Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/54082
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dc.contributor.authorHashemi, Mehdi-
dc.date.accessioned2020-02-28T10:02:49Z-
dc.date.available2020-02-28T10:02:49Z-
dc.date.issued2020-02-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/54082-
dc.description201-206en_US
dc.description.abstractThe study area is located in Nehbandan-Khash zone according to the structural classification of Iran. The outcrops of this area are mainly composed of Cenozoic and Quaternary units. The structure of the area, under the influence of faults and folding, has a trend from north-northwest to south-southeast. Airborne data of radiometric was collected in the study area. In the exploration area of Zahedan, after processing and statistical analysis airborne radiometric data and preparing the map of the radioactive elements with the same intensity, the anomaly ranges were determined. For this purpose, two Ordinary Kriging and inverse distance squared technique were used to estimate the data. The trend of these radioactive element anomalies in the area was the general northwest-southeast trend, as identified in the maps. These anomalies of the radioactive elements are found in the Oligo-Miocene granodiorites units. Three anomaly ranges are located in the north-eastern corner of the sheet, which are proposed as valuable anomalies for continuing exploratory study.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.49(02) [February 2020]en_US
dc.subjectAnomaliesen_US
dc.subjectGranodioriteen_US
dc.subjectRadiometryen_US
dc.subjectRadioactive elementsen_US
dc.subjectZahedanen_US
dc.titleRemote sensing and airborne geophysics studies for uranium and thorium exploration in Zahedan area (Southeastern Iran)en_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.49(02) [February 2020]

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