Magnetic field statistical characteristics and their relation to the geological structure of quartz-gold deposits
| Parent link: | Saint Petersburg 2010 - 4th Saint Petersburg International Conference & Exhibition 2010: New Discoveries Through Integration of Geosciences: proc. of meeting, Saint Petersburg, Russia, 5-8 April 2010.— , 2014 Т. 1.— 2014.— P. 460-465 |
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| Beste egile batzuk: | |
| Gaia: | The analysis of experimental data obtained from typical gold deposits in Kuznetskoe Ala Tau and Transbaikal showed that density distribution of increment induction is subjected to the logarithmic normal distribution law, the asymmetry of which, reflects ore prospect metamorphism grade. The spectral dispersion density decreases at average, inversely proportional to square frequency. Local dispersion density increases in low dispersion density background can be in individual ore-bearing zones, which in its turn are associated ore bodies . The magnetic field is characterized by abnormal anisotropy, reflecting the development of diversified elements of the formation structure. Normal entropy induction variations exceeds 0.8, indicating the heterogeneous petromagnetic zone structure. The paper includes field observation technique recommendations and interpretation results. В фонде НТБ ТПУ отсутствует |
| Hizkuntza: | ingelesa |
| Argitaratua: |
2014
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| Formatua: | Liburu kapitulua |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=602218 |
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| 200 | 1 | |a Magnetic field statistical characteristics and their relation to the geological structure of quartz-gold deposits |f L. Ya. Erofeev, A. N. Orekhov | |
| 320 | |a Ref.: p. 465 (6 tit.) | ||
| 330 | |a The analysis of experimental data obtained from typical gold deposits in Kuznetskoe Ala Tau and Transbaikal showed that density distribution of increment induction is subjected to the logarithmic normal distribution law, the asymmetry of which, reflects ore prospect metamorphism grade. The spectral dispersion density decreases at average, inversely proportional to square frequency. Local dispersion density increases in low dispersion density background can be in individual ore-bearing zones, which in its turn are associated ore bodies . The magnetic field is characterized by abnormal anisotropy, reflecting the development of diversified elements of the formation structure. Normal entropy induction variations exceeds 0.8, indicating the heterogeneous petromagnetic zone structure. The paper includes field observation technique recommendations and interpretation results. | ||
| 333 | |a В фонде НТБ ТПУ отсутствует | ||
| 461 | |t Saint Petersburg 2010 - 4th Saint Petersburg International Conference & Exhibition 2010: New Discoveries Through Integration of Geosciences |o proc. of meeting, Saint Petersburg, Russia, 5-8 April 2010 |d 2014 | ||
| 463 | |t Т. 1 |v P. 460-465 |d 2014 | ||
| 610 | 1 | |a труды учёных ТПУ | |
| 700 | 1 | |a Erofeev |b L. Ya. |c geologist, geophysicist |c Professor of Tomsk Polytechnic University, Doctor of geological and mineralogical sciences |f 1935- |g Leonid Yakovlevich |3 (RuTPU)RU\TPU\pers\32553 | |
| 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 | |
| 801 | 1 | |a RU |b 63413507 |c 20110823 | |
| 801 | 2 | |a RU |b 63413507 |c 20150625 |g RCR | |
| 942 | |c BK | ||