The Blagodatnoe gold-sulfide deposit (Yenisei Ridge, Russia): the nature of geophysical anomalies and the succession and causes of formation of petrophysical zoning; Russian Geology and Geophysics; Vol. 55, iss. 11
| Parent link: | Russian Geology and Geophysics: Scientific Journal Vol. 55, iss. 11.— 2014.— [P. 1321-1332] |
|---|---|
| Hovedforfatter: | |
| Institution som forfatter: | |
| Summary: | Title screen Data on geophysical fields and petrophysical heterogeneity, parageneses and the thermodynamic conditions and age of their formation, and fluid inclusions were used for the genetic reconstruction of petrophysical zoning at the Blagodatnoe gold-sulfide deposit. Petrophysical associations of the preore and ore stages of the deposit formation are clearly reflected in anomalies of the magnetic and natural electric fields and the aureoles of radioactive elements. At the early preore stage (752 Ma), reduced solutions with high activity of K, enriched in U, Th, and, probably, Au, were supplied to intensely foliated tectonic zones. Their interaction with initial metasedimentary rocks gave rise to contiguous zones of quartz–muscovite and chlorite metasomatic rocks. Режим доступа: по договору с организацией-держателем ресурса |
| Sprog: | engelsk |
| Udgivet: |
2014
|
| Fag: | |
| Online adgang: | http://dx.doi.org/10.1016/j.rgg.2014.10.007 |
| Format: | Electronisk Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=653381 |
MARC
| LEADER | 00000naa0a2200000 4500 | ||
|---|---|---|---|
| 001 | 653381 | ||
| 005 | 20250227115141.0 | ||
| 035 | |a (RuTPU)RU\TPU\network\18822 | ||
| 090 | |a 653381 | ||
| 100 | |a 20170301d2014 k||y0rusy50 ba | ||
| 101 | 0 | |a eng | |
| 102 | |a NL | ||
| 135 | |a drcn ---uucaa | ||
| 181 | 0 | |a i | |
| 182 | 0 | |a b | |
| 200 | 1 | |a The Blagodatnoe gold-sulfide deposit (Yenisei Ridge, Russia): the nature of geophysical anomalies and the succession and causes of formation of petrophysical zoning |d Золото-сульфидное месторождение Благодатное (Енисейский кряж, Россия): природа геофизических аномалий, последовательность и причины образования петрофизической зональности |f Yu. V. Kolmakov | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 320 | |a [References.: 49 tit.] | ||
| 330 | |a Data on geophysical fields and petrophysical heterogeneity, parageneses and the thermodynamic conditions and age of their formation, and fluid inclusions were used for the genetic reconstruction of petrophysical zoning at the Blagodatnoe gold-sulfide deposit. Petrophysical associations of the preore and ore stages of the deposit formation are clearly reflected in anomalies of the magnetic and natural electric fields and the aureoles of radioactive elements. At the early preore stage (752 Ma), reduced solutions with high activity of K, enriched in U, Th, and, probably, Au, were supplied to intensely foliated tectonic zones. Their interaction with initial metasedimentary rocks gave rise to contiguous zones of quartz–muscovite and chlorite metasomatic rocks. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | |t Russian Geology and Geophysics |o Scientific Journal | ||
| 463 | |t Vol. 55, iss. 11 |v [P. 1321-1332] |d 2014 | ||
| 510 | 1 | |a Золото-сульфидное месторождение Благодатное (Енисейский кряж, Россия): природа геофизических аномалий, последовательность и причины образования петрофизической зональности |z rus | |
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a золотое оруденение | |
| 610 | 1 | |a петрофизическая зональность | |
| 610 | 1 | |a Енисейский кряж | |
| 700 | 1 | |a Kolmakov |b Yu. V. |c geologist |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences |f 1966- |g Yuriy Viktorovich |3 (RuTPU)RU\TPU\pers\35859 |9 19002 | |
| 712 | 0 | 2 | |a Национальный исследовательский Томский политехнический университет (ТПУ) |b Институт природных ресурсов (ИПР) |b Кафедра геофизики (ГЕОФ) |3 (RuTPU)RU\TPU\col\18667 |
| 801 | 2 | |a RU |b 63413507 |c 20170301 |g RCR | |
| 856 | 4 | |u http://dx.doi.org/10.1016/j.rgg.2014.10.007 | |
| 942 | |c CF | ||