Geology and geochemistry of the Degana pluton—A proterozoic rapakivi granite in Rajasthan,India     

B. Chattopadhyay  S. Chattopadhyay  V. S. Bapna 《Mineralogy and Petrology》1994,50(1-3):69-82

Summary The Degana pluton hosts one of the few known tungsten deposits in India It is an epizonal, moderately high silica pluton emplaced during the Proterozoic in a posttectonic setting. Though homogeneous in composition, it displays textural heterogeneity from coarse-grained hypidiomorphic to fine-grained porphyritic to hypabyssal granite porphyry. Genetically related rhyolites are also present. Coherency of geochemical and mineralogical attributes in the Degana pluton can be explained by fractional crystallisation. Complex variety of hydrothermal and pneumatolytic features is also present. At shallow depths, emanation differentiation has led to progressive enrichment of Li, Rb, and W. Both the plutonic and volcanic phases of the magma show development of rapakivi texture and other diagnostic characteristics of the rapakivi granites.The Degana granite is a specialised granite and classified as an A-type intraplate anorogenic granite of mantle plume origin. The mineralogy and chemistry of the Degana pluton compares well with the various rapakivi granites of south-eastern Fennoscandia. Chemical and textural characteristics of the Degana pluton provide a constraint on the formation of the rapakivi texture when interpreted in terms of experimentally determined phase equilibria. The mantling process is interpreted as a result of pressure fluctuations due to escape and recharging of volatiles (e.g., H2O and F) accompanying the emplacement of the magma.

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Geologie und Geochemie des Degana-Plutons—ein proterozoischer Rapakivi Granite in Rajasthan, Indien

Zusammenfassung Der Degana Pluton enhält eine der wenigen in Indien bekannten Wolfram-Lagerstätten. Es handelt sich hier um einen epizonalen Pluton mit höheren Si-Gehalten, der während des Proterozoikums in ein posttektonisches Setting intrudiert wurde. Obwohl er in seiner Zusammensetzung homogen ist, zeigt er Heterogenität auf dem texturellen Bereich, die von grobkörnig hypidiomorph bis feinkörnig porphyritisch und schließlich bis zu hypabyssischen Granitporphyren reicht. Genetisch verwandte Rhyolite kommen im Untersuchungsgebiet auch vor. Übereinstimmende geochemische und mineralogische Parameter können auf fraktionierte Kristallisation zurückgeführt werden. Eine komplexe Vielfalt von hydrothermalen und pneumotolytischen Erscheinungen ist bemerkenswert. In geringen Tiefen hat die Emanations-Differentiation zu einer progressiven Anreicherung von Li, Rb und W geführt. Sowohl die plutonischen als auch die vulkanischen Erstarrungsprodukte des Magmas zeigen die Entwicklung von Rapakivi-Texturen und anderen diagnostischen Eigenschaften der Rapakivi-Granite.Der Degana-Granit ist ein spezialisierter Granit und ist als ein anorogener Intraplattengranit des A-Typs zu klassifizieren, der auf einen mantle plume zurückgeführt wird. Die Mineralogie und Chemie des Degana-Plutons läßt sich gut mit der verschiedener Rapakivi Granite im südöstlichen Fennoskandien vergleichen. Chemische und texturelle Eigenheiten des Degana Plutons ermöglichen eine Eingrenzung der Bildung von Rapakivi Texturen, sofern sie im Sinne experimentell bestimmter Phasen-Gleichgewichte interpretiert werden. Die Entstehung von Überwachsungen einzelner Kristalle wird als Resultat von Druckschwankungen interpretiert, die auf das Entweichen und die Neuzufuhr von volatilen Phasen (i.e. H₂O und F) im Gefolge der Platz nahme des Magmas zurückzuführen sind.

