Zobrazeno 1 - 10
of 28
pro vyhledávání: '"B. Veeraiah"'
Publikováno v:
Geosystems and Geoenvironment, Vol 2, Iss 2, Pp 100141- (2023)
A conspicuous zone marked with linear Bouguer gravity anomalies encompassed with overall regional gravity high zone spreads about 5° length and width of about 1 to 1 1/2° in the central part of Dharwar Craton is not entirely relatable to surface ge
Externí odkaz:
https://doaj.org/article/cffe50e097bb4eccb4d94a6bb60df333
Publikováno v:
Journal of the Geological Society of India. 96:239-249
Dharwar craton (DC), by far the largest geological domain in South Indian Shield, occupying about 0.5 million sq. km area, is well-studied terrain both for regional geoscientific aspects and as part of mineral exploration over several important block
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d70f011b011dc221d45c5d51f5026d0
https://doi.org/10.1007/s12594-020-1543-8
https://doi.org/10.1007/s12594-020-1543-8
Publikováno v:
Journal of Earth System Science. 130
The eastern margin of the Chitradurga Schist Belt is widely believed as the dividing line of Dharwar Craton (DC) into Western Dharwar Craton (WDC) and Eastern Dharwar Craton (EDC). This study aims at re-defining the division of DC based on pronounced
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd70747e7d9c77a45f4532f7a0e4f34f
https://doi.org/10.1007/s12040-021-01621-2
https://doi.org/10.1007/s12040-021-01621-2
Publikováno v:
Journal of the Geological Society of India. 98:146-146
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::259e3943f62d304ed31788e78f7d6bce
https://doi.org/10.1007/s12594-022-1944-y
https://doi.org/10.1007/s12594-022-1944-y
Akademický článek
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Publikováno v:
Journal of the Geological Society of India. 90:711-719
In this paper, we present results of the Ground Electrical and Electromagnetic (GEE) studies (MT, CSAMT, DRS) carried out in the Koyna-Warna zone since 1976 and discuss their relevance in understanding the seismicity of the Koyna-Warna seismic zone.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9fd9065780ef9f0f5d21da39d6a02234
https://doi.org/10.1007/s12594-017-0780-y
https://doi.org/10.1007/s12594-017-0780-y
Autor:
P. Chandra Sekhara Reddy, B. Veeraiah
The Present study area Panyam mandal is situated in the Kurnool district of Andhra Pradesh. Geologically this mandal is covered with three types of geological formations, Nandyal shales, koilakuntla limestones and Panyam quartzites. Southern half of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::27893eaf2da2fc597b5856980ed5ecac
https://zenodo.org/record/2562699
https://zenodo.org/record/2562699
Akademický článek
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Autor:
B., Veeraiah1 veerngri@yahoo.com, D., Himabindu2 dhimabindu_g@rediffmail.com, G., Ramadass3 profgrdass@yahoo.co.in
Publikováno v:
ICFAI Journal of Earth Sciences. Jul2008, Vol. 2 Issue 3, p37-46. 10p. 3 Graphs, 6 Maps.
Publikováno v:
Hydrogeology Journal. 19:355-366
Exploration and exploitation of groundwater in sedimentary areas are reasonably simple. However, the problem of salinity in coastal areas makes the job very difficult, especially when the freshwater aquifers are not extensive and are entrapped betwee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::def8bec72a7314651c68e08d9aaf5162
https://doi.org/10.1007/s10040-010-0697-7
https://doi.org/10.1007/s10040-010-0697-7