was observed during the bloom. The phytoplankton community showed an extreme reduction in diversity (12 species to one) and sharp decrease in standing stock (12.84 × 103 to 8.86 × 106 cells/L) during this period. The late bloom condition coincided with sudden and huge arrival of a clupoid fish Hilsa ilisha which forms the most potential fisheries in Sundarban deltaic region. An attempt has been made to correlate the satellite remote sensing‐derived information to the bloom conditions. The MODIS‐Aqua derived chlorophyll and TMI satellite derived sea surface temperature and wind speed maps have been interpreted. 相似文献
126.
Sudip Dey Prasamita Sarkar Chandrani Debbarma Sushmita Paul 《Environmental Earth Sciences》2012,66(2):421-431
This paper aims to assess the geophysical signatures like morphology and structure of a fault line, which is situated in a
part of southern Baromura hill of Tripura, northeast India. In this work manual observations and technical applications were
adopted for understanding the morphological and structural characters of the fault line. As tectonic mapping is one of the
main objectives of this study, the remote sensing technique was used to prepare a tectonic map of the study area. Geothermal
range of the area was measured by unsupervised classification of Landsat TM thermal infrared band (band 6). The classified
thermal band was overlaid by another classified shortwave infrared band (band 7 of Landsat TM), which explains the structural
evidences of the study area. In addition, an automated digital elevation model (DEM) was prepared to assess the morphological
characters of the study area particularly near the confluence of R. Maharani and R. Gumti. To analyse the structural condition
of the faulted zone, resistivity characters of the rocks were measured by “vertical electrical sounding” (VES) method. The
electrical resistivity character of this area strongly supports that a displacement occurred in this place. Finally an attempt
was made to explain the character of faulting on the basis of morphological signatures and structural evidences for future
disaster management planning. 相似文献
127.
Stability of slope will always a problem due to its geodynamic nature of Himalayan region. The area investigated belongs to
the Lower Siwalik formation, which is prone to failure due to presence of various weak planes or structures present in the
rock mass. Frequent landslides causing loss of life, property, disturbance of morphological, surface and subsurface water
flow pattern. A huge landslide in the Amiyan area occurred in 1999 and blocked the Gaula River which caused loss of agricultural
land and other properties as well as waterlogged upstream side. The debris of Amiyan slope contains soil and sandstones of
various types. This article deals with instability analysis of slopes of the Amiyan area, near Kathgodam, Nainital, Uttarakhand.
This area experiences a number of local as well as regional slides. Extensive field surveys have been carried out to understand
the geological detail. Laboratory experiments have been conducted to determine the various physicomechanical properties of
rock mass. These properties have been used as input parameters for the numerical simulation. A number of researchers have
used two-dimensional numerical models to simulate the slide area. Three-dimensional slope stability studies provide a better
understanding of the mechanism of failure as well as zone of influence. The computed deformations and stress distribution,
along the failure surface, have been compared with the field measurements and found to be in good agreement with field observations.
In this case, finite difference method has been applied on the stability analysis of Amiyan slope. The study indicates that
the slope is vulnerable and needs proper protection. 相似文献
128.
Santanu Banerjee Shovan Lal Chattoraj P. K. Saraswati Somnath Dasgupta Urbashi Sarkar Adam Bumby 《Geological Journal》2012,47(4):357-371
An integrated study of the sedimentology, micropalaeontology, mineralogy and geochemistry of glauconites in the Oligocene Maniyara Fort Formation (western Kutch, India), has been undertaken. Authigenic glauconites, mostly of evolved type, formed within a back‐barrier lagoonal environment. Foraminifera help constrain the biostratigraphy and along with sedimentological evidence, provide information on the depositional conditions. Glauconite in the Maniyara Fort Formation occurs either as infillings within intra‐particle pores of larger foraminifers, or as an altered form of faecal pellets. X‐ray diffraction studies reveal the less mature nature of glauconite infillings compared to the glauconite pellets. Electron microprobe investigation confirms a relative enrichment of K2O and total Fe2O3 in the latter. Both varieties of glauconite formed by initial authigenic precipitation of K‐poor glauconite and subsequently matured by addition of potassium in the interlayer sites and fixation of total iron in the octahedral sites; calcium, magnesium and aluminum were released from the glauconite structure concomitantly. Alkaline conditions during the entire process of glauconite formation did not allow dissolution of foraminiferal tests. Mineralogical and chemical characteristics of the Maniyara Fort Formation glauconites are more similar to deep marine glauconites than those reported from other shallow or marginal marine settings. A low negative cerium anomaly, as well as abundant pyrite, suggests formation of glauconite in sub‐oxic micro‐environments, created by decay of organic matter associated with foraminiferal chambers and faecal pellets. Sub‐oxic condition apparently prevailed relatively longer within the Maniyara Fort Formation lagoons. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
129.
130.
Results of comparison exercises carried out between the state-of-the-art TOPEX/POSEIDON altimeter-derived ocean surface wind speed and ocean wave parameters (significant wave height and wave period) and those measured by a set of ocean data buoys in the North Indian Ocean are presented in this article. Altimeter-derived significant wave height values exhibited rms deviation as small as - 0.3 m, and surface wind speed of - 1.6 m/s. These results are found consistent with those found for the Pacific Ocean. For estimation of ocean wave period, the spectral moments-based semiempirical approach, earlier applied on GEOSAT data, was extended to TOPEX/POSEIDON. For this purpose, distributions of first four years of TOPEX/POSEIDON altimeter data and climatology over the North Indian Ocean were analyzed and a new set of coefficients generated for estimation of wave period. It is shown that wave periods thus estimated from TOPEX/POSEIDON data (for the subsequent two years), when compared with independent data set of ocean data buoys deployed in the North Indian Ocean, exhibit improved accuracy (rms ~ - 1.4 nos) over those determined earlier with GEOSAT data. 相似文献