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Application of Remote Sensing and Geographic Information System in infrastructure development     

Mahamaya Chattopadhyay  R S Resmi  A S Promodhlal 《Journal of the Indian Society of Remote Sensing》2002,30(3):143-147

Road transportation network development is a vital component of infrastructure development. Absence of database on roads of Trivandrum district was felt as a major hindrance in prioritizing improvement/development/repair of the roads for better traffic efficacy. High resolution PAN imagery (IRS-IC, September-December 1999, 1:25,000 scale) was visually interpreted to decipher road net work for preparing an elaborate database for Kerala Highway. The data were incorporated on 1:25,000 scale SOI base maps. Field verification was carried out to identify and categorize the PWD roads as per their administrative sections. Final maps were digitized in ARC/INFO environment. Information about terrain conditions was also generated using satellite remote sensing images and aerial photographs. Incorporating the height source and elevation data in the value field and taking mass points as input, a TIN (Triangulated Irregular Network) model of a sample area near Vellanad, 22 km east of Trivandrum city was created to analyse the terrain-road network interrelationship. Our case study involving draping of road network on TIN model as well as on geomorphology map established that this methodology could be used to define alternative and efficient route corridors, with particular emphasis on selection of the least-cost route and prioritization of repair.  相似文献   

Single hidden layer artificial neural network models versus multiple linear regression model in forecasting the time series of total ozone     

G. Bandyopadhyay B.Sc. in chemistry  M.Sc.  S. Chattopadhyay B.Sc. 《International Journal of Environmental Science and Technology》2007,4(1):141-149

Present paper endeavors to develop predictive artificial neural network model for forecasting the mean monthly total ozone concentration over Arosa, Switzerland. Single hidden layer neural network models with variable number of nodes have been developed and their performances have been evaluated using the method of least squares and error estimation. Their performances have been compared with multiple linear regression model. Ultimately, single-hidden-layer model with 8 hidden nodes have been identified as the best predictive model.  相似文献   

Feed forward Artificial Neural Network model to predict the average summer-monsoon rainfall in India     

Surajit Chattopadhyay 《Acta Geophysica》2007,55(3):369-382

In the present research, possibility of predicting average summer-monsoon rainfall over India has been analyzed through Artificial Neural Network model. In formulating the ANN — based predictive model, three-layer network has been constructed with sigmoid non-linearity. The monthly summer monsoon rainfall totals, tropical rainfall indices and sea surface temperature anomalies have been considered as predictors while generating the input matrix for the ANN. The data pertaining to the years 1950–1995 have been explored to develop the predictive model. Finally, the prediction performance of neural net has been compared with persistence forecast and Multiple Linear Regression forecast and the supremacy of the ANN has been established over the other processes.  相似文献   

Radiatively driven electron–positron jets from two-component accretion flows     

Indranil Chattopadhyay  Santabrata Das  Sandip K. Chakrabarti 《Monthly notices of the Royal Astronomical Society》2004,348(3):846-856

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The Effect of Relative Sunspot Numbers,Solar Flare Numbers and Variable Component of 10.7 cm Solar Flux on The Seasonal Variation of 6300 Å Line Intensity at Calcutta     

Midya  S. K.  Chattopadhyay  R.  Pal  C. M. 《Earth, Moon, and Planets》1997,77(2):93-97

The paper presents the seasonal variation of 6300 Å line intensity at Calcutta with relative sunspot number, solar flare number and variable component of 10.7 cm solar flux. A study has been made and important results have been obtained which are as follows. (i) Intensity of 6300 Å line shows periodic variation with relative sunspot number, solar flare number and variable component of 10.7 cm solar flux during the period 1984–1986 which is the secondary peak of the descending phase of 21st solar cycle. (ii) 6300 Å line intensity at Cachoeira Paulista station, taken by Sahai et al. (1988), also shows periodic variation with solar parameters during the period 1978–1980 which is the peak phase of the solar cycle. (iii) A possible explanation of such a type of variation is also presented.  相似文献   

Editorial     

Samir Mandal  Indranil Chattopadhyay  Anuj Nandi  Santabrata Das 《Journal of Astrophysics and Astronomy》2018,39(1):1

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Study of magnetized accretion flow with cooling processes     

Kuldeep Singh  Indranil Chattopadhyay 《Journal of Astrophysics and Astronomy》2018,39(1):10

We have studied shock in magnetized accretion flow/funnel flow in case of neutron star with bremsstrahlung cooling and cyclotron cooling. All accretion solutions terminate with a shock close to the neutron star surface, but at some regions of the parameter space, it also harbours a second shock away from the star surface. We have found that cyclotron cooling is necessary for correct accretion solutions which match the surface boundary conditions.  相似文献   

