Variance - Correlation analysis in the exploration of hydrothermal (fluidogenous) deposits using surface gamma-ray spectrometry; Journal of Applied Geophysics; Vol. 159

Bibliografiske detaljer
Parent link:Journal of Applied Geophysics
Vol. 159.— 2018.— [P. 597-604]
Institution som forfatter: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Andre forfattere: Sobolev I. S. Igor Stanislavovich, Orekhov A. N. Aleksandr Nikolaevich, Bratec T. Tatiana, Rikhvanov L. P. Leonid Petrovich, Soboleva N. P. Nadezhda Petrovna
Summary:Title screen
This paper describes a possibility of using variance-correlation analysis for the detection of hydrothermal alterations by conducting a surface gamma-ray spectrometry survey. Gamma-ray spectrometry data processing includes a low-pass filtration, identification of potassium, uranium and thorium residual components, as well as an analysis of their variance and correlation. The high variance of radioactive elements and the features of their correlation are dependent on the mineral structure of hydrothermally altered rock that forms the secondary dispersion halos. The variance intensity, as well as the strength and the type of correlational anomalies, depends on the fluidogenic systems scale.
Режим доступа: по договору с организацией-держателем ресурса
Sprog:engelsk
Udgivet: 2018
Fag:
Online adgang:https://doi.org/10.1016/j.jappgeo.2018.10.007
Format: Electronisk Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=659300

MARC

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330 |a This paper describes a possibility of using variance-correlation analysis for the detection of hydrothermal alterations by conducting a surface gamma-ray spectrometry survey. Gamma-ray spectrometry data processing includes a low-pass filtration, identification of potassium, uranium and thorium residual components, as well as an analysis of their variance and correlation. The high variance of radioactive elements and the features of their correlation are dependent on the mineral structure of hydrothermally altered rock that forms the secondary dispersion halos. The variance intensity, as well as the strength and the type of correlational anomalies, depends on the fluidogenic systems scale. 
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701 1 |a Sobolev  |b I. S.  |c geologist, geochemist  |c associate Professor of Tomsk Polytechnic University, candidate of geological-mineralogical Sciences  |f 1974-  |g Igor Stanislavovich  |3 (RuTPU)RU\TPU\pers\36879 
701 1 |a Orekhov  |b A. N.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences  |f 1962-  |g Aleksandr Nikolaevich  |3 (RuTPU)RU\TPU\pers\32554 
701 1 |a Bratec  |b T.  |g Tatiana 
701 1 |a Rikhvanov  |b L. P.  |c Professor of Tomsk Polytechnic University  |c Doctor of geological- mineralogical sciences  |c Honored geologist of Russia  |c Honored Worker of higher professional education of the Russian Federation  |f 1945-  |g Leonid Petrovich  |3 (RuTPU)RU\TPU\pers\25922 
701 1 |a Soboleva  |b N. P.  |c specialist in the field of landscape  |c Associate Professor of Tomsk Polytechnic University, Candidate of geographical sciences  |f 1975-  |g Nadezhda Petrovna  |3 (RuTPU)RU\TPU\pers\32402  |9 16353 
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