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| Paper Type | : | Research Paper |
| Title | : | Demarcation of Faults and Fracture Zones from Very Low Frequency-EM Studies |
| Country | : | India |
| Authors | : | M. Preeti || G. Ramadass |
| : | 10.9790/0990-0605010104 ![]() |
Abstract: The Very Low Frequency-EM method is helpful to identify the different geological formations, faults and fractures depending upon their variable conductive properties. The study area Putluru and Yellanur mandals in Ananthapur district, AP mainly covered with Tadipatri shales and few sills and dyke intrusions are present in these shales. Real and Imaginary component plots and Real component pseudo sections up to depth of 60m clearly demarcated the tectonically disturbed zones from the undisturbed areas. Several faults and fractures are identified from these VLF studies which are highly conductive. The evidence of sill intrusions are inferred from high resistive zones in the medium resistive zones of Tadipatri shales.
Keywords- Tadipatri shales, Conductive zones, Sill intrusions, faults and fractures.
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Abstract: Seismic characteristics in the Middle Benue Trough were investigated at 39 acquisition stations Seismic refraction method. Two overlapping reversed profiles were shot into 12 stations of geophones at each station. Each shot hole was 1.5m deep primed with 0.20kg dynamite as source. The acquisition equipment was McSeis-160MXTM. Analysis of the results revealed 2-layers cases. The velocity of the Low-Velocity Layer, Vo, varies between 399 and 944ms-1 with average of 659.13 ms-1. The underlying Consolidated Layer has velocity, V1, which varies between 1210 and 4240ms-1 with an average of 2214.00ms-1. Velocity appears greater when shooting up-dip, while velocity is reduced when shooting down-dip which could be attributed to either dipping layers or/and subsurface sediment heterogeneity. Depth of refractor, Z, varies between 2.80 and 6.5m with average of 4.38m. Elevation varies between 63 and 228m with average of 148.51m. Weathered thickness and elevation were highly variable resulting from both surface- and surface-topographic.........
Keywords- Seismic refraction, velocity, weathered and consolidated layers, bedrock, Middle Benue Trough, Nigeria.
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Abstract: With the advent of remote sensing techniques, there are a large number of tools that can contribute directly to the analysis of the modified urban environment, since the expansion of a certain occupied area as well as its occupation can be easily detected through images of satellite. The objective of this research is to evaluate the changes occurred in Planning Area 4 - in Rio de Janeiro, using TM / LANDSAT Image Detection techniques to detect soil cover changes occurring in the period from 2000 to 2015. The images were submitted to specific curves with the spectral response of the targets to verify the adjustment of the images. Finally, the GEOBIA model was generated for the identification of urban areas, using the descriptors NDBI, NDWI and NDVI. After the modeling of the descriptors and the mapping of urban areas in the PA 4 it was possible to identify changes and social characteristics of the results.
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