Role of ocean–atmosphere interaction on northward propagation of Indian summer monsoon intra-seasonal oscillations (MISO)     

S. Sharmila  P. A. Pillai  S. Joseph  M. Roxy  R. P. M. Krishna  R. Chattopadhyay  S. Abhilash  A. K. Sahai  B. N. Goswami 《Climate Dynamics》2013,41(5-6):1651-1669

Atmospheric dynamical mechanisms have been prevalently used to explain the characteristics of the summer monsoon intraseasonal oscillation (MISO), which dictates the wet and dry spells of the monsoon rainfall. Recent studies show that ocean–atmosphere coupling has a vital role in simulating the observed amplitude and relationship between precipitation and sea surface temperature (SST) at the intraseasonal scale. However it is not clear whether this role is simply ‘passive’ response to the atmospheric forcing alone, or ‘active’ in modulating the northward propagation of MISO, and also whether the extent to which it modulates is considerably noteworthy. Using coupled NCEP–Climate Forecast System (CFSv2) model and its atmospheric component the Global Forecast System (GFS), we investigate the relative role of the atmospheric dynamics and the ocean–atmosphere coupling in the initiation, maintenance, and northward propagation of MISO. Three numerical simulations are performed including (1) CFSv2 coupled with high frequency interactive SST, the GFS forced with both (2) observed monthly SST (interpolated to daily) and (3) daily SST obtained from the CFSv2 simulations. Both CFSv2 and GFS simulate MISO of slightly higher period (~60 days) than observations (~45 days) and have reasonable seasonal rainfall over India. While MISO simulated by CFSv2 has realistic northward propagation, both the GFS model experiments show standing mode of MISO over India with no northward propagation of convection from the equator. The improvement in northward propagation in CFSv2, therefore, may not be due to improvement of the model physics in the atmospheric component alone. Our analysis indicates that even with the presence of conducive vertical wind shear, the absence of meridional humidity gradient and moistening of the atmosphere column north of convection hinders the northward movement of convection in GFS. This moistening mechanism works only in the presence of an ‘active’ ocean. In CFSv2, the lead-lag relationship between the atmospheric fluxes, SST and convection are maintained, while such lead-lag is unrealistic in the uncoupled simulations. This leads to the conclusion that high frequent and interactive ocean–atmosphere coupling is a necessary and crucial condition for reproducing the realistic northward propagation of MISO in this particular model.  相似文献   

Tectonic and lithologic control over landslide activity within the Larji–Kullu Tectonic Window in the Higher Himalayas of India     

Brijendra K. Mishra  Dipanjan Bhattacharjee  Anupam Chattopadhyay  Ganesh Prusty 《Natural Hazards》2018,92(2):673-697

The purpose of this study is to analyze and characterize recent landslide events in the Larji–Kullu Tectonic Window (LKTW), and to establish a relationship between the tectonic and lithologic characters of the terrain and the landslides activity. Using multispectral satellite image analysis with selected field investigation, a landslide occurrence database has been generated for the period between 1984 and 2015. To decipher the accelerated occurrences of landslides in the region, an integrated study is undertaken in the Kullu (also known as Kulu) valley of Beas River basin within the LKTW complex, to analyze the litho-structural and terrain slope interactions using morpho-tectonic parameters such as Topographic/Bedding Plane Interaction Angle (TOBIA) index, terrain surface roughness index and lithological competency analysis. A prominent clustering of landslides is observed in the north of Sainj River, contained within the tectonic window. Major sites of landslides are found to be located in the intensely fractured Manikaran Quartzite occurring within the core of the LKTW. The landslides are mostly associated with southern and southwestern-facing slopes and activations are pronounced in the ‘Orthoclinal’ slope class with gradient of 37°–48°. Thematic maps, e.g., geological, structural, geomorphological, slope and slope-aspect maps are generated and considered together to understand the morpho-tectonic scenario of the tectonic window. Observations from the above-stated thematic maps along with the occurrences of moderate magnitude earthquake epicenters helped to infer neotectonic movements along the Sainj River fault. Tectonic upliftment of the northern bank of the Sainj River along with increased precipitation through decades has resulted in recurrent landslides within the LKTW.  相似